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    Wyświetlanie 1-12 z 12
    Tytuł:
    The major Baltic inflow in January 2003 and preconditioning by smaller inflows in summer-autumn 2002: a model study
    Autorzy:
    Meier, H.E.M.
    Doscher, R.
    Broman, B.
    Piechura, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/48684.pdf
    Data publikacji:
    2004
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    climate variability
    numerical modelling
    bottom boundary layer
    Baltic Sea
    major inflow
    Baltic inflow
    Opis:
    Using the results of the Rossby Centre Ocean model (RCO) the Baltic inflows in summer/autumn 2002 and January 2003 have been studied. The model results were extracted from a long simulation with observed atmospheric forcing starting in May 1980. In RCO a bottom boundary layer model was embedded. Both the smaller inflows and the major inflow in January 2003 are simulated in good agreement with observations. We found that a total of 222 km3 water entered the Baltic in January; the salinity of 94 km3 was greater than 17 PSU. In August/September 2002 the outflow through the Sound and inflow across the Darss Sill were simulated. The net inflow volume amounted to about 50 km3.
    Źródło:
    Oceanologia; 2004, 46, 4
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Inflow waters in the deep regions of the Southern Baltic Sea - transport and transformations
    Autorzy:
    Piechura, J.
    Beszczynska-Moller, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/47562.pdf
    Data publikacji:
    2004
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    transport
    temperature
    deep region
    transformation
    Baltic Sea
    inflow water
    mixing
    Opis:
    A medium-sized inflow (about 200 km3 according to IOW data, - personal communication) of saline water into the southern Baltic Sea occurred during January 2003. Unlike any previously observed inflow, this one brought very cold water, of temperatures around 1-2oC and less. Since the temperature of the deep water in the southern Baltic before the inflow was exceptionally high (11-12oC), the inflowing waters produced dramatic changes and a steep temperature gradient. The movement of the inflowing waters through the deep basins and channels of the Baltic Sea from the Arkona Basin to the Gdańsk Deep during next 4-8 months is described. Frequent mesoscale structures and intensive mixing followed the eastward transport of the inflow water, particularly in the Bornholm Deep and Słupsk Furrow. The present paper is based on data collected during 6 cruises r/v "Oceania" between December 2002 and August 2003. The last cruise in August took place in order to assess the long-term consequences of the inflow.
    Źródło:
    Oceanologia; 2004, 46, 1
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Warm waters of summer 2002 in the deep Baltic Proper
    Autorzy:
    Feistel, R.
    Nausch, G.
    Mohrholz, V.
    Lysiak-Pastuszak, E.
    Seifert, T.
    Matthaus, W.
    Kruger, S.
    Hansen, I.S.
    Powiązania:
    https://bibliotekanauki.pl/articles/47540.pdf
    Data publikacji:
    2003
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    temperature
    hydrography
    inflow
    warm water
    summer
    salinity
    Baltic Sea
    oxygen condition
    Opis:
    From October 2002 until March 2003 surprisingly warm, oxygenated waters were frequently encountered in the Baltic Sea in the area between the Bornholm and Fårö Deeps from the halocline down to the bottom. Owing to their ventilation effect in the stagnating deep waters, their occasional observations have partly been incorrectly attributed to the inflow events of October 2002 or January 2003. The emergence of some of these waters can be traced back to the exceptional summer weather conditions in August and September 2002 in central Europe. The warm waters played a remarkable renewal pacemaker role for the subsequent important winter inflow of January 2003. The evolution of this summer inflow is described and possible causes are discussed.
    Źródło:
    Oceanologia; 2003, 45, 4
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Evidence for a warm water inflow into the Baltic Proper in summer 2003
    Autorzy:
    Feistel, R.
    Nausch, G.
    Heene, T.
    Piechura, J.
    Hagen, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/48845.pdf
    Data publikacji:
    2004
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    Gotland Basin
    temperature
    hydrography
    inflow
    warm water
    Baltic Sea
    oxygen condition
    climate change
    Opis:
    The exceptional warm water inflow into the Baltic Sea in summer 2002, which preceded the major Baltic inflow of January 2003, was surprisingly repeated in modified form in summer 2003. Its warm waters even replaced the renewed, cold inflow waters in the eastern Gotland Basin and commenced another warm period in its deep layers, where the previous one had lasted from 1997 to 2003. Details of the temporal and spatial behaviour of this new baroclinic inflow are presented from various measurements carried out from the Kiel Bight up to Gotland, covering the Darss Sill, the Arkona, Bornholm, Gdańsk Basins and the Słupsk Channel, focused mainly on the time period between July 2003 and July 2004. Hypothetically, the repetition of these exceptional warm inflow events could be regarded as a possible regional indicator for global climatic change.
    Źródło:
    Oceanologia; 2004, 46, 4
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Temporal and spatial evolution of the Baltic deep water renewal in spring 2003
    Autorzy:
    Feistel, R.
    Nausch, G.
    Matthaus, W.
    Hagen, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/48009.pdf
    Data publikacji:
    2003
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    temporal evolution
    inflow
    spring
    deep water renewal
    Baltic Sea
    oxygen condition
    spatial evolution
    Opis:
    In January 2003, a deep-water renewal process in the Baltic Sea commenced with an inflow of about 200 km3 of cold and well oxygenated water from the Kattegat, half of which was of salinity >17 PSU; it is considered to be the most important inflow since 1993. Related front propagation and the ventilation of anoxic waters between the western and the central Baltic were recorded by the Darss Sill measuring mast, the Arkona Basin buoy, a subsurface mooring in the Eastern Gotland Basin, and hydrographic research cruises conducted in January, February, March, May and August 2003. Already in May, the central Gotland Basin was reached by water with near-bottom oxygen concentrations among the highest ever recorded there. A comprehensive review of the observed spatial and temporal structures together with additional background data is presented. Estimates of the intensity of the present inflow are discussed.
    Źródło:
    Oceanologia; 2003, 45, 4
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Inflow waters in the deep regions of the Southern Baltic Sea - transport and transformations
    Autorzy:
    Piechura, J.
    Beszczynska-Moller, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/48744.pdf
    Data publikacji:
    2003
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    transport
    temperature
    hydrography
    deep region
    transformation
    environment
    salinity
    Baltic Sea
    ecosystem
    inflow water
    mixing
    Opis:
    A medium-sized inflow (about 200 km3 according to IOW data, – personal communication) of saline water into the southern Baltic Sea occurred during January 2003. Unlike any previously observed inflow, this one brought very cold water, of temperatures around 1–2◦C and less. Since the temperature of the deep water in the southern Baltic before the inflow was exceptionally high (11–12◦C), the inflowing waters produced dramatic changes and a steep temperature gradient. The movement of the inflowing waters through the deep basins and channels of the Baltic Sea from the Arkona Basin to the Gdańsk Deep during next 4–8 months is described. Frequent mesoscale structures and intensive mixing followed the eastward transport of the inflow water, particularly in the Bornholm Deep and Słupsk Furrow. The present paper is based on data collected during of 6 cruises r/v ‘Oceania’ between December 2002 and August 2003. The last cruise in August took place in order to assess the long-term consequences of the inflow.
    Źródło:
    Oceanologia; 2003, 45, 4
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Unusual Baltic inflow activity in 2002-2003 and varying deep-water properties
    Autorzy:
    Feistel, R.
    Nausch, G.
    Hagen, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/48654.pdf
    Data publikacji:
    2006
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    Sopot
    temperature
    inflow
    residence time
    deep water renewal
    conference
    salinity
    Baltic Sea
    Baltic Monitoring Programme
    Opis:
    The unusual sequence of inflow events into the Baltic Sea that occurred in 2002 and 2003 includes the first ever important baroclinic inflow to be described (August 2002), the Major Baltic Inflow (January 2003), which gave rise to the highest oxygen levels in the Gotland Deep since the 1930s, and the baroclinic inflow (August 2003) that elevated the Gotland Basin deep water salinity to values last observed in 1977, and caused the surface salinity to rise again. From these trend changes, salt residence times were estimated at about 20 years in the deep waters and 30 years above the pycnocline. Ventilation of the remote Karlsö Deep took until 2005, two years after the inflow event responsible, at a time when the Bornholm and Eastern Gotland Basins were already returning to stagnation.
    Źródło:
    Oceanologia; 2006, 48, S
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Wpływ wlewów z Morza Północnego do Morza Bałtyckiego na rozwój stada dorsza.
    The impact of inflows from the North Sea to the Baltic Sea on the development of a cod stock.
    Autorzy:
    Wodzinowski, Tycjan
    Radtke, Krzysztof
    Nadolna-Ałtyn, Katarzyna
    Szymanek, Lena
    Witalis, Bartosz
    Powiązania:
    https://bibliotekanauki.pl/chapters/2118885.pdf
    Data publikacji:
    2016
    Wydawca:
    Morski Instytut Rybacki - Państwowy Instytut Badawczy
    Tematy:
    wlew słonych wód
    Morze Bałtyckie
    tarło dorsza
    Baltic Sea
    cod spawning
    inflow of saline water
    Opis:
    Wlewy słonej wody z Morza Północnego są zjawiskiem o dużym znaczeniu dla Morza Bałtyckiego. Decydują o zmianie stosunków zasoleniowych i tlenowych, często także temperaturowych na obszarach i głębokościach zasiedlonych przez dorsza. Mogą wpływać na sukces reprodukcyjny ryb tego gatunku, nie są jednak jedynym czynnikiem wpływającym na sam proces reprodukcji. Porównując zapisy historyczne, widać, że od połowy lat 90. XX w. wlewy zaczęły być zjawiskami incydentalnymi. Brak wlewów prowadzi do utrwalenia pionowej stratyfikacji gęstościowej, a co za tym idzie – do stagnacji wody, szczególnie przy dnie, na głębokościach poniżej halokliny. W konsekwencji następuje zmniejszenie się zawartości rozpuszczonego tlenu w tej warstwie wód Morza Bałtyckiego. W obecnej chwili można stan taki uznać za sytuację normalną. Skutkiem stagnacji wody poniżej halokliny w dłuższym okresie jest zwiększenie się obszarów hipoksji, a nawet anoksji. Następstwem tego zjawiska jest zmniejszanie się zasięgu bytowania dorszy w Bałtyku, co w konsekwencji prowadzi do zagęszczenia stada i wzrostu konkurencji o pokarm, mających wpływ na kondycję ryb tego gatunku. W odniesieniu do postępu stagnacji wody nie bez znaczenia dla sukcesu rozrodczego dorszy jest również przesuwanie w czasie występowania szczytu tarła z maja i pierwszej połowy czerwca na koniec lipca i sierpień.
    The inflows of saline water from the North Sea are a phenomenon of great importance to the Baltic Sea. They decide about the salinity and oxygen relations, often also about the temperature in the areas and depths inhabited by cod. They may affect the reproduction success of fish of this species, but they are not the only factor influencing the very process of reproduction. Comparing the historical records, it can be seen that since the mid-90s inflows began to be incidental phenomena. The lack of inflows leads to consolidation of the vertical density stratification, and thus the stagnation of water especially at the bottom at depths below the halocline. As a consequence, a reduction in the dissolved oxygen content in this layer of the Baltic Sea occurs. At the moment, such a state can be considered a normal situation. The stagnant water below the halocline in the long term results in the expansion of areas of hypoxia, or even anoxia. The consequence of this phenomenon is a limited range of cod distribution in the Baltic Sea, which in turn leads to the stock concentration in these areas and increased competition for food, affecting the condition of fish. With respect to the progress of water stagnation, shifting the time of the spawning peak from May and the first half of June to the end of July and August is not without significance for the reproduction success of cod.
    Źródło:
    95-lecie Morskiego Instytutu Rybackiego: aktualne tematy badań naukowych. Tom I. Zasoby ryb i rybołówstwo; 35-41
    9788361650164
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Dissolved oxygen variability in the Southern Baltic Sea in 2013—2018
    Autorzy:
    Rak, D.
    Walczowski, W.
    Dzierzbicka-Glowacka, L.
    Shchuka, S.
    Powiązania:
    https://bibliotekanauki.pl/articles/2079094.pdf
    Data publikacji:
    2020
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    dissolved oxygen concentration
    oxygenation
    sea water
    water column
    surface layer
    seasonal cycle
    major inflow
    Baltic Sea
    Opis:
    This paper discusses changes in the dissolved oxygen concentration (DOC) in the southern Baltic Sea. The oxygenation of the whole water column was estimated. Monthly mean DOCs, as well as a detailed description of the annual surface layer dissolved oxygen (DO) cycle, are presented. The DO cycle at the surface is characterized by two maxima in March/April and November, and by two minima in July/August and December. The DO decline time after the major Baltic inflow (MBI) in 2014 was estimated at about 10 months for the Bornholm Deep and Słupsk Furrow. Whereas the Bornholm Basin was relatively well oxygenated, low oxygen concentrations (<4 mg l−1) were measured in the deep layer of the Gdańsk Deep throughout the inflow period. In addition, the cod spermatozoa activation layer together with the neutral egg buoyancy layer for the Bornholm Basin and Słupsk Furrow are discussed on the basis of the measured DOCs and the variability in hydrographic conditions.
    Źródło:
    Oceanologia; 2020, 62, 4PA; 525-537
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Argo floats in the Southern Baltic Sea
    Autorzy:
    Walczowski, W.
    Merchel, M.
    Rak, D.
    Wieczorek, P.
    Goszczko, I.
    Powiązania:
    https://bibliotekanauki.pl/articles/2079087.pdf
    Data publikacji:
    2020
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    dissolved oxygen
    inflow
    monitoring system
    Polish Exclusive Economic Zone
    Agro float
    Baltic Sea
    measurement technique
    innovative activity
    Opis:
    This work aims to familiarize the reader with issues related to modern oceanographic measurement techniques performed by Argo autonomous profiling floats. The opportunity for this is the three years of innovative activity on the part of Argo-Poland in the Baltic Sea. Based on the experience and results acquired by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN), we can say that a revolution in the Baltic Sea monitoring is underway. During three years of activity, the floats launched by IO PAN provided more than 1600 CTD profiles, including 600 O2 profiles. Together with synoptic data from ships, data from moorings and surface buoys, the Argo float measurements are an important part of the southern Baltic monitoring system. Two Argo floats launched by IO PAN collected enough data to determine the dynamics of the oxygen content in various layers, the extent of hypoxic and anoxic zones, and to detect small baroclinic inflows to the Gotland and Gdańsk Deeps.
    Źródło:
    Oceanologia; 2020, 62, 4PA; 478-488
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Distinctive features of water exchange across the Słupsk Sill (a full-scale experiment)
    Autorzy:
    Paka, V.
    Golenko, N.
    Korzh, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/47795.pdf
    Data publikacji:
    2006
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    Sopot
    water exchange
    thermohaline structure
    Slupsk Sill
    saline water
    conference
    Baltic Sea
    high-resolution transect
    inflow water
    brackish water
    Opis:
    The flows of brackish waters in the upper layer and saline waters in the lower layer meet above the Słupsk Sill, which makes this one of the most significant features of the Baltic Sea, controlling as it does the ventilation of the deep basins in its central region. Earlier high-resolution measurements using towed scanning probes conducted here for more than ten years had revealed the complexity and variability of the water dynamics in this area. Mapping surveys repeated in quick succession are needed to study the water exchange in such an area. A survey of this kind was attempted in October 2003 during the 57th cruise of the r/v ‘Professor Shtokman’. Three surveys were carried out in the areas of the Słupsk Sill, the eastern Bornholm Basin, and the western Słupsk Furrow by means of a scanning probe towed along closely-spaced transects. The water structure around the sill was different each time, despite the rather short time gaps between the surveys. As follows from the data analysis, during the first survey, the saline Bornholm waters flowed over the sill as an axially symmetrical jet and entrained the adjacent freshened cold waters of the intermediate layer. In ten days, this joint flow displaced to the southern flank of the sill and propagated in the Słupsk Furrow along its southern border, with the dense core of saline waters gradually moving over the bottom to the northern border. Concurrently, the contrary flow of the main volume of cold freshened waters, originating from northern areas and leaving the Baltic Sea, was pushed away from the southern wall of the furrow and blocked at a significant distance from the sill. In three days, the blocked waters forced their way through towards its northern flank. Just below these waters, waters of elevated salinity were found above the eastern slope of the sill at the depth of its ridge, while waters of a similar salinity occurred below the depth of the ridge above the western slope of the sill. There were no indications of intensive overflow in the central and southern areas of the sill. Accordingly, the return flow of Bornholm waters across the sill became possible.
    Źródło:
    Oceanologia; 2006, 48, S
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The inflow of 234U and 238U from the River Odra drainage basin to the Baltic Sea
    Autorzy:
    Skwarzec, B.
    Tuszkowska, A.
    Borylo, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/47957.pdf
    Data publikacji:
    2010
    Wydawca:
    Polska Akademia Nauk. Instytut Oceanologii PAN
    Tematy:
    Baltic Sea
    Odra River
    Polska
    Szczecin Lagoon
    concentration
    drainage basin
    inflow
    natural radionuclide
    radionuclide
    trace element
    uranium
    water sample
    Opis:
    In this study the activity of uranium isotopes 234U and 238U in Odra river water samples, collected from October 2003 to July 2004, was measured using alpha spectrometry. The uranium concentrations were different in each of the seasons analysed; the lowest values were recorded in summer. In all seasons, uranium concentrations were the highest in Bystrzyca river waters (from 27.81±0.29 Bq m−3 of 234U and 17.82±0.23 Bq m−3 of 238U in spring to 194.76±3.43 Bq m−3 of 234U and 134.88 ± 2.85 Bq m−3 of 238U in summer). The lowest concentrations were noted in the Mała Panew (from 1.33±0.02 Bq m−3 of 234U and 1.06±0.02 Bq m−3 of 238U in spring to 3.52 ± 0.05 Bq m−3 of 234U and 2.59 ± 0.04 Bq m−3 of 238U in autumn). The uranium radionuclides 234U and 238U in the water samples were not in radioactive equilibrium. The 234U/238U activity ratios were the highest in Odra water samples collected at Głogów (1.84 in autumn), and the lowest in water from the Noteć (1.03 in winter and spring). The 234U/238U activity ratio decreases along the main stream of the Odra, owing to changes in the salinity of the river’s waters. Annually, 8.19 tons of uranium (126.29 GBq of 234U and 100.80 GBq of 238U) flow into the Szczecin Lagoon with Odra river waters.
    Źródło:
    Oceanologia; 2010, 52, 4
    0078-3234
    Pojawia się w:
    Oceanologia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-12 z 12

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