Skocz do pozycji: 1.

Tytuł:

A Strategic Environmental Assessment for Southern Coastal of West Java Province, Indonesia

Autorzy:

Rizal, Achmad
Andriani, Yuli
Kusumartono, F. X. Hermawan

Powiązania:

https://bibliotekanauki.pl/articles/1046561.pdf

Data publikacji:

2019

Wydawca:

Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN

Tematy:

Environmental
West Java
management
southern coastal

Opis:

Urban development along the southern coastal zone of West Java province involves land-use changes that have a direct impact on coastal ecosystems and services. The southern coastal, a metropolitan area to the south of west java province, is a study case in which the urban coastal occupation is reflected, with the consequent loss of certain services that the ecosystems offer to the population. The research analyses the Environmental Impact Assessment and the impacts of Coastal Zone Management proposals. The methodology used in the research leads to the Drivers-Pressures-State change-Impact-Response (DPSIR) perspective. The approach to the DPSIR has been based on a set of objectives that have brought a strong focus on the long-term preservation of the environment. As such, the planning process has included - and is recommended to include - the following steps: a) Environmental risk assessment; b) Sieve mapping process; c) Formulation of development regulations; d) Local development plans; e) Environmental Impact Assessment, f) Environmental Management Plan. In this sense, management responses should focus on the conservation of these threatened services, with the coordination and cooperation among different public administrations.

Źródło:

World Scientific News; 2019, 137; 188-209
2392-2192

Pojawia się w:

World Scientific News

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 2.

Tytuł:

Vulnerability assessment of Southern coastal areas of Iran to sea level rise: evaluation of climate change impact

Autorzy:

Goharnejad, H.
Shamsai, A.
Hosseini, S.A.

Powiązania:

https://bibliotekanauki.pl/articles/48331.pdf

Data publikacji:

2013

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

climate change
sea level rise
coastal area
Iran
general circulation model
sea-level change
artificial intelligence
artificial neural network
hydrological model

Źródło:

Oceanologia; 2013, 55, 3
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 3.

Tytuł:

The evolution of the southern Baltic coastal zone

Autorzy:

Mojski, J.E.

Powiązania:

https://bibliotekanauki.pl/articles/47713.pdf

Data publikacji:

2000

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

coastal zone
Holocene
post-glacial topography
forecast
Baltic Sea
evolution
Late Glacial
water level

Opis:

This article discusses the formation and evolution of the coastal zone of the southern Baltic from the decay of the last Scandinavian ice-sheet, which took place some 14 ka BP. During the first 4 ka, the shores of the then southern Baltic basins were shaped under the dominant influence of considerable variations in water level and the young, post-glacial topography emerging from under the ice. Later, until the beginning of the Atlantic transgression, the shores were also unstable, because sea level changes resulting from periodic connections with the World Ocean followed one another in rapid succession. Since that transgression destroyed much of the former shoreline, its reconstruction is at best highly problematical, and in some places no longer possible. The maximum range of the Litorina Sea gave rise to a coastal zone that in many places is to this day quite conspicuous in the local topography and sediments. During the last 4 ka, the shoreline has changed relatively little, thus the present shoreline is largely redolent of the original one. In the coming 100 years or so, the abrasion of the cliffs along the southern Baltic shore will probably accelerate, as will the retrogradation of certain sections of the shoreline, with the result that the shoreline will be less of a straight line than it is at present. Land up to a height of 1 m above sea level will be inundated. The greatest changes in the lie of the shoreline are to be expected in the River Wisła (Vistula) delta and around the Zalew Szczeciński (Oderhaff, Szczecin Lagoon).

Źródło:

Oceanologia; 2000, 42, 3
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 4.

Tytuł:

Development of the Southern Coastal zone of the Eastern Gulf of Finland (from lebyazhye to the St. Petersburg flood protective dam)

Autorzy:

Suslov, G. A.
Ryabchuk, D. V.
Nesterova, E. N.
Fedorova, E. K.

Powiązania:

https://bibliotekanauki.pl/articles/1204981.pdf

Data publikacji:

2008

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

sand drift
coastal zone dynamics
southern coastal zone of the Gulf of Finland

Opis:

In July–September 2004 and April 2005, the specialists of the Department of Marine and Environmental Geology of All-Russian Geological Institute (VSEGEI) conducted field studies of the coastal zone of the Gulf of Finland from thesouthern alignment of the St. Petersburg Flood Protective Dam to Lebyazhye. The basic purpose of the studies is the analysis of coastal zone dynamics. Along the southern coast of the Gulf of Finland from Lebyazhye to the Dam, three different coastal dynamics zones were identified: (1) flat accumulative shore with aquatic plants, (2) erosion zone and (3) zone of modern sand accumulation. Along-shore sand drift in the eastern direction was also determined. Alongside with routine observations, the comparative analysis of space photography images of the study area, carried out during last 20 years, allowed finding out that as a result of intense eastward sand transfer, as mush as 80 metres of sand accumulative bodies have been eroded since 1982 near the village of Izhora. To the west of a small river, a 230-metres long sand split has been formed since 1982.

Źródło:

Polish Geological Institute Special Papers; 2008, 23; 109-116
1507-9791

Pojawia się w:

Polish Geological Institute Special Papers

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 5.

Tytuł:

Wave-induced bedload transport – a study of the southern Baltic coastal zone

Autorzy:

Dudkowska, A.
Gic-Grusza, G.

Powiązania:

https://bibliotekanauki.pl/articles/94655.pdf

Data publikacji:

2017

Wydawca:

Uniwersytet im. Adama Mickiewicza w Poznaniu

Tematy:

sediment transport models
non-cohesive sediments
bottom shear stress
northern Europe
modele transportu osadów
nierówne osady
naprężenie ścinające
północna Europa

Opis:

The wave-induced bedload transport and spatial distribution of its magnitude in the southern Baltic coastal zone of Poland are estimated. The vicinity of Lubiatowo was selected as a representative part of the Polish coast. It was assumed that transport is a function of shear stress; alternative approaches, based on force balances and discharge relationships, were not considered in the present study. Four models were studied and compared over a wide range of bottom shear stress and wind-wave conditions. The set of models comprises classic theories that assume a simplified influence of turbulence on sediment transport (e.g., advocated by authors such as Du Boys, Meyer-Peter and Müller, Ribberink, Engelund and Hansen). It is shown that these models allow to estimate transport comparable to measured values under similar environmental conditions. A united general model for bedload transport is proposed, and a set of maps of wave bedload transport for various wind conditions in the study area is presented.

Źródło:

Geologos; 2017, 23, 1; 1-14
1426-8981
2080-6574

Pojawia się w:

Geologos

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 6.

Tytuł:

Distribution and invasiveness of a colonial ascidian, Didemnum psammathodes, along the Southern Indian coastal water

Autorzy:

Jaffar, H.A.
Akram, A.S.
Arshan, M.L.K.
Sivakumar, V.
Tamilselvi, M.

Powiązania:

https://bibliotekanauki.pl/articles/48689.pdf

Data publikacji:

2016

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Źródło:

Oceanologia; 2016, 58, 3
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 7.

Tytuł:

Przydatność skanowania laserowego do badań strefy brzegowej południowego Bałtyku
Suitability of laser scanning in the southern Baltic coastal zone research

Autorzy:

Dudzińska-Nowak, J.

Powiązania:

https://bibliotekanauki.pl/articles/129862.pdf

Data publikacji:

2007

Wydawca:

Stowarzyszenie Geodetów Polskich

Tematy:

skanowanie laserowe
NMT
NMPT
strefa brzegowa
laser scanning
DTM
DSM
coastal zone

Opis:

Strefa brzegowa ze względu na swa niedostępność i dynamiczne procesy w niej zachodzące stanowi bardzo ciekawy, ale równocześnie, trudny obszar badawczy. Zróżnicowanie środowisk wymagało do tej pory stosowania różnych technik badawczych, a analiza pozyskanych w ten sposób wyników nie pozwalała na pełny opis skomplikowanych zjawisk i prawidłowości rozwoju. Nowe możliwości w badaniach strefy brzegowej pojawiły sie wraz ze skonstruowaniem zintegrowanych urządzeń skanowania laserowego (LiDAR) pozwalających na równoczesna, szybka i precyzyjna rejestracje rzeźby dna morskiego i przylegającej do niego powierzchni ładu. Wykonanie pomiarów w okresie największej przejrzystości wody i przy sprzyjających warunkach pogodowych, uwzględniających siłę wiatru i falowania, pozwala na rejestracje dna do 2.5÷3 głębokości krążka Secchi`ego, co w warunkach południowego Bałtyku odpowiada ok. 30 m. Analiza otrzymanego modelu pokrycia powierzchni terenu (DSM) oraz po odfiltrowaniu roślinności i innych obiektów - trójwymiarowego modelu powierzchni terenu (DTM), może pozwolić na powiązanie przyczyn i skutków procesów dynamicznych obserwowanych zarówno w podwodnej jak i nadwodnej części strefy brzegowej. Stwarza, wiec nieporównanie większe możliwości zrozumienia uwarunkowań i przebiegu zjawisk decydujących o skutkach, jakie obserwujemy w strefie brzegowej, szczególnie w aspekcie zniszczeń posztormowych zagrażających infrastrukturze.
The coastal zone, due to its inaccessibility and dynamic processes, is a very interesting but difficult research area. Until recent years, the variety of coastal environments required the use of different research techniques, however the analysis of the results obtained, was not detailed enough to describe very complicated phenomena and coastal development. The integrated laser Canning (LiDAR) technology creates new opportunities to obtain fast, accurate and simultaneous data of the sea bottom and the beach relief. Laser scanning measurements taken in the highest water transparency with good sea and weather conditions make it possible to obtain 2.5÷3 Secchi Depth, which - in case of the south Baltic Sea - equals approximately 30 meters. The analysis of Digital Surface Model (DSM) and Digital Terrain Model (DTM), obtained through filtering vegetation and other objects, allows to identify the relationship between the causes and effects of dynamic processes observed in the underwater and the land part of the coastal zone. Application of the laser scanning technique creates better opportunities to understand the conditions and phenomena observed in the coastal zone, especially storm damages posing threat to the infrastructure.

Źródło:

Archiwum Fotogrametrii, Kartografii i Teledetekcji; 2007, 17a; 179-187
2083-2214
2391-9477

Pojawia się w:

Archiwum Fotogrametrii, Kartografii i Teledetekcji

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 8.

Tytuł:

The Holocene sea level rise in the Southern Baltic as reflected in coastal peat sequences

Autorzy:

Lampe, R.
Janke, W.

Powiązania:

https://bibliotekanauki.pl/articles/1187355.pdf

Data publikacji:

2004

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

archaeology
medieval period
changes of coastline

Opis:

Coastal peatlands depend in respect to their vertical growth totally on the sea level, are witnesses of its variations and, furthermore, preserve remnants of organisms which permit conclusions about the nutrient content and salinity of the flood water and thus of the surrounding sea. Black layers which occur frequently in the peat profiles point to evolution phases whereas the sea level fell or the mire became desiccated. Around thirty radiocarbon data, data from pollen and diatom analyses as well as from geochemical investigations provide the base to reconstruct the sea level history. The placement of particular transgression/regression stages could be determined with a higher accuracy than before and demonstrate a strong correlation to climate oscillations such as to the Late Bronze Age dry period or the Little Ice Age climate deterioration. Uncertainties still remain in regard to the regression magnitudes and to the length of the hiatuses in the peat sequences.

Źródło:

Polish Geological Institute Special Papers; 2004, 11; 19-29
1507-9791

Pojawia się w:

Polish Geological Institute Special Papers

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 9.

Tytuł:

An assessment the wind potential energy as a generator of electrical energy in the coastal area of southern Iraq

Autorzy:

Hadi, Firas A.
Abdulsada Al-Knani, Basim
Abdulwahab, Rawnak Adel

Powiązania:

https://bibliotekanauki.pl/articles/118705.pdf

Data publikacji:

2020

Wydawca:

Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie

Tematy:

wind energy
Basrah
wind speed analysis
wind potential

Opis:

Renewable energies have the potential to provide relatively clean energy, mostly for domestic energy. Wind power generation is expected to rise in the near future and has grown exponentially over the past decade in many countries. The most important parameter that must be taken into consideration when designing and studying wind power conversion systems is the wind speed. Probability density functions (PDF) such as Weibull is often used in wind speed and wind power analyses. This research presents an assessment of wind power based on the Weibull distribution statistics in the coastal of southern Iraq at Basrah province. Wind speed data for the study site were obtained from NASA at a height of 50 m for the period 1979–2016 with a time interval of 10 min. The data at a height of 50 m were extrapolated using the power law in order to estimate the wind speed at new heights: 30, 70 and 100 m. The different parameters of the Weibull function as well as the daily and monthly wind speeds, mean, variance and potential energy at four altitudes were estimated and analysed using Windographer software. Results indicate that the maximum wind speed at 100 m is 6.4 m·s–1, giving an average power density of 298 W·m–2, which indicates that the location of the study has marginal and useless potential for installing large wind turbines.

Źródło:

Scientific Review Engineering and Environmental Sciences; 2020, 29, 1; 37-53
1732-9353

Pojawia się w:

Scientific Review Engineering and Environmental Sciences

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 10.

Tytuł:

Ice phenomena in rivers of the coastal zone (southern Baltic) in the years 1956-2015
Zlodzenie rzek strefy przymorskiej (południowy Bałtyk) w latach 1956-2015

Autorzy:

Ptak, M.
Choinski, A.

Powiązania:

https://bibliotekanauki.pl/articles/85199.pdf

Data publikacji:

2016

Wydawca:

Akademia Pomorska w Słupsku

Tematy:

ice phenomenon
river
Rega River
Parseta River
Lupawa River
coastal zone
Baltic Sea
Polska
1956-2015 period
climate change

Opis:

The paper presents a description of the course of ice phenomena in three rivers (Rega, Parsęta, Łupawa) in the coastal zone (Southern Baltic) in the territory of Poland. An evident acceleration of the term of decline of ice phenomena has been observed over the period of the last 60 years, varying from 3 to 5 days∙dec-1. The situation caused shortening of the ice season in a range from 3 to 7 days dec-1. The observed transformation of the ice regime of rivers should be associated with climatic changes. The analysis of air temperature in the same period for two meteorological stations (Kołobrzeg, Łeba) suggests a considerable increase in the mean annual air temperature, amounting to 0.3 and 0.2ºC∙dec-1, respectively. In the monthly distribution, temperature growth was the highest in April, where an increase in air temperature of 0.5ºC∙dec-1 and 0.4ºC∙dec-1 was recorded, respectively.
W pracy przedstawiono charakterystykę zlodzenia trzech rzek (Rega, Parsęta, Łupawa) w strefie przymorskiej (Południowy Bałtyk) na terenie Polski. Ustalono, że w okresie ostatnich 60 lat wyraźnie widoczne jest przyspieszenie terminu zakończenia zjawisk lodowych wynoszące od 3 do 5 dni∙dec-1. Sytuacja ta spowodowała skrócenie sezonu lodowego w przedziale od 3 do 7 dni∙dec-1. Obserwowaną transformację reżimu lodowego rzek należy wiązać ze zmianami klimatycznymi. Analiza temperatury powietrza w tym samym okresie dla dwóch stacji meteorologicznych (Kołobrzeg, Łeba) pozwala stwierdzić, że nastąpił znaczny wzrost średniej rocznej temperatury powietrza, który wynosił odpowiednio 0,3 i 0,2°C∙dec-1. W układzie miesięcznym ocieplenie było najwyższe w kwietniu, kiedy odnotowano wzrost temperatury powietrza odpowiednio rzędu 0,5°C∙dec-1 i 0,4°C∙dec-1.

Źródło:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 2016, 20
1643-0115

Pojawia się w:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 11.

Tytuł:

Analysis of 50-year wind data of the Southern Baltic Sea for modelling coastal morphological evolution – a case study from the Darss-Zingst Peninsula

Autorzy:

Zhang, W.
Harff, J.
Schneider, R.

Powiązania:

https://bibliotekanauki.pl/articles/48896.pdf

Data publikacji:

2011

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

Baltic Sea
coastal morphological evolution
coastline change
Darss-Zingst Peninsula
modelling
morphodynamic model
sea level
statistical analysis
wind
wind direction
wind speed

Opis:

High-resolution wind series in the southern Baltic Sea for the period of 1958–2007 are analysed to generate representative climate input conditions for a multi-scale morphodynamic model to simulate decadal-to-centennial coastline change. Four seasonal wind classes, each characterized by a predominant distribution of wind direction and speed, are derived from statistical analysis. Further calibration of this statistical description is done by sensitivity studies of the model to generate similar coastline changes of the Darss-Zingst peninsula as the measured data for the last century. The coastline change of this area is then projected for the next 300 years based on four different climate scenarios, through which impacts of accelerated sea level rise and storm frequency on the long-term coastline change are quantified.

Źródło:

Oceanologia; 2011, 53, (1-TI)
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 12.

Tytuł:

Geohazard assessment of the coastal zone : the case of the southern Baltic Sea

Autorzy:

Uścinowicz, Grzegorz
Szarafin, Tomasz
Pączek, Urszula
Lidzbarski, Mirosław
Tarnawska, Ewa

Powiązania:

https://bibliotekanauki.pl/articles/2058861.pdf

Data publikacji:

2021

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

coastal measurements
northern Poland
land-sea interaction

Opis:

Research by the Polish Geological Survey has been carried out along the southern Baltic coastal zone over a distance of 38 km. The Baltic Sea is classified as non-tidal, and its southern coasts are built entirely of weakly lithified sedimentary rocks. These deposits form three main types of coast, namely cliffs, barriers and alluvial coasts (wetlands), with the research focusing on the first two. Methods including remote sensing, mapping (geological, hydrogeological), offshore survey (bathymetric and geophysical measurements), laboratory analyses and modelling revealed a number of natural hazards. These are, respectively: (1) permanently occurring hazards, causing material damage such as: landslides, coastal erosion and seabed erosion; (2) incidental hazards such as dune breakage and storm surge overflow and (3) hypothetical threats that may occur in the future, such as hydrogeohazards defined here as flooding resulting from groundwater level rise or more rarely, earthquake threats.

Źródło:

Geological Quarterly; 2021, 65, 1; 5
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 13.

Tytuł:

What is the diet of Palaemon elegans Rathke, 1837 (Crustacea, Decapoda), a non-indigenous species in the Gulf of Gdańsk (Southern Baltic Sea)?

Autorzy:

Janas, U.
Baranska, A.

Powiązania:

https://bibliotekanauki.pl/articles/49052.pdf

Data publikacji:

2008

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

alga
Ostracoda
plant component
Baltic Sea
Crustacea
Gammarus
diet
macrozoobenthos
Decapoda
prawn
Ectocarpaceae
coastal zone
Palaemon elegans
non-indigenous species
dietary component
Cladophora
feeding
Gdansk Gulf
Harpacticoida
Chironomidae
animal component

Opis:

Palaemon elegans, a new component of the Gulf of Gdańsk macrozoobenthos, colonised the southern Baltic coastal zone in the late 20th and early 21st century. Analysis of the stomach contents of P. elegans revealed 16 plant and animal taxa that these prawns had fed on. The principal dietary component was detritus, with a mean frequency of occurrence in stomachs of > 80%. The most frequently occurring plant components in the diet were algae from the genus Cladophora and the family Ectocarpaceae, while the most significant animal components were Harpacticoida, Chironomidae, Ostracoda and Gammarus spp. The results of the study show that the dietary composition of P. elegans differed significantly between stations and months. The foraging area consisted of two distinctive regions – the Inner Puck Bay, and the Outer Puck Bay together with the Dead Vistula River; two of the stations – Gdynia and Sopot – were distinct from all the others. However, no obvious seasonality in the food composition could be demonstrated.

Źródło:

Oceanologia; 2008, 50, 2; 221-237
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 14.

Tytuł:

Sulphates in particles of different sizes in the marine boundary layer over the Southern Baltic Sea

Autorzy:

Falkowska, L.
Lewandowska, A.

Powiązania:

https://bibliotekanauki.pl/articles/48464.pdf

Data publikacji:

2004

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

coastal zone
marine boundary layer
sulphate
aerosol
concentration
Baltic Sea

Opis:

Concentrations of sulphate ions and particle size distributions were measured in the marine boundary layer using a ten-cascade Berner impactor at Hel between December 1997 and March 1998, and with a filter packin Gdynia from February to May 2001. In the marine boundary layer over the Hel Peninsula the presence of natural sea-salt and non-sea-salt sulphate ions (nssSO4 2−) was confirmed in the aerosols. The nssSO4 were present in all size ranges only in December 1997 and in the first half of January 1998, making up an average of 83.7±2.4% of the total sulphate content. In the other winter months, nssSO4 2− were recorded only in aerosols of diameters from 0.4 to 1.5 μm, and their average contribution dropped by over 20%. The extended growing season in the Southern Baltic resulted in the formation of fine particles that appeared in the marine boundary layer in early winter. At that time the proportion of nssSO4 2− in ultra-fine particles ranged from 75.7% to 100%. The concentration of nssSO4 2−, which varied from 0.8 to 2.3 nmol m−3 in particles < 0.4 μm in size probably constituted the natural background aerosol population in the relatively clean coastal environment of the Southern Baltic Sea. In the coastal urbanised area of Gdynia, the sulphate concentration in aerosols was higher than at Hel (av. 75.3 nmol m−3) but the proportion of nssSO4 was low, of the order of 24%. Sea salt was then the dominant source of sulphate.

Źródło:

Oceanologia; 2004, 46, 2
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 15.

Tytuł:

Coastal up- and downwelling in the Southern Baltic

Autorzy:

Kowalewski, M.
Ostrowski, M.

Powiązania:

https://bibliotekanauki.pl/articles/47800.pdf

Data publikacji:

2005

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

hydrodynamic modelling
downwelling
upwelling
coastal upwelling
coastal downwelling
Baltic Sea

Opis:

A three-dimensional hydrodynamic model was used to determine 12 zones of upand downwelling in the southern part of the Baltic Sea.O n the basis of a seven-year numerical simulation, the annual frequency of up- and downwelling events in various regions was analysed, their vertical velocity evaluated and the probability of their occurrence for different wind directions calculated.V erification of the model results demonstrated their good correspondence with satellite images, on average equal to 92%.The poorest consistency was recorded for upwelling in the Bornholm region (81%).The annual average frequency of strong upwelling (velocities > 10−4 m s−1) ranged from c.5–7% off the eastern coasts of the southern Baltic to > 31% along the north-eastern coast of Bornholm.A long the Polish coast (excepting the Vistula Spit) downwelling was recorded more frequently than upwelling.The frequency of strong vertical currents was highest in the area to the north of the Hel Peninsula, where high percentages of strong upwelling (27.1%) and downwelling (37.1%) were recorded.

Źródło:

Oceanologia; 2005, 47, 4
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 16.

Tytuł:

Effects of zonal circulation over the Southern Baltic on precipitation at Polish coastal stations
Wpływ cyrkulacji strefowej nad południowym Bałtykiem na opady polskiego wybrzeża

Autorzy:

Swiatek, M.

Powiązania:

https://bibliotekanauki.pl/articles/84855.pdf

Data publikacji:

2004

Wydawca:

Akademia Pomorska w Słupsku

Tematy:

zonal circulation
Southern Baltic Sea
precipitation
Polska
coastal station
coastal zone
geostrophic wind
wind
air mass flow

Źródło:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 2004, 08
1643-0115

Pojawia się w:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 17.

Tytuł:

Alien species of fish parasites in the coastal lakes and lagoons of the Southern Baltic

Autorzy:

Morozinska-Gogol, J.

Powiązania:

https://bibliotekanauki.pl/articles/47573.pdf

Data publikacji:

2009

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

parasite
alien species
aquaculture
Baltic Sea
Southern Baltic
fish parasite
coastal lake
lagoon
infected fish

Opis:

Alien species are now found all over the world. New fish parasites have been unintentionally introduced with infected alien fish imported for aquaculture or have sometimes spread with their intermediate invertebrate hosts transported in the ballast waters of ships. Four alien fish parasites have been recorded in Polish coastal lakes and lagoons, all parasitising eels. Three were introduced with the final host – the Japanese eel – introduced for aquaculture (Anguillicola crassus, Pseudodactylogyrus anguillae and Pseudodactylogyrus bini) and one (Paratenuisentis ambiguus) with its sole intermediate host (Gammarus tigrinus).

Źródło:

Oceanologia; 2009, 51, 1; 105-115
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 18.

Tytuł:

Coastal response to climatic changes : discussion with emphasis on southern Baltic Sea

Autorzy:

Łabuz, T. A.

Powiązania:

https://bibliotekanauki.pl/articles/295126.pdf

Data publikacji:

2012

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

coastal changes
climate factors
South Baltic coast

Opis:

The influence of climate change on coastal areas is indisputable. Natural or anthropogenic elements of the coastal zone often reveal unforeseen changes, not comparable with earlier observations. However, human activity is influenced by climatic events that affect settlements and local economies. This paper presents the increasing threat of climate change to world coastal safety with an emphasis on field research from the coast of the southern Baltic Sea. The main climatic factors that influence the land and shallow seas of the coastal zone are: wind, waves, storm surges, ice jams and flooding.We are forgetting about the relationship between these factors and parts of the affected environment.Acostly shore protection scheme in one area forces erosion in another. It is proposed not to analyse the environmental events on average; such scientific results do not provide the basis for calculating real land erosion. In this paper, it is argued that nature does not respect average values; we need to prepare for greater change due to the escalation of those factors affecting the coast.

Źródło:

Landform Analysis; 2012, 21; 43-55
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 19.

Tytuł:

Geochemistry of surface sediments of a coastal Lake Sarbsko (northern Poland)

Autorzy:

Woszczyk, Michał
Cieśliński, Roman
Spychalski, Waldemar

Powiązania:

https://bibliotekanauki.pl/articles/2026076.pdf

Data publikacji:

2009

Wydawca:

Polska Akademia Nauk. Czytelnia Czasopism PAN

Tematy:

coastal lake
lake sediment geochemistry
Gardno-Łeba Coastal Plain
southern Baltic
Polska

Opis:

The main goal of the pre sented re search was to in ves ti gate spa tial dis tri bu tion of sur face sed i ments and to rec og nize re la tion ships be tween chem i cal com po si tion of wa ter and sed i ments in a coastal Lake Sarbsko (north ern Po land). The Lake Sarbsko is a fresh wa ter ba sin. The wa ter col umn is well ox y gen ated and wa ters ex hibit only mi nor spa tial vari - abil ity of chem i cal com po si tion in di cat ing rapid and good mix ing. Sur face sed i ments of Lake Sarbsko are strongly di - ver si fied with re spect to chem i cal com po si tion. The sed i ments of Lake Sarbsko are char ac ter ized by el e vated con tent of terrigenous sil ica in di cat ing en hanced in put of clastic ma te rial from the wa ter shed and/or in creased dy nam ics of the lake wa ters. More over, SiO2ter is strongly neg a - tively cor re lated with SiO2biog, or ganic mat ter and el e ment con tents, which ar gues for di lut ing ef fect of the for mer to - wards authigenic com po nents of sed i ments. Ba si cally, terrigenous sil ica (quartz) con tent is high est in the lake shores and de clines to wards the lake cen ter. Biogenic sil ica, or ganic mat ter and most of el e ments dis play re versed ten dency. CaCO3 was en coun tered in three iso lated ar eas, where it co-oc curs with FeS. It is an tic i pated that pre cip i ta tion of cal - cite in Lake Sarbsko re sulted from postdepositional pro cesses. Spa tial dis tri bu tion of Fe, Mn, Ca, Mg, Na and K in Lake Sarbsko is also gov erned by their geo chem i cal af fin i ties to or ganic mat ter (Fe), Fe/Mn ox ides (Fe, Mn), sulphides (Fe), clay min er als (Na, K, Mg, Mn) and car bon ates (Ca, Mn).

Źródło:

Studia Quaternaria; 2009, 26; 41-53
1641-5558
2300-0384

Pojawia się w:

Studia Quaternaria

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 20.

Tytuł:

Variability of coastal water hydrodynamics in the Southern Baltic - hindcast modelling of an upwelling event along the Polish coast

Autorzy:

Jankowski, A.

Powiązania:

https://bibliotekanauki.pl/articles/49140.pdf

Data publikacji:

2002

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

variability
temperature
coastal water
hydrodynamics
numerical modelling
Baltic Sea
surface layer
hydrological condition
coastal area

Opis:

This paper presents the results of an attempt to reproduce, with the aid of a numerical circulation model, the hydrological conditions observed in the coastal area of the southern Baltic in September 1989. A large fall in surface layer seawater temperature was recorded in September 1989 at two coastal stations in the vicinity of Kołobrzeg and Władysławowo. This upwelling-like phenomenon was assumed to be related to the specific anemobaric situation in September 1989, however typical of this phenomenon to occur along the Polish Baltic coast (Malicki & Miętus 1994). A three-dimensional (3-D) σ-coordinate baroclinic model of the Baltic Sea, with a horizontal resolution of ∼5 km and 24 sigma-levels in the vertical, was applied to investigate water circulation and thermohaline variability. Hindcast numerical simulation showed that the model provided a good reproduction of the temporal history of the surface seawater temperature and the duration of the upwelling-like fall, but that the model results were underestimated. The maxima of this large fall in the surface layer temperature at both coastal stations are closely related to the phase of change of the upwelling-favourable wind direction to the opposite one. The results of simulation runs showed details of upwelling development due to wind field fluctuations in time and differences in shaping the temperature and current patterns in conjunction with the variations in topography and coastline features in some areas along the Polish coast. Two different hydrodynamic regimes of water movements along the coast resulting from topographical features (the Słupsk Bank) can be distinguished. From the model simulation the specific conditions for the occurrence and development of upwelling at the eastern end of the Polish coast (in the vicinity of Władysławowo) can be deduced.

Źródło:

Oceanologia; 2002, 44, 4
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 21.

Tytuł:

The impact of Klaipeda Port entrance channel dredging on the dynamics of coastal zone, Lithuania

Autorzy:

Zilinskas, G.
Janusaite, R.
Jarmalavicius, D.
Pupienis, D.

Powiązania:

https://bibliotekanauki.pl/articles/2079089.pdf

Data publikacji:

2020

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

Klaipeda Port
Southern Baltic
Lithuania
entrance channel
dredging
coastal zone
sediment transport
lithodynamic condition
coastal erosion

Opis:

Dredging entrance channels to ports on open littoral drift seashores often causes major morphological changes to the shoreline. This study aims to assess the impact of dredging the Port of Klaipėda's entrance channel and the construction of the jetties on the coastal zone. Based on an analysis of cartographic material collected between 1835 and 2017, and on field data (bathymetric surveys and cross-shore profile levelling), changes to the coastal zone in the area nearest to the port were evaluated. The dominant longshore sediment transport on the Lithuanian nearshore runs from south to north. Thus, based on established patterns, intensive accretion could have been expected to take place on the southern side of the port jetties and erosion on their northern side. However, in the case of the Port of Klaipėda, in the area nearest to the port on the updrift side of the port jetties, where accretion would have been expected to take place, the nearshore depth increased throughout the 20th century (when the length and configuration of the jetties did not change). The shoreline shifted landward instead of moving further out to sea. The present study shows that the intensive dredging of the entrance channel caused nearshore and shore erosion on the updrift side of the port jetties, even while a sufficient sediment load was being transported by the longshore drift.

Źródło:

Oceanologia; 2020, 62, 4PA; 489-500
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 22.

Tytuł:

Baltic Sea coastal erosion; a case study from the Jastrzębia Góra region

Autorzy:

Uścinowicz, G.
Kramarska, R.
Kaulbarsz, D.
Jurys, L.
Frydel, J.
Przezdziecki, P.
Jegliński, W.

Powiązania:

https://bibliotekanauki.pl/articles/94521.pdf

Data publikacji:

2014

Wydawca:

Uniwersytet im. Adama Mickiewicza w Poznaniu

Tematy:

barrier and cliff coast
coastal landslides
coastal erosion
coastal protection
southern Baltic Sea
wybrzeże klifowe
osuwiska
erozja wybrzeża
ochrona wybrzeża
południowe Morze Bałtyckie

Opis:

The coastline in the Jastrzębia Góra area can be divided into three major zones of general importance: a beach and barrier section, a cliff section, and a section protected by a heavy hydrotechnical construction. These areas are characterised by a diverse geology and origin, and hence different vulnerability to erosion. In addition, observations have demonstrated a different pace of erosion within each zone. Based on the results obtained by remote sensing methods (analysis of aerial photographs and maps), it has been determined that the coastline in the barrier area, i.e., to the west of Jastrzębia Góra, moved landwards by about 130 m, in a period of 100 years, and 80 m over about 50 years. A smaller displacement of the shoreline could be observed within the cliff. Between the middle of the twentieth and the start of the twenty-first centuries the shore retreated by about 25 m. However, in recent years, an active landslide has led to the displacement of the uppermost part of the cliff locally up to 25 m. Another issue is, functioning since 2000, a heavy hydrotechnical construction which has been built in order to protect the most active part of the cliff. The construction is not stable and its western part, over a distance of 50 m, has moved almost 2 m vertically downwards and c. 2.5 m horizontally towards the sea in the past two years. This illustrates that the erosional factor does not comprise only marine abrasion, but also involves land-based processes determined by geology and hydrogeology. Changes in the shoreline at the beach and barrier part are constantly conditioned by rising sea levels, the slightly sloping profile of the sea floor and low elevation values of the backshore and dune areas. Cliffs are destroyed by mass wasting and repetitive storm surges that are responsible for the removal of the colluvium which protects the coast from adverse wave effects. Presumably, mass movements combined with groundwater outflow from the cliff, plus sea abrasion cause destabilisation of the cliff protection construction.

Źródło:

Geologos; 2014, 20, 4; 259-268
1426-8981
2080-6574

Pojawia się w:

Geologos

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 23.

Tytuł:

Badania hydrogeologiczne wybrzeża Bałtyku Południowego
Hydrogeological investigation of the Southern Baltic coast

Autorzy:

Burzyński, K.
Sadurski, A.

Powiązania:

https://bibliotekanauki.pl/articles/2075402.pdf

Data publikacji:

2015

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

gruntowe wody przybrzeżne
bilans wodny
hydrogeologia wybrzeża
coastal groundwater
fresh/salt water balance
coastal hydrogeology

Opis:

The coastal area of the Southern Baltic is the limit of two different hydrogeochemical environments – fresh and brackish water of sea intrusion and salt ascending water from deep Mesozoic strata. Recognition of these waters occurrence and their origin started about hundred years ago in the Gdańsk region. The Vistula delta plane was the first area of the detailed studies. At that time two sources of the salt waters have been stated – salt water ascension from the Mesozoic strata in the central part of the delta and remaining sea water from the early stages of the delta evolution. The last mentioned belongs to the young relic sea water from the Littorina time. More detailed investigations along the polish Baltic coast has been started in 70. of XX century. The new investigation methods were implemented during last 40 years, especially geoelectrical logging, remote sensing, isotopic and chemical composition examination of water samples, noble gas dissolved in groundwater. The numerical simulation models has been applied and also groundwater chemical modeling is adopted in hydrogeological practice.

Źródło:

Przegląd Geologiczny; 2015, 63, 10/1; 622--627
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 24.

Tytuł:

Limitation of lignin derivatives as biomarkers of land derived organic matter in the coastal marine sediments

Autorzy:

Pempkowiak, J.

Powiązania:

https://bibliotekanauki.pl/articles/2079190.pdf

Data publikacji:

2020

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

lignin oxidation
biomarker
stable carbon isotope
nonlinear analysis
Gdansk Bay
Southern Baltic Sea
coastal sediment

Opis:

Lignin oxidation products (vanillyl, syringil and cummaryl phenols), and δ13C were measured in a variety of land and marine samples collected in Inner Puck Bay – dominated by marine vascular plants, small river run-off, and shallow bottom, and in Gdańsk Bay – characterized by large river run-off, small marine vascular plants population, and the average depth exceeding euphotic zone. Both study areas are parts of the Gdańsk Basin, Southern Baltic. Typical δ13C values (δ13C = -28‰) and both composition and concentrations of lignin phenols were measured in samples originating from land. Small, yet easily measurable amounts of lignin phenols were found in marine vascular plants biomass (Σ8 = 90 µg/100 mg organic matter). The biomass was characterized by exceptionally high δ13C values (-12‰). No lignin phenols and typical δ13C values (-22‰) were measured in marine phytoplankton biomass. δ13C and both composition and content of lignin phenols in organic matter of surface sediments collected in the study area fall in the range marked by the end members. The proportion of land derived organic matter calculated using lignin phenols, or δ13C in Gdańsk Bay were comparable, while in Puck Bay they differed substantially. It was concluded that a) in areas with substantial bottom coverage with vascular plants the two end members approach, usually employed to establish the contribution of organic matter sources, is insufficient, b) organic matter originating from three sources: riverine, phytoplankton, and vascular plants contribute to sedimentary organic matter in Puck Bay with the respective proportion 30:40:30.

Źródło:

Oceanologia; 2020, 62, 3; 374-386
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 25.

Tytuł:

Waves, currents and sea level variations along the Letipea - Sillamäe coastal section of the Southern Gulf of Finland

Autorzy:

Suursaar, U.

Powiązania:

https://bibliotekanauki.pl/articles/48913.pdf

Data publikacji:

2010

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

wave
variation
hydrodynamic condition
measurement
Doppler current prolifer
calibration
semi-empirical hindcast
water parameter
upwelling
coastal jet
climate change
Baltic Sea
Letipea-Sillamae coastal section
Finland Gulf

Opis:

Variations in the hydrodynamic conditions were studied on the basis of 336 days of measurements with a Doppler current profiler. With wave data as a calibration reference, a semi-empirical hindcast of wave parameters is presented in the fetch- limited near-shore area for the period 1966–2008. A resultant 4–6 cm s−1 westward current dominated along the coast. Occasional fast sub-surface westward currents under modest wind forcing, as well as asymmetrical vertical profiles for westward and eastward currents indicated the influence of upwelling-related baroclinic coastal jets. The average frequency of upwelling was estimated at 17%; some of the events were identified in near-homothermic winter conditions on the basis of salinity and multi-layer flow records. While the mean sea level trend at Narva-Jõesuu roughly approximated the global estimates for 1899–2009, the annual maximum sea level increase was 5–8 mm yr−1. Both mean and maximum wave heights declined as a result of decreasing winds from the north.

Źródło:

Oceanologia; 2010, 52, 3; 391-416
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 26.

Tytuł:

The development of unconsolidated sedimentary coastal cliffs (Pobrzeże Kaszubskie, Northern Poland)

Autorzy:

Uścinowicz, G.
Jurys, L.
Szarafin, T.

Powiązania:

https://bibliotekanauki.pl/articles/2060378.pdf

Data publikacji:

2017

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

cliff coast
landslides
soft sediments
Southern Baltic

Opis:

In the course of fieldwork based on geological and landslide mapping and spatial analyses of map information at least 2 types of landslides were identified. Type I: simple landslides developed in homogeneous and undisturbed rocks, for instance – loams, clays and sands. This type of landslide includes many examples developed mainly on the stretch (segment of the studied area) approximately between 132.25 and 133.50 km and 128.50 and 129.50 km of the Polish coastline. Type II: complex landslides in which the movement and displacement of rock masses occurs under complex geological and hydrogeological conditions. The complex factors are determined by phenomena such as glaciotectonics, discontinuities of rock layers and thrust zones; the slip surface occurs at considerable depths, and sometimes several slip surfaces can be distinguished. These landslide types are located in the vicinity of Jastrzębia Góra and Rozewie, near km 134 and 131.5. Prediction of the formation of this landslide types is difficult. Even if long-term observations are available, the mass movement, variable over time, is difficult to interpret. It is clear that the changes are continuous, but occur with varying intensity. Proper recognition of the types of mass movement is crucial to establishing the appropriate methods to prevent their development.

Źródło:

Geological Quarterly; 2017, 61, 2; 491--501
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 27.

Tytuł:

Ammonia and ammonium over the Southern Baltic Sea. Part 2. The origin of ammonia and ammonium over two coastal stations: Gdynia and Hel

Autorzy:

Lewandowska, A.
Falkowska, L.
Beldowska, M.

Powiązania:

https://bibliotekanauki.pl/articles/48111.pdf

Data publikacji:

2004

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

coastal zone
Gdynia
aerosol
ammonium
ammonia
concentration
Hel Peninsula
Baltic Sea

Opis:

Ammonia concentrations in aerosols and ammonium concentrations in the air were measured in the coastal zone of the southern Baltic Sea. The main study area was the Hel Peninsula, where measurements were carried out from December 1997 to March 1998. There was a second such area in Gdynia, where the first measurement period extended from May to December 2000, and the second one lasted from February to May 2001. At the same time, chloride, sulphate and sodium concentrations in the aerosols were determined; meteorological parameters were also measured. Aerosol samples were collected with a filter pack, and the gaseous phase species were collected on denuders. At both stations, the ammonium concentration in aerosols was at least one order of magnitude higher than that of the ammonia in the air samples. It was found that the marine boundary layer always contained ammonium chloride and ammonium sulphate. The presence of ammonium nitrate was detected only when winds were slight and was attributed to local anthropogenic sources. The ammonia concentration related to nitrate increased with rising air humidity and a falling temperature. The contribution of marigenic ions in aerosols was noted at onshore wind of speeds > 3.5 m s−1. In winter as in summer, conditions occurred facilitating light backscattering by a ‘wet’ aerosol, which contained ammonium nitrate and ammonium sulphate in proportions of 2.5:1 and 1:1.

Źródło:

Oceanologia; 2004, 46, 2
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 28.

Tytuł:

Coastal hydrodynamics beyond the surf zone of the South Baltic Sea

Autorzy:

Ostrowski, R.
Stella, M.
Szmytkiewicz, P.
Kapinski, J.
Marcinkowski, T.

Powiązania:

https://bibliotekanauki.pl/articles/47802.pdf

Data publikacji:

2018

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

hydrodynamic process
coastal region
surf zone
Southern Baltic Sea
wind velocity
bottom sediment
water column
theoretical investigation
experimental investigation

Źródło:

Oceanologia; 2018, 60, 3
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 29.

Tytuł:

Geological structure of the southern Baltic coast and related hazards

Autorzy:

Uścinowicz, Sz.
Zachowicz, J.
Graniczny, M.
Dobracki, R.

Powiązania:

https://bibliotekanauki.pl/articles/1186556.pdf

Data publikacji:

2004

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

klify
mierzeje
erozja brzegu
ruchy masowe
powodzie sztormowe
południowy Bałtyk
cliffs
barriers
coastal erosion
landslides and storm floods
Southern Baltic

Opis:

Długość polskiego wybrzeża morskiego wynosi 498 km (bez linii brzegowej Zalewów Wiślanego i Szczecińskiego). W budowie geologicznej strefy brzegowej, podobnie jak środkowej i północnej Polski, dominują osady czwartorzędowe. Biorąc pod uwagę geomorfologię i budowę geologiczną wyróżniono trzy zasadnicze typy wybrzeży: klify o łącznej długości ok. 101 km, wybrzeża wydmowe (mierzeje) o łącznej długości ok. 380 km oraz wybrzeża nizinne typu Wetland o długości ok. 17 km. Na wybrzeżach klifowych wyróżniono trzy typy ruchów masowych: obrywy dominujące na klifach, w których występuje glina zwałowa, zsuwy i osypiska dominujące na klifach zbudowanych głównie z osadów piaszczystych oraz typowe osuwiska występujące na klifach o złożonej strukturze geologicznej, gdzie główną rolę odgrywają warstwy ilaste będące powierzchnią poślizgu dla warstw wyżej ległych. Poważne zagrożenia związane są też z erozją niskich i wąskich mierzei, które łatwo mogą być przerwane w czasie sztormów. Nisko położone obszary zaplecza mierzei w takim wypadku zagrożone są powodziami sztormowymi. Podobne zagrożenia powodziowe istnieją też na zapleczu mierzei relatywnie stabilnych - szerokich z wysokimi wałami wydmowymi. Powodzie mogą wystąpić w przypadku wysokich stanów wody spowodowanych spiętrzeniami sztormowymi i barycznymi, dochodzącymi maksymalnie do 2 m ponad średni poziom morza, kiedy dochodzi do wlewów wód morskich do Zalewów i jezior przybrzeżnych.

Źródło:

Polish Geological Institute Special Papers; 2004, 15; 61-68
1507-9791

Pojawia się w:

Polish Geological Institute Special Papers

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 30.

Tytuł:

Fine resolution of primary production and its limitation in phytoplankton communities of the Darss-Zingst Bodden chain, a coastal lagoon of the Southern Baltic Sea

Autorzy:

Schumann, R.
Schoor, A.
Schubert, H.

Powiązania:

https://bibliotekanauki.pl/articles/85129.pdf

Data publikacji:

2009

Wydawca:

Akademia Pomorska w Słupsku

Tematy:

primary production
phytoplankton community
Darss-Zingst Bodden chain
coastal lagoon
Baltic Sea
nutrient limitation
size class
aggregate
German coast
nanophytoplankton
heterogeneity
coastal water
eutrophication

Opis:

Evaluated direct methods for estimating primary production are both a precondition and a supplement for modeling scenarios in a eutrophicated and changing coastal ecosystem. Analyses of phytoplankton succession, integral primary production and potential limitation of phytoplankton growth of the shallow brackish Darss-Zingst Bodden chain indicate the extraordinary importance of colony-forming nanophytoplankton for primary productivity. Respective studies began in the 1990s. Exemplary studies focus on the contribution of individual aggregates and phytoplankton colonies to potential primary production as well as the microscale visualization and seasonal variability of extracellular enzymatic phosphate hydrolysis. Results from these studies suggest that an inhomogeneous distribution of productivity and limitation is relevant to the pelagic zones. This paper discusses the effect of heterogeneity on ecosystem behavior in this specific trophy succession state in the context of a future strategy to supplement bulk methods for productivity and limitation analyses especially for barely distinguishable phytoplankton species in euthropicated coastal waters.

Źródło:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 2009, 13 part II
1643-0115

Pojawia się w:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 31.

Tytuł:

Aspects of water quality and transport modelling in the Oder Estuary (Southern Baltic Sea): background, strategy and example

Autorzy:

Schernewski, G.
Neumann, T.
Podsetchine, V.
Wielgat, M.
Tejakusuma, I.

Powiązania:

https://bibliotekanauki.pl/articles/241098.pdf

Data publikacji:

2001

Wydawca:

Polska Akademia Nauk. Instytut Budownictwa Wodnego PAN

Tematy:

water quality
transport modelling
Odra estuary
Baltic Sea
coastal zone management
coastal water management

Opis:

Various types of utilization, conflicting interests and environmental problems call for coastal water management as part of an integrated coastal zone management. This is especially necessary for the Oder (Odra) estuary at the German/Polish border. The river Oder causes severe, ongoing and large scale eutrophication, which limits the ecological and economic value of its adjacent coastal ecosystems. Simulation models are an important tool with which to tackle these practical problems and support management. We present a general concept of a decision support system with an integration of sub-models. Two types of models for long-term water quality forecasts and scenario simulations, as well as short-term prediction of water pollution are available at present. Spatial human-pathogenic virus transport and decay simulations are used as an example to demonstrate their practical use.

Źródło:

Archives of Hydro-Engineering and Environmental Mechanics; 2001, 48, 3; 111-122
1231-3726

Pojawia się w:

Archives of Hydro-Engineering and Environmental Mechanics

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 32.

Tytuł:

Significance of nutrient fluxes via submarine groundwater discharge in the Bay of Puck, Southern Baltic Sea

Autorzy:

Szymczycha, B.
Klostowska, Z.
Lengier, M.
Dzierzbicka-Glowacka, L.

Powiązania:

https://bibliotekanauki.pl/articles/2079294.pdf

Data publikacji:

2020

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

nutrient flux
nitrogen
phosphorus
submarine groundwater discharge
biogeochemistry
coastal zone
Puck Bay
Southern Baltic Sea

Opis:

In this study, we collected submarine groundwater discharge (SGD) and seawater samples at six sites in the Bay of Puck, in the southern Baltic Sea, in order to estimate the nutrient distribution in groundwater affected areas. In addition, we estimated nutrient fluxes via SGD, including both fresh SGD (FSGD) and recirculated seawater SGD (RSGD), to the entire Bay of Puck. Phosphate (PO43−) concentrations varied significantly among study sites and seasons, while both ammonium (NH4+) and nitrates (NO3−) concentrations varied only seasonally. The N:P ratio indicated P limitation in most of the samples. The estimated seasonal and annual loads, via SGD, of both dissolved inorganic nitrogen (DIN; 9303 t yr−1) and PO43− (950 t yr−1), were the most significant source of nutrients to the Bay of Puck, and notably higher than quantified before (FSGD nutrient loads of 50 t yr−1 and 56 t yr−1 for DIN and PO43−, respectively). The SGD fluxes reported here indicate some of the highest rates of sediment-water fluxes reported in the Baltic Sea. These results suggest that SGD (both FSGD and RSGD) should be considered as source of chemical substances to the marine environment.

Źródło:

Oceanologia; 2020, 62, 2; 117-125
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 33.

Tytuł:

Wind influence on the formation of nearshore currents in the southern Baltic: mumerical modelling results

Autorzy:

Sokolov, A.
Chubarenko, B.

Powiązania:

https://bibliotekanauki.pl/articles/241238.pdf

Data publikacji:

2012

Wydawca:

Polska Akademia Nauk. Instytut Budownictwa Wodnego PAN

Tematy:

currents
waves
numerical modelling
coastal zone
Baltic Sea

Opis:

A two-dimensional numerical model was used for a simulation of vertical average longshore currents generated by both wind friction and wind-wave action in the nearshore zone. The modelling domain includes the southern part of the Baltic Proper (all boundaries were closed). Wind, uniform in space and varying in time, was the only forcing in the model. The correlation coefficient higher than 0.8 was obtained by model calibration versus the field measurements of currents conducted at the Lubiatowo field station (southern Baltic) during about 1.5 months in 2006. Comparative simulations of total currents including both wind-induced drift and wave components, and of total currents including only a wind-induced drift component, showed that the input of the drift component into currents in the nearshore zone is greater than commonly believed. Wind-induced drift strongly dominates outside the zone of wave transformation, and its input into the total resulting currents remains noticeable even in a zone between the shoreline and the depth of the first wave breaking. Thus, wind-induced drift constitutes up to 50% of the resulting longshore currents for longshore winds and no less than 20% of the longshore component of currents for winds at 45 degrees to the longshore direction.

Źródło:

Archives of Hydro-Engineering and Environmental Mechanics; 2012, 59, 1-2; 37-48
1231-3726

Pojawia się w:

Archives of Hydro-Engineering and Environmental Mechanics

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 34.

Tytuł:

Ciliate Mesodinium rubrum in the coastal zone of the southern Baltic Sea (Central Pomerania)
Orzęsek Mesodinium rubrum w strefie brzegowej południowego Bałtyku (Pomorze Środkowe)

Autorzy:

Rychert, K.
Pączkowska, M.

Powiązania:

https://bibliotekanauki.pl/articles/85017.pdf

Data publikacji:

2012

Wydawca:

Akademia Pomorska w Słupsku

Opis:

The abundance and biomass of Mesodinium rubrum was assessed in the coastal zone of the southern Baltic Sea near the town of Ustka. The two-year study permitted estimating the mean annual biomass of M. rubrum, which was 2.8 3gC l-1 and 3.1 3gC l-1 in 2006 and 2007, respectively. During the year, abundance changed irregularly with the highest values observed during spring (April-June). The standing crops estimated correspond well with the biomass of this ciliate observed in other regions of the Baltic Sea.
Mesodinium rubrum Lohmann 1908 (= Myrionecta rubra Jankowski 1976) to pospolity orzęsek występujący w wodach słonych i słonawych. Zgodnie z aktualnymi ustaleniami jest on miksotrofem odżywiającym się drogą fotosyntezy prowadzonej w przetrzymywanych kryptofitach, jest on jednakże również zdolny do fagocytozy. M. rubrum jest najczęściej obserwowanym orzęskiem w Morzu Bałtyckim, ze względu jednak na to, że jest on funkcjonalnym autotrofem zalicza się go do fitoplanktonu. Prezentowane badania miały na celu uzupełnienie wiedzy na temat sezonowego występowania M. rubrum w południowej części Morza Bałtyckiego na stanowisku badawczym w pobliży miasta Ustka (54º35′N, 16º50′E). Istnienie tego typu danych umożliwia obserwację długofalowych zmian zachodzących w efekcie działania wielkoskalowych procesów, takich jak eutrofizacja oraz globalne ocieplenie. Badania prowadzono od kwietnia 2006 do kwietnia 2008, pobierając łącznie 30 prób podczas wszystkich pór roku. Próby utrwalano kwaśnym płynem Lugola i analizowano pod mikroskopem odwróconym za pomocą metody Utermöhla. Biomasa M. rubrum zmieniała się dość nieregularnie. Najniższą biomasę notowano zimą, natomiast jej szczytowy wzrost obserwowano w okresie kwiecień-czerwiec. Najwyższą wartość (12,7 3gC l-1) zaobserwowano w czerwcu 2006 roku. Średnioroczna biomasa dla okresu pomiędzy kwietniem 2006 a kwietniem 2007 wynosiła 2,8 3gC l-1. Podobną wartość (3.1 3gC l-1) określono również dla następnego okresu (IV 2007 – IV 2008). Wartości te są podobne do średniorocznej biomasy określonej dla wód otwartego Bałtyku oraz Zatoki Kilońskiej. Jednocześnie są niższe niż średnioroczna biomasa obliczona dla bardziej żyznych rejonów Bałtyku, takich jak Basen Arkoński czy też Basen Gdański.

Źródło:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 2012, 16
1643-0115

Pojawia się w:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 35.

Tytuł:

Suitability Study for Tourism Sites in the Southern Coast of West Java

Autorzy:

Ramdhani, Fajri
Liyantono, Liyantono
Pramono, Gatot
Faizal, Ibnu

Powiązania:

https://bibliotekanauki.pl/articles/1031294.pdf

Data publikacji:

2021

Wydawca:

Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN

Tematy:

Coastal Tourism
India Ocean
Indonesia
Mapping
West Java

Opis:

Diversity of tourist attraction of the regencies/cities in West Java provides an alternative for travellers. One of the potential activity that can be utilized is coastal tourism. The main objective of this research was to provide a suitable site for tourism sites which can be used as a guide for government, private and planners to decide for the development of coastal tourism. Furthermore, visitors can use this application to get information about the beach resources—primary data in tabular data form and secondary data in vector format and satellite imagery format. ArcGIS was used for spatial analysis of thematic. Simple Additive Weighting method was used in this research to rank the factors and to calculate the weight in each factor. This method was commonly used for resolving spatial decision-making problems. The decision-maker directly assigns a weight of relative importance to each factor. There were 32 beach sites visited in the survey with 20 sites of suitable category and 12 sites belonging to a very suitable category. Pangandaran Regency has the most beach site at ten beaches (32.5%), consisting of 7 sites of suitable category and three sites of very suitable category. They are followed by Sukabumi which has nine sites, consisting of 7 sites of suitable category and two sites of very suitable category. The least number of sites were found in Cianjur regency, which only has three sites, consisting of 1 suitable site and two very suitable sites. According to the result, it can be seen that tourism was more developed in Pangandaran and Sukabumi regency. Besides the infrastructure support, natural conditions also influence the development of coastal tourism in the area.

Źródło:

World News of Natural Sciences; 2021, 34; 127-143
2543-5426

Pojawia się w:

World News of Natural Sciences

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 36.

Tytuł:

Identifying the main sources of silicate in coastal waters of the Southern Gulf of Valencia (Western Mediterranean Sea)

Autorzy:

Sospedra, J.
Niencheski, L.F.H.
Falco, S.
Andrade, C.F.F.
Attisano, K.K.
Rodilla, M.

Powiązania:

https://bibliotekanauki.pl/articles/48753.pdf

Data publikacji:

2018

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

silicon
coastal water
Valencia Gulf
Mediterranean Sea
salinity
discharge
nutrient
marine environment

Opis:

Silicon is a major nutrient for siliceous primary producers, which can become a potential limiting nutrient in oligotrophic areas. Most of the silicon inputs to the marine environment come from continental discharges, from both superficial and ground waters. This study analyses the main sources of silicon and their dynamics along the southernmost 43 km of shoreline in the Gulf of Valencia (Western Mediterranean Sea). The salinity and silicate concentration in the different compartments (springs, freshwater wells, beach groundwater, surf zone and coastal waters) in this coastal area were determined. In addition, chlorophyll a and phytoplankton community were analyzed in the surf zone and coastal waters. Silicate concentrations in freshwater wells ranged between 130 and 150 μM, whereas concentrations of this nutrient declined to 49 μM in freshwater–seawater mixture transects. At the same time, there was a positive gradient in silicate for both freshwater and coastal waters southward. An amount of 18.7 t of dissolved silicate was estimated in the nearest first kilometre nearest to the coastline, 6 t of this silicate belonged to the background sea level. On the other hand, the sum of the main rivers in the area supplies 1.6 t of dissolved silicate per day. This implies that a large amount of the remaining 11.1 t must derive from submarine groundwater discharges, which would thus represent 59% of the coastal dissolved silicate budget. Overall, it is suggested that a subterranean transport pathway must contribute considerably to silicate concentrations throughout this zone, which is characterized as permeable.

Źródło:

Oceanologia; 2018, 60, 1
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 37.

Tytuł:

Ice thrusts and piles on the shores of the Southern Baltic Sea coast (Poland) lagoons
Nasunięcia i spiętrzenia lodowe na brzegach zalewów polskiego wybrzeża Bałtyku

Autorzy:

Girjatowicz, J.P.

Powiązania:

https://bibliotekanauki.pl/articles/84907.pdf

Data publikacji:

2004

Wydawca:

Akademia Pomorska w Słupsku

Tematy:

ice thrust
ice pile
shore
Southern Baltic Sea
coastal zone
Polska
lagoon
Szczecin Lagoon
Vistula Lagoon

Źródło:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline; 2004, 08
1643-0115

Pojawia się w:

Baltic Coastal Zone. Journal of Ecology and Protection of the Coastline

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 38.

Tytuł:

Reconstruction of palaeoecological changes in Lake Łebsko on the basis diatom analysis (the southern Baltic coast, Poland)

Autorzy:

Staszak-Piekarska, A.
Rzodkiewicz, M.

Powiązania:

https://bibliotekanauki.pl/articles/294304.pdf

Data publikacji:

2015

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

coastal lakes
diatom communities palaeoreconstructions
Gardno-Łeba Lowland

Opis:

This study focuses on diatom assemblages occurring in core Łeb1 of Late-glacial and Holocene deposits from Lake Łebsko, off the southern coast of the Baltic Sea. Diatom-inferred environmental characteristics, e.g., water level, water salinity (conductivity), trophic status and pH, from the Holocene are presented. In the sediments from the early Boreal/early Atlantic period, an increase in the participation of brackish-freshwater species is observed, as well as increased numbers of Chaetoceros spores in the samples. The Atlantic sediments of Lake Łebsko mirror conditions typical of the Littorina Sea phase during the development of the Baltic Sea (from c. 7,500 BP to c. 5,000 BP). However, communities of that period dominated by fresh-brackish water species suggest the relatively low salinity of the waters. The presence of isolated frustules of Terpsinoë americana and other typically marine species, e.g., Mastogloia smithii, and the occurrence of silts with Cardium shell detritus point to the Littorina transgression and the functioning of a lagoon within the area of present-day Lake Łebsko. During Subboreal occurrence, a higher number of brackish-freshwater diatoms corresponds to an increase in the water level of the Baltic Sea (approximately 3,000 14C BP). Changes in diatom community structure imply a close relationship with the climate controlled eustatic rise of ocean level and the consequent Littorina transgression, as with other southern Baltic Sea localities.

Źródło:

Landform Analysis; 2015, 29; 81-90
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 39.

Tytuł:

Variability of currents over the southern slope of the Gulf of Finland

Autorzy:

Suhhova, I.
Pavelson, J.
Lagemaa, P.

Powiązania:

https://bibliotekanauki.pl/articles/48946.pdf

Data publikacji:

2015

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

stratification
upwelling
downwelling
Finland Gulf
coastal sea water
seasonal thermocline
current velocity

Źródło:

Oceanologia; 2015, 57, 2
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 40.

Tytuł:

Microphytobenthic primary production on exposed coastal sandy sediments of the Southern Baltic Sea using ex situ sediment cores and oxygen optodes

Autorzy:

Kuriyama, K.
Grundling-Pfaff, S.
Diehl, N.
Woelfel, J.
Karsten, U.

Powiązania:

https://bibliotekanauki.pl/articles/2078927.pdf

Data publikacji:

2021

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

microphytobenthos
primary production
sandy sediment
coastal water
benthic diatom
oxygen consumption
oxygen production
respiration
hydrodynamics
Baltic Sea

Opis:

The shallow coastal water zone of the tide-less southern Baltic Sea is dominated by exposed sandy sediments which are typically inhabited by microphytobenthic communities, but their primary production is poorly studied, and hence four stations between 3.0 and 6.2 m depth were investigated. Sediment cores were carefully taken to keep the natural layering and exposed in a controlled self-constructed incubator. Respiratory oxygen consumption and photosynthetic oxygen production were recorded applying planar oxygen optode sensors. We hypothesized that with increasing water depths the effects of wind- and wave-induced erosion and mixing of the upper sediment layer are dampened and expected higher microphytobenthic biomass and primary production in the incubated cores. Our data partly confirm this hypothesis, as cores sampled at the most exposed stations contained only 50% chlorophyll a m−2 compared to the deeper stations. However, primary production was highly variable, probably due to fluctuating sediment-disturbing conditions before the cores were taken. Due to these physical forces sand grains were highly mobile and rounded, and small epipsamic benthic diatoms dominated, which preferentially occurred in some cracks and crevices as visualized by scanning electron microscopy. The data fill an important gap in reliable production data for sandy sediments of the southern Baltic Sea, and point to the ecological importance and relevant contribution of microphytobenthic communities to the total primary production of this marine ecosystem. Oxygen planar optode sensor spots proved to be a reliable, sensitive and fast detection system for ex situ oxygen exchange measurements in the overlying water of intact sediment cores.

Źródło:

Oceanologia; 2021, 63, 2; 247-260
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 41.

Tytuł:

Kartografia 4D w strefie brzegowej południowego Bałtyku - zadanie państwowej służby geologicznej
Integrated geological mapping of the coastal zone of the southern Baltic Sea - task of the Polish Geological Survey

Autorzy:

Uścinowicz, Grzegorz

Powiązania:

https://bibliotekanauki.pl/articles/20225724.pdf

Data publikacji:

2023

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

morze Bałtyckie
strefa przybrzeżna
interakcje ląd-morze
mapowanie geologiczne
Baltic Sea
coastal zone
land-sea interactions
geological mapping

Opis:

The research task Geological integrated coastal zone mapping concerns the recognition and visualization of the geological structure of the Polish coastal zone, enriched with the modelling of erosion-accumulation processes, including prediction of changes in the position of the shoreline and identification of geohazards. It has been running since 2012 and implements multi-instrumental research methods. To date, a total length of about 155 km of the Polish coastal zone has been studied in an area of about 621 km 2 . The main results of the work are presented in the form of maps (e.g., lithogenetic, hydrogeological, geohazard), models (e.g., morpho-geological, hydrodynamic, predictive) and specialized analyses (e.g., morphodynamical, slope stability). In general, the work carried out is done for a utilitarian purpose, i.e. aimed at the practical use of environmental information. According to the standards of the Polish Geological Survey, most of the geological data acquired can be geoprocessed.

Źródło:

Przegląd Geologiczny; 2023, 71, 3; 138-144
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 42.

Tytuł:

Effects of atmospheric circulation on water temperature along the Southern Baltic Sea coast

Autorzy:

Girjatowicz, J.P.
Swiatek, M.

Powiązania:

https://bibliotekanauki.pl/articles/48210.pdf

Data publikacji:

2019

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

atmospheric circulation
water temperature
surface temperature
thermal property
air mass
correlation
Baltic Sea
coastal zone

Źródło:

Oceanologia; 2019, 61, 1
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 43.

Tytuł:

Adenosine triphosphate in the marine boundary layer in the Southern Baltic Sea

Autorzy:

Pryputniewicz, D.
Falkowska, L.
Burska, D.

Powiązania:

https://bibliotekanauki.pl/articles/48770.pdf

Data publikacji:

2002

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

organic matter
marine boundary
adenosine triphosphate
coastal water
vertical distribution
spring
microlayer
Baltic Sea
marine ecosystem

Opis:

Changes in adenosine triphosphate (ATP) concentration were measured in the offshore and coastal waters of the GdańskBasi n in spring. As regards the vertical distribution, it was found that high ATP concentrations occurred mainly in the euphotic layer (above the thermocline) and near the bottom (below the halocline). The high concentrations of ATP in the euphotic layer resulted from primary and secondary production, while the other maximum was due to the presence of bacteria actively degrading organic matter. Changes in ATP concentration in the euphotic layer were closely correlated with the phase of the day. An increase in ATP concentrations in the surface microlayer was observed in the evening and at night, probably as a result of heterotroph proliferation. During daylight, ATP production was inhibited by increasing radiation, hence its concentrations in the sea surface microlayer were considerably lower. Strong winds exerted a significant influence on ATP concentrations in the surface microlayer and in the subsurface water. Windstress depressed ATP concentrations. The biomass of living microorganisms in the microlayer was comparable with the microbiomass beneath the halocline.

Źródło:

Oceanologia; 2002, 44, 4
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 44.

Tytuł:

Variability and correlations of shoreline and dunes on the Southern Baltic coast (CRS Lubiatowo, Poland)

Autorzy:

Pruszak, Z.
Ostrowski, R.
Schonhofer, J.

Powiązania:

https://bibliotekanauki.pl/articles/48165.pdf

Data publikacji:

2011

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

variability
correlation
shoreline
dune
Baltic coast
Lubiatowo
Polska
field investigation
coastal zone
wave energy

Opis:

The paper analyses the results of field investigations into the evolution of the shoreline and dune toe positions in a multi-bar, dissipative coastal zone. The correlations between the changes in the shoreline and the dune toe range from −0.4 to 0.8. It is most often the case that the dune toe is stable while the shoreline moves. Consistent cross-shore migration is slightly more likely to happen than the divergent or convergent movements of both lines. Shoreline retreat and advance attain respective rates of 0.7 m day−1 and 0.4 m day−1. Deep-water wave energy of about 50 kJ m−1 constitutes the boundary between shore accumulation and erosion.

Źródło:

Oceanologia; 2011, 53, 1
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 45.

Tytuł:

Seasonal pattern of the chlorophyll-a in a coastal lagoon from the Southern Baja California (Mexico), described with in situ observations and MODIS-Aqua imagery

Autorzy:

Jimenez-Quiroz, M.C.
Martell-Dubois, R.
Cervantes-Duarte, R.
Cerdeira-Estrada, S.

Powiązania:

https://bibliotekanauki.pl/articles/2078912.pdf

Data publikacji:

2021

Wydawca:

Polska Akademia Nauk. Instytut Oceanologii PAN

Tematy:

chlorophyll a
coastal lagoon
remote sensing
transitional zone
climatology
seasonal pattern
phytoplankton biomass
distribution
multivariate statistical method
MODIS-Aqua data

Opis:

This study aims to estimate, with a climatology perspective, the average seasonal pattern of phytoplankton biomass (SP-PBavg) and its distribution in Bahia Magdalena (Mexico) as a baseline to evaluate PB changes in future studies. This lagoon is in a semi-arid region, lacks river discharges, and channels with vegetation are limited at the north and south zones. SP-PBavg was estimated with chlorophyll-a (chl-a) data obtained in 21 sites on daily MODISAqua imagery (2002—2013; n = 2,418) from a ready-to-use public database. The first step was to establish criteria to use imagery and validate with in situ observations taken in 14 sites (2002—2011; n = 312). MODIS-Aqua overestimated chl-a (mean ± confidence interval95: 5.09 ± 0.97 mg m−3; n = 225); with differences among sites. There were no differences near the inlet lagoon (p <0.05), where the water characteristics are Case-1 while values were significantly higher in the eastern shore and two or three times higher in the mouth of north and south channels, whose water characteristics are similar to Case-2. Multivariate statistical methods allow defining zones into the lagoon and describe their SP-PBavg with both in situ and MODIS Aqua data, but the former’s sample size was small, and the patterns were only delineated. In the inlet surroundings, chl-a peaks from March/April to June/July. On the eastern shore, where MODIS Aqua and in situ data were correlated, despite concentration differences, chla is higher from March/April to October, with peaks in June and September. In the mouth of internal channels, chl-a was higher than other sites and during a longer period; however, the very high MODIS-Aqua values suggest that the satellite also detects organic matter supplied by phytoplankton and other vegetables, which explain the high lagoon’s productivity. These results validate the use of MODIS Aqua imagery to describe the chl-a seasonal patterns in the sea’s vicinity

Źródło:

Oceanologia; 2021, 63, 3; 329-342
0078-3234

Pojawia się w:

Oceanologia

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 46.

Tytuł:

Benthic Foraminiferal Assemblages and Biotopes in a Coastal Lake: the Case Study of Lake Varano (Southern Italy)

Autorzy:

Frontalini, Fabrizio
Margaritelli, Giulia
Francescangeli, Fabio
Rettori, Roberto
Du Châtelet, Eric Armynot

Powiązania:

https://bibliotekanauki.pl/articles/763429.pdf

Data publikacji:

2013

Wydawca:

Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego

Tematy:

benthic foraminifera, biotopes, sediment, Lake Varano, Italy

Opis:

The benthic foraminiferal assemblages in Lake Varano (southern Italy) have been investigated in detail. Statistical analyses enable us to recognize two main biotopes and five sub-biotopes that reflect different ecological and environmental conditions. The assemblages mainly seem to be influenced by the hydrological (namely salinity) and sediment conditions in the lake. These biotopes are characterized by specific sub-assemblages and variations in relative species’ abundances. The Outer Lake Biotope is affected by marine influence and is dominated by the foraminiferal species Ammonia beccarii, Ammonia parkinsoniana and Aubignyna perlucida, which are more common in open water environments. In contrast, the Inner-Marginal Lake Biotope reflects more restricted conditions where low salinity values and sand are associated with high numbers of miliolids. These two main biotopes are thus subjected to different degrees of confinement and water residence times, both of which are related to the water exchange time of the lake with the Adriatic Sea. In addition five sub-biotopes (Intermediate Marine, Mixing, “Urban”, Marginal, and Innermost) represented by particular foraminiferal assemblages are identified that characterize particular sub-environments. These sub-biotopes are, to some extent, separated by salinity gradients as well as the grain-size and the organic matter of sediments.

Źródło:

Acta Protozoologica; 2013, 52, 3
1689-0027

Pojawia się w:

Acta Protozoologica

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 47.

Tytuł:

Potential Use of Mangroves as Nature-Based Solutions to Improve Navigation Conditions in a Port in Southern Brazil

Autorzy:

Previti, L. S.
Alfredini, P.

Powiązania:

https://bibliotekanauki.pl/articles/24201478.pdf

Data publikacji:

2023

Wydawca:

Uniwersytet Morski w Gdyni. Wydział Nawigacyjny

Tematy:

navigation
fluid mud
coastal ecosystem
mangroves
wetlands
port engineering
nature based solutions
deforestation

Opis:

Mangroves and the associated shoal forest known as ‘restinga' are ecosystems of great ecological relevance that play a significant role in the protection of the coastline in tropical regions. In Brazil, the coastal region has been severely affected by urban expansion. The Paranaguá Port, located in Paraná State (Brazil), is the fourth most important Brazilian port in throughput, and is located in an estuarine region which features large mangrove forests. An historical assessment of its inner access channel dredging rates was made to assess the impacts that the expansion of the Port in the last 30 years may have caused to the ecosystem. In the following, the historical data concerning the dredged volume in the inner access channel was compared to the mangrove and the shoal forest associated variation, aiming to establish a potential correlation between vegetation and siltation in the inner access channel to show as the preservation or restoration of specific ecosystems has potential to Nature-Based Solutions.

Źródło:

TransNav : International Journal on Marine Navigation and Safety of Sea Transportation; 2023, 17, 3; 507--513
2083-6473
2083-6481

Pojawia się w:

TransNav : International Journal on Marine Navigation and Safety of Sea Transportation

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 48.

Tytuł:

Określenie tendencji rozwojowych brzegu na podstawie badań teledetekcyjnych
Trends in coast development as determined by remote sensing research

Autorzy:

Dudzińska-Nowak, J.

Powiązania:

https://bibliotekanauki.pl/articles/131202.pdf

Data publikacji:

2008

Wydawca:

Stowarzyszenie Geodetów Polskich

Tematy:

strefa brzegowa
zmiany brzegowe
teledetekcja
Bałtyk południowy
coastal zone
coastline changes
remote sensing
Southern Baltic

Opis:

Obserwowane w ostatnich latach na świecie sukcesywne nasilanie się procesów erozji brzegu (Zawadzka 1999, Pruszak 2003, Living with erosion... 2004) powoduje coraz szersze zainteresowanie naukowców, reprezentujących różne dziedziny nauki, problemami strefy brzegowej. Jednakże złożoność zachodzących na brzegu morskim procesów, ich przyczyn i uwarunkowań, stwarza poważne problemy w ich opisie. Wielokrotnie podejmowane próby wyjaśnienia mechanizmów reakcji zachodzących w strefie brzegowej, jak do tej pory, nie dały zadowalających wyników. Poznanie prawidłowości rozwoju linii brzegowej ma kluczowe znaczenie dla rozwoju regionalnego i zagospodarowania przestrzennego, szczególnie w aspekcie bezpieczeństwa brzegu i jego infrastruktury, a także planowania rozwiązań prawnych i finansowych w odniesieniu do obszarów zagrożonych zniszczeniem. Wykorzystanie w badaniach metod teledetekcyjnych może przyczynić się do wyznaczenia obszarów ulegających morfodynamicznym procesom erozji i akumulacji, a co za tym idzie do poznania prawidłowości rozwoju brzegu. Szczególnie do tego celu przydatne są przetworzone fotogrametrycznie zdjęcia lotnicze, które pozwalają na przeprowadzenie szczegółowych, krótko- i długookresowych obserwacji obejmujących swoim zasięgiem znaczny obszar. Celem prezentowanych badań było odtworzenie położenia linii podstawy wydmy / podnóża klifu wybrzeża Gminy Rewal w latach 1938, 1951, 1973 i 1996 oraz określenie na tej podstawie wielkości zmian i tendencji rozwojowych brzegu. W wyniku przeprowadzonych pomiarów określono wielkość i tempo zmian zachodzących w tym rejonie. Wykazano wyraźny charakter erozyjny analizowanego wybrzeża. Zaobserwowano znaczne zróżnicowanie wielkości zmian nawet na sąsiadujących ze sobą, jednorodnych geomorfologicznie, odcinkach brzegu. Wyznaczenie szczególnie zagrożonych odcinków brzegu, o znacznej wielkości i dynamice zmian erozyjnych, ma duże znaczenie zarówno dla samorządów lokalnych, jak i instytucji odpowiedzialnych za bezpieczeństwo brzegu, szczególnie w aspekcie obserwowanego nasilania się zjawiska erozji.
In the last years, the intensity of erosion processes have been observed worldwide (Zawadzka 1999, Pruszak 2003, Living with erosion...2004). Consequently, coastal zone problems have become a focus of interest for researchers representing different scientific disciplines. The complexity of processes operating in the coastal zone, their causes, and effects are very difficult to describe and analyse. Previous efforts to explain interactions between the litho-, hydro-, and atmosphere were not successful. Using remote sensing data makes it possible to collect short- and long-time observation series on coastline changes, whereby coast development processes may be followed. Photogrammetric georeferenced aerial photographs, taken in different years, supply short and long-term observation series. The area of study was a 20 km long stretch of the western Polilsh coast in the Rewal municipality (Maritime Bureau km 380-360). Analyses were carried out based on 4 series of aerial photograph taken in 1938, 1951, 1973, and 1996. The 1996 series was used to develop an orthophotomap, which was subsequently used to calibrate the remaining series (1938, 1951, and 1973). The dune base /cliff foot line was identified on every picture in each year. The changes in the location was calculated in different time spans (1938-51, 1951-73, 1973-96). Results of the calculations were used to analyse trends in the coast development and the rate of the changes; classification of dynamics changes was effected as well. Based on coastline change diagrams for 1938-1951, 1951-1973 and 1973-96, the magnitude of coast accretion and erosion in the area were analysed. As indicated by the results obtained, the Rewal municipality coast is erosive. In all the periods analysed, a substantial diversity of the magnitude of changes was observed, even in neighbouring, morphologically homogenous areas. The temporal analysis indicates an increase in the length of the coast affected by erosion; at the same time, the accretion area has been reduced; the accumulative sections of the coast have become shorter and shorter. The situation recorded in aerial photographs represents a net effect of coastal processes, so measurements taken indirectly incorporate effects of every factor that produced changes in the dune base /cliff foot line position in an individual period, e.g., sea level changes, storm surge damages, impacts of coastal defence structure (link side effect), and other human activities. Application of aerial photographs to measurements of dune base line changes makes it possible to look for patterns in coastline development. Identification of dangerous sections of the coast, affected by heavy coastal erosion and high dynamics of changes is very important for spatial planning, coastal protection, and ther activities, particularly in the part of the coast exposed to erosion hazard.

Źródło:

Archiwum Fotogrametrii, Kartografii i Teledetekcji; 2008, 18a; 99-109
2083-2214
2391-9477

Pojawia się w:

Archiwum Fotogrametrii, Kartografii i Teledetekcji

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 49.

Tytuł:

The first geological record of a palaeotsunami on the southern coast of the Baltic Sea, Poland

Autorzy:

Rotnicki, K.
Rotnicka, J.
Goslar, T.
Wawrzynniak-Wydrowska, B.

Powiązania:

https://bibliotekanauki.pl/articles/2059831.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Baltic Sea
onshore tsunami deposits
age of tsunami
Holocene coastal changes
meteorite impact

Opis:

Tsunami deposits were unknown along the southern coast of the Baltic Sea for a long time. The results of present research provided evidence of high-energy event layers. They occur on the bottom of two hemispherical hollows that are cut into glaciolimnic silt and glaciofluvial sand and gravel from the Late Weichselian Age. The event deposits are represented by poorly sorted marine sand with admixtures of pebbles and allochthonous detritus of biogenic origin: marine, brackish and occasionally freshwater shells and shell debris of molluscs and snails, plant macrofossils from the marine nearshore zone, shreds and lumps of peaty material, gyttja and organogenic silt, lumps of charcoal, wood pieces and tree branches and trunks. All these features are commonly considered indicative of tsunamis. The age of the biogenic detritus found in the tsunami layer ranges from 10 390 to 6 630 cal. yr BP, whereas the oldest gyttja covering the event layers is 6 600 cal. yr BP old. This means that the tsunami occurred between 6 630 and 6 600 cal. yr BP. Various causes of tsunami event have been taken into consideration, including the impact of meteorites within the coastal plain and the littoral zone of the southern Baltic Sea.

Źródło:

Geological Quarterly; 2016, 60, 2; 417--440
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 50.

Tytuł:

A groundwater flow model for the Wolin Island area, including glaciotectonic deformation

Autorzy:

Hoc, R.
Sadurski, A.
Wiśniowski, Z.

Powiązania:

https://bibliotekanauki.pl/articles/94492.pdf

Data publikacji:

2018

Wydawca:

Uniwersytet im. Adama Mickiewicza w Poznaniu

Tematy:

GIS
groundwater modeling
groundwater exploitation
coastal hydrogeology
southern Baltic Sea coast
modelowanie wód gruntowych
eksploatacja wód podziemnych
hydrogeologia
Morze Bałtyckie

Opis:

During the construction of mathematical models for mapping hydrogeological conditions it is necessary to apply simplifications, both in the geological structure and in hydrogeological parameters used. The present note discusses problems surrounding the mapping of glaciotectonic disturbances that occur in the northern part of Wolin Island (northwest Poland). For this part of the island, a direct outflow of groundwater towards the Baltic Sea basin has been determined on the basis of geophysical survey results. An important feature in the hydrogeological conditions here is the isolation of groundwater from both the Baltic Sea and Szczecin Lagoon by clay with a Cretaceous xenolith. Such a geological structure explains the presence of perched water at considerable heights in zones close to the cliffs, without any significant hydraulic connection with surrounding reservoirs. Hydrogeological conditions of Wolin Island have been modelled using the Visual MODFLOW package v.4.2. In the vertical section, these conditions can be simplified to one aquifer (Pleistocene-Holocene), in which two aquifers can be distinguished. In a large part of the island, these remain in mutual hydraulic contact: layer I – upper, with an unconfined aquifer, and layer II – lower, with a confined aquifer, locally an unconfined one. The schematisation of hydrogeological conditions adopted here has allowed to reproduce present groundwater dynamics in the study area.

Źródło:

Geologos; 2018, 24, 3; 207-216
1426-8981
2080-6574

Pojawia się w:

Geologos

Dostawca treści:

Biblioteka Nauki

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