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Wyświetlanie 1-15 z 135
Tytuł:
Factors regulating bacterial abundance in Antarctic coastal and shelf waters
Autorzy:
Zdanowski, Marek K.
Powiązania:
https://bibliotekanauki.pl/articles/2052461.pdf
Data publikacji:
1998
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
heterotrophic bacteria
protozooplankton
phytoplankton
krill
organic matter
temperature
sea water
freshwater
Źródło:
Polish Polar Research; 1998, 19, 3-4; 169-180
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmiany temperatury powierzchni Morza Barentsa w latach 1951-2006
Changes in the sea surface temperature of the Barents Sea in the years 1951-2006
Autorzy:
Zblewski, S.
Powiązania:
https://bibliotekanauki.pl/articles/260773.pdf
Data publikacji:
2007
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
temperatura powierzchni morza
NAO
Morze Barentsa
Prąd Zachodniospitsbergeński
Prąd Nordkapski
sea surface temperature
Barents Sea
West Spitsbergen Current
North Cape Current
Opis:
Praca charakteryzuje zmiany temperatury powierzchni Morza Barentsa (TPM) zachodzące w okresie 1951–2006. Stwierdzono występowanie słabych, dodatnich i istotnych statystycznie trendów TPM w gridach leżących poza obszarem bezpośredniego oddziaływania ciepłych prądów morskich. Odnotowano słaby i nierównomiernie rozłożony w przestrzeni wzrost temperatury powierzchni morza – silniejszy we wschodniej części Morza Barentsa. W badanym okresie (1951–2006) na obserwowaną zmienność rocznej TPM znacznie silniejszy wpływ wywierają procesy oceaniczne niż zmienność zimowej cyrkulacji atmosferycznej.
The aim of this work was to analyse monthly and annual values of sea surface temperatures of the Barents Sea in the years covering the period from 1951 up to 2006 averaged to chosen grids 2x2° (Fig. 1).The analysis showed that in the course of SST a clearly marked period (1976–1988) of significant decrease in annual values of water temperature was noted, with the minimum observed in 1980 (Fig. 2). This phenomenon is connected with Great Salinity Anomaly.The research showed that the general decrease in annual SST takes place towards north-east and at the same time, following the same direction, the increase in amplitude of inter-annual changes can be observed (Fig. 3). ‘The warm sources of the North Cape Current and West Spitsbergen Current moving away and the transfer of heat from the ocean to the atmosphere are the cause of this situation. This significant drop in annual sea surface temperature in the NE part of the Barents Sea is also influenced by flows of cold and fresh Surface Arctic Waters from the Arctic and Kara seas. There were also great differences observed in the course of annual SST in the western and eastern parts of the examined sea area. (Fig.4). In the eastern part rapid falls in water temperature can be noted by even 0.7°C from year to year. They result from the sea ice spreading and Surface Arctic Waters from the Kara Sea and from the north region of the Barents Sea which cut off the flow of heat from the deeper parts of the sea towards the surface and to the atmosphere.In the examined period weak positive trends in the annual sea surface temperature were observed and they are statistically significant in almost all grids (Tab.1). The strongest trends were noted in the east part of the examined sea area. Positive and statistically significant trends of the monthly SST are observed in summer and autumn in grids located farthest NE.The analysis showed that the influence of winter atmospheric circulation on the temperature of the sea surface is weak or rather moderate (Tab. 2) and that the observed changeability in annual sea surface temperature of the Barents Sea is mainly controlled by oceanic processes.
Źródło:
Problemy Klimatologii Polarnej; 2007, 17; 61-70
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmiany temperatury powierzchni Morza Czukockiego (1982-2008)
Changes of sea surface temperature at the Chukchi Sea (1982-2008)
Autorzy:
Zblewski, S.
Marsz, A. A.
Powiązania:
https://bibliotekanauki.pl/articles/261049.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Morze Czukockie
temperatura powierzchni morza
cyrkulacja atmosferyczna
sea surface temperature
atmospheric circulation
Opis:
Praca charakteryzuje zmiany temperatury powierzchni Morza Czukockiego zachodzące w okresie 1982-2008 oraz wpływ na te zmiany cyrkulacji atmosferycznej. Stwierdzono występowanie dodatnich, istotnych statystycznie, miesięcznych i rocznych trendów temperatury powierzchni morza (TPM), nierównomiernie rozłożonych w przestrzeni. Obserwuje się występowanie asynchronicznych związków między cyrkulacją atmo-sferyczną a TPM, przy czym zmiany cyrkulacji atmosferycznej wyprzedzają w czasie zmiany TPM. W badanym okresie najsilniejszy wpływ na miesięczne i roczne zmiany TPM ma charakter cyrkulacji atmosferycznej występu-jącej w dłuższych okresach – wiosną, a nawet w całym okresie marzec-sierpień i marzec-wrzesień, poprzedzającym moment wystąpienia maksimum temperatury powierzchni morza. Wpływ cyrkulacji atmosferycznej na zmiany TPM nie jest bezpośredni, lecz realizuje się poprzez wpływ na dryf lodów na Morzu Czukockim w okresie wiosen-nym i letnim.
This work characterizes changes in sea surface temperature of the Chukchi Sea observed in the period 1982- 2008 and the way atmospheric circulation (mid-troposphere circulation, modified Arctic Dipole) influences these changes. The research made use of homogeneous data series of sea surface temperature (SST) originating from the data set NOAA NCDC ERSST v.2, in a 2�‹. x 2�‹�É grid (Fig. 1). In the examined period (1982-2008) the increase in sea surface temperature of the Chukchi Sea was observed (Table 1). In the central and southern part of the sea the increase in SST is much stronger (+0.067 deg/year) than in the northern part (0.002 deg/year). This phenomenon is connected with the fact that the northern part of the examined sea area was freed from ice only after the year 2002. During the observed period there was also mean annual increase in SST ranging from 0.62�‹C in the south-west part to 0.03�‹C in the northern part of the examined region (Fig. 2). In the period 1982-2008 strong, statistically significant correlations between SST and the character of the atmospheric circulation observed before were noted. The correlations of SST in the Chukchi Sea are stronger than those with the modified Artic Dipole. The changeability of value of the modified Arctic Dipole from March to September explains 36% (in the eastern part of the sea area) and up to 46% (in the western part) of annual changeability in SST. However the influence of changes in atmospheric circulation on the changeability of SST is not direct. The character of atmospheric circulation noted in spring season (III-V) and even during the entire spring and summer seasons (III-VIII) has influence on the ice drifting in the Chukchi Sea. The drifting ice has influence on the time during which the sea surface accumulates the heat and as a consequence affects the sea surface temperature. This sequence of consecutive correlations seems to be most important for the changes in the SST. The secondary role affecting the changes in SST in the Chukchi Sea plays the increased transport of warm water from the Bering Sea forced by strong positive phases of modified Arctic Dipole in September. This influence is limited to the area up to the southern part of the Chukchi Sea and to the time till the last three months (October-December).
Źródło:
Problemy Klimatologii Polarnej; 2009, 19; 147-158
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Fast separation and detection of main components in complex raw biological materials using temperature-controlled planar micro-chromatography (micro-TLC)
Szybkie rozdzielanie i detekcja głównych składników złożonych materiałów biologicznych za pomocą mikrochromatografii planarnej (micro-TLC) prowadzonej w warunkach kontrolowanej temperatury
Autorzy:
Zarzycki, P. K.
Ślączka, M. M.
Zarzycka, M. B.
Włodarczyk, E.
Baran, M. J.
Heese, T.
Głód, B. K.
Powiązania:
https://bibliotekanauki.pl/articles/158415.pdf
Data publikacji:
2010
Wydawca:
Stowarzyszenie Inżynierów i Techników Mechaników Polskich
Tematy:
chromatografia planarna
micro-TLC
liofilizacja
żółć ryb
troć wędrowna (Salmo trutta m. trutta)
kwasy żółciowe
spirulina
preparaty farmaceutycze
detekcja fluorymetryczna
kwas fosforomolibdenowy
temperatura
frakcjonowanie
fingerprinting
planar chromatography
lyophilization
fish bile
sea trout (Salmo trutta m. trutta)
bile acids
pharmaceutical formulations
fluorimetric detection
phosphomolybdic acid
temperature
fractionation
Opis:
This paper is a continuation of our previous research focusing on development of micro-TLC methodology. The main goal of present paper is to demonstrate the separation and detection capability of micro-TLC technique involving simple analytical protocols without multi-steps sample pre-purification. In present studies components of interest were isolated from biological samples including fish bile and spirulina cells. Described methodology can be applied for fast fractionation or screening of target substances as well as chemo-taxonomic studies and fingerprinting of complex mixtures, which are present in raw biological or environmental samples.
Chromatografia cienkowarstwowa jest powszechnie wykorzystywaną metodą analityczną stosowaną w rozdzielaniu substancji obecnych w złożonych próbkach biologicznych, środowiskowych oraz preparatach farmaceutycznych. Związane jest to głównie z prostotą sprzętu, możliwością jednoczesnej analizy wielu próbek w trakcie jednego procesu analitycznego. Dodatkowo, istotna jest możliwość bezpośredniego analizowania złożonych próbek bez ich wstępnego oczyszczenia. Obecna publikacja jest kontynuacją badań dotyczących zastosowania mikrochromatografii planarnej prowadzonej w warunkach kontrolowanej temperatury (rys. 1). W szczególności, w pracy wykazano potencjał analityczny mikrochromatografii planarnej w rozdzielaniu złożonych próbek, bez potrzeby ich uprzedniego wieloetapowego oczyszczania.Jako materiały badane wykorzystano spirulinę oraz żółć rybią (rys. 2 - 4). Wykazano, iż detekcja analitów może być znacząco poprawiona poprzez umieszczenie uprzednio rozwiniętych płytek chromatograficznych w parach jodu lub poprzez wybarwienie plamek odczynnikiem wywołującym (kwasem fosforomolibdenowym). Niskocząsteczkowe substancje z próbek środowiskowych (wody z jezior, ścieki surowe oraz oczyszczone) były zatężane przy pomocy ekstrakcji do fazy stałej. Badania wykazały obecność szeregu pasm na mikrochromatogramach cienkowarstwowych, które są specyficzne dla poszczególnych ekosystemów wodnych Pomorza Środkowego. Opisana metodologia może znaleźć zastosowanie w szybkim frakcjonowaniu oraz oznaczaniu ilościowym substancji niskocząsteczkowych pochodzących ze złożonych materiałów biologicznych, jak również w badaniach przesiewowych dużej ilości próbek środowiskowych (rys. 5 - 8).
Źródło:
Pomiary Automatyka Kontrola; 2010, R. 56, nr 4, 4; 360-364
0032-4140
Pojawia się w:
Pomiary Automatyka Kontrola
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A more accurate formula for calculating the net longwave radiation flux in the Baltic Sea
Autorzy:
Zapadka, T.
Wozniak, B.
Dera, J.
Powiązania:
https://bibliotekanauki.pl/articles/47558.pdf
Data publikacji:
2007
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
temperature
cloud
radiation flux
water vapour
atmosphere
long-wave radiation
sea surface
Baltic Sea
Źródło:
Oceanologia; 2007, 49, 4
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Longwave radiation budget at the Baltic Sea surface from satellite and atmospheric model data
Autorzy:
Zapadka, T.
Krezel, A.
Wozniak, B.
Powiązania:
https://bibliotekanauki.pl/articles/47597.pdf
Data publikacji:
2008
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
air temperature
sea surface
heat budget
Baltic Sea
temporal analysis
spatial analysis
long-wave radiation
cloud cover
model data
Opis:
The net longwave radiation flux LW↑↓ in the Baltic Sea in 2001 has been subjected to spatial and temporal analysis. Maps of the mean monthly LW↑↓ over the Baltic were drawn using the new semi-empirical formula for the Baltic Sea (Zapadka et al. 2007). The input data for the formula, such as sea surface and air temperatures, and cloud cover, were obtained from the Tiros N/NOAA and METEOSAT 7 satellites and from the UMPLfo recast model (see http://meteo.icm.edu.pl). The mean annual LW↑↓ for 2001 was estimated at 63 W m−2 and compared with available data from other sources. The monthly maps of the net flux LW↑↓ over the Baltic show that the total values reach a minimum (LW↑↓≈50 W m−2) in April, September, October and a maximum (LW↑↓≈80 W m−2) in November. The statistical error of daily maps, on which the monthly maps were based, is no more than 18 W m−2.
Źródło:
Oceanologia; 2008, 50, 2; 147-166
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sea surface temperature retrieval from MSG-SEVIRI data in the Baltic Sea area
Autorzy:
Wozniak, M.
Krezel, A.
Powiązania:
https://bibliotekanauki.pl/articles/47694.pdf
Data publikacji:
2010
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
sea surface temperature
Baltic Sea
algorithm
mid-latitude region
spatial resolution
regression analysis
surface temperature
marine environment
climate change
Opis:
The aim of the paper was to confirm the proposition that the classical SST algorithms MCSST and NLSST originally prepared for AVHRR data could also be used for Meteosat/SEVIRI data with satisfactory accuracy in the mid-latitude region, where the spatial resolution is about 7×7 km. The research was performed in the southern Baltic Sea (between 13◦E 53◦N and 21◦E 58◦N). Data were collected in all the seasons of 2007. The coefficients were found by means of regression analysis. SSTs determined on the basis of AVHRR data were used in the regression analysis instead of in situ data. A set of paired AVHRR and SEVIRI images spaced no more than 8 minutes apart were compared. The results show that the method is capable of producing sea surface temperatures with a statistical error (standard deviation) of 1◦C.
Źródło:
Oceanologia; 2010, 52, 3; 331-344
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Biodiversity of the Arctic Ocean in the face of climate change
Autorzy:
Weslawski, J.M.
Powiązania:
https://bibliotekanauki.pl/articles/11979.pdf
Data publikacji:
2011
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
biodiversity
Arctic Ocean
climate change
global climate change
Arctic sea
aquatic ecosystem
Arctic environment
sea water
water temperature
salinity level
Opis:
Global climate changes which has been observed over the recent years affects organisms occurring in the Arctic seas and the functioning of the whole maritime ecosystems there. The research note presents and briefly analyses the biological diversity of the Arctic Ocean and the most important factors which change the relations between organisms and the environment in the Arctic.
Źródło:
Papers on Global Change; 2011, 18
2300-8121
1730-802X
Pojawia się w:
Papers on Global Change
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Distribution and role of the genus Oithona (Copepoda: Cyclopoida) in the South China Sea
Autorzy:
Wang, L.
Du, F.
Wang, X.
Li, Y.
Ning, J.
Powiązania:
https://bibliotekanauki.pl/articles/47786.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
Oithona
Copepoda
Cyclopoida
temperature
hydrological factor
phytoplankton
ichthyoplankton
South China Sea
Oithona plumifera
Oithona similis
Opis:
The relationships between the small cyclopoid copepod Oithona and hydrological factors, phytoplankton and ichthyoplankton were evaluated using the data obtained in the central South China Sea (SCS) in summer 2014. The genus abundance ranged from 6.00 ind. m3 to 93.75 ind. m3 with high abundance band occurring in the branch of SCS Monsoon Jet. The lower temperature and higher salinity in the surface water of the band than other zones indicated that deep water intrusion was a positive factor for aggregation of the genus. The community structure of the genus was dominated by Oithona plumifera and Oithona similis made up 97% of the genus abundance associated with Oithona tenuis. The result of db-RDA analysis showed that the community structure of the genus was affected by temperature, Chl a, larval fishes and fish spawns, and temperature was the most important limiting factor. The result of GAMs analysis showed that abundance of O. tenuis, and copepodites were affected by Chl a, larval fishes and fish spawns; abundance of O. similis was affected by Chl a and fish spawns; and abundance of O. plumifera was affected by Chl a and larval fishes. Therefore, we suggest that the branch of SCS Monsoon Jet and deep water intrusion favor aggregation of plankton in the central SCS in summer. We confirm that the temperature is the limiting factor to the reproduction of the genus Oithona in tropic seas and the genus Oithona is a food-web linker between primary production and larval fishes in the central SCS.
Źródło:
Oceanologia; 2017, 59, 3
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Oceanographic observations in the Nordic Sea and Fram Strait in 2016 under the IO PAN long-term monitoring program AREX
Autorzy:
Walczowski, W.
Beszczynska-Moller, A.
Wieczorek, P.
Merchel, M.
Grynczel, A.
Powiązania:
https://bibliotekanauki.pl/articles/48885.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
Nordic Sea
Fram Strait
spatial distribution
salinity
water temperature
Atlantic water
physical oceanography
monitoring programme
Opis:
Since 1987 annual summer cruises to the Nordic Seas and Fram Strait have been conducted by the IO PAN research vessel Oceania under the long-term monitoring program AREX. Here we present a short description of measurements and preliminary results obtained during the open ocean part of the AREX 2016 cruise. Spatial distributions of Atlantic water temperature and salinity in 2016 are similar to their long-term mean fields except for warmer recirculation of Atlantic water in the northern Fram Strait. The longest observation record from the section N along 768300N reveals a steady increase of Atlantic water salinity, while temperature trend depends strongly on parametrization used to define the Atlantic water layer. However spatially averaged temperature at different depths indicate an increase of Atlantic water temperature in the whole layer from the surface down to 1000 m.
Źródło:
Oceanologia; 2017, 59, 2
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Distribution of phytoplankton along the thermohaline gradient in the North-Eastern Adriatic channel; winter aspect
Autorzy:
Vilicic, D.
Kuzmic, M.
Bosak, S.
Silovic, T.
Hrustic, E.
Buric, Z.
Powiązania:
https://bibliotekanauki.pl/articles/47482.pdf
Data publikacji:
2009
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
Adriatic Sea
chlorophyll
diatom
dinoflagellate
distribution
nutrient
oligotrophic water
phytoplankton composition
picoplankton
salinity
temperature
thermohaline
transition zone
water transparency
Opis:
The distribution of phytoplankton and its relation to the hydrographic features in the north-eastern Adriatic was investigated in February 2008. The area of interest included a thermohaline gradient in the channel situated between the coast and the islands lying parallel to the coast. The gradient is controlled by the influx of oligotrophic karstic riverine water at the south-eastern end,subma rine springs in the middle part,an d warmer offshore waters at the north-western end of the channel. The change of temperature and salinity in the estuarine transition zone was accompanied by abundant diatoms and dinoflagellates below the halocline,with dominant chain-forming diatoms (Chaetoceros, Bacteriastrum) in abundances reaching 5×105 cells dm−3. The impact of coastal submarine springs detected by infrared remote sensing resulted in the growth of cyanobacteria in the nitrogen-depleted surface waters. The greater contribution of picoplankton, as well as of nanoplanktonic coccolithophorids and cryptophytes,in the outer channel system indicated their preference for oligotrophic conditions. Flow cytometric counts of nanophytoplankton were 10–30 times greater than inverted microscope counts. Cyanobacteria were about five times more abundant than picoeukaryotes. The study demonstrates how different techniques (remote sensing and in situ investigations) can be useful in understanding the biological and hydrographic set-up in the specific oligotrophic eastern Adriatic coastal environment.
Źródło:
Oceanologia; 2009, 51, 4
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New coupled atmosphere-ocean-ice system COSMO-CLM/NEMO: assessing air temperature sensitivity over the North and Baltic Seas
Autorzy:
Van Pham, T.
Brauch, J.
Dieterich, C.
Frueh, B.
Ahrens, B.
Powiązania:
https://bibliotekanauki.pl/articles/48930.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
coupled atmosphere-ocean-ice system
temperature sensitivity
air temperature
Baltic Sea
North Sea
regional climate modelling
COSMO-CLM model
Źródło:
Oceanologia; 2014, 56, 2
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Monitoring the effect of upwelling on the chlorophyll a distribution in the Gulf of Finland (Baltic Sea) using remote sensing and in situ data
Autorzy:
Uiboupin, R.
Laanemets, J.
Sipelgas, L.
Raag, L.
Lips, I.
Buhhalko, N.
Powiązania:
https://bibliotekanauki.pl/articles/48503.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
spatio-temporal variability
chlorophyll a
distribution
variability
upwelling
Baltic Sea
Finland Gulf
sea surface temperature
remote sensing
spatial distribution
ecological status
satellite image
Opis:
The spatio-temporal variability of chlorophyl a (Chl a) caused by a sequence of upwelling events in the Gulf of Finland in July–August 2006 was studied using remote sensing data and field measurements. Spatial distributions of sea surface temperature (SST) and Chl a concentration were examined using MODIS and MERIS data respectively. The MERIS data were processed with an algorithm developed by the Free University of Berlin (FUB) for case 2 waters. Evaluation of MERIS Chl a versus in situ Chl a showed good correlation (r2 = 0.67), but the concentration was underestimated. The linear regression for a 2 h window was applied to calibrate MERIS Chl a. The spatio-temporal variability exhibited the clear influence of upwelling events and related filaments on Chl a distribution in the western and central Gulf. The lowest Chl a concentrations were recorded in the upwelled water, especially at the upwelling centres, and the highest concentrations (13 mg m−3) were observed about two weeks after the upwelling peak along the northern coast. The areas along the northern coast of upwelled water (4879 km2) on the SST map, and increased Chl a (5526 km2) two weeks later, were roughly coincident. The effect of upwelling events was weak in the eastern part of the Gulf, where Chl a concentration was relatively consistent throughout this period.
Źródło:
Oceanologia; 2012, 54, 3
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Effects of global climate oscillations on intermonthly to interannual variability of sea levels along the English Channel Coasts (NW France)
Autorzy:
Turki, I.
Massei, N.
Laignel, B.
Shafiei, H.
Powiązania:
https://bibliotekanauki.pl/articles/2079277.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
sea level
interannual variability
storm
atmospheric circulation
climatic oscillation
sea surface temperature
sea level pressure
North Atlantic oscillation
English Channel
Opis:
This work examines the multiscale variability in sea level along the English Channel coasts (NW France) using a wavelet multiresolution decomposition of water level values and climate oscillations in order to gain insights in the connection between the global atmospheric circulation and the local-scale variability of the monthly extreme surges. Changes in surges have exhibited different oscillatory components from the intermonthly (~3–6-months) to the interannual scales (~1.5-years, ~2–4-years, ~5–8-years) with mean explained variances of ~40% and ~25% of the total variability respectively. The correlation between the multiresolution components of surges and 28 exceptional stormy events with different intensities has revealed that energetic events are manifested at all timescales while moderate events are limited to short scales. By considering the two hypotheses of (1) the physical mechanisms of the atmospheric circulation change according to the timescales and (2) their connection with the local variability improves the prediction of the extremes, the multiscale components of the monthly extreme surges have been investigated using four different climate oscillations (Sea Surface Temperature (SST), Sea-Level Pressure (SLP), Zonal Wind (ZW), and North Atlantic Oscillation (NAO)); results show statistically significant correlations with ~3–6-months, ~1.5-years, ~2–4-years, and ~5–8-years, respectively. Such physical links, from global to local scales, have been considered to model the multiscale monthly extreme surges using a time-dependent Generalized Extreme Value (GEV) distribution. The incorporation of the climate information in the GEV parameters has considerably improved the fitting of the different timescales of surges with an explained variance higher than 30%. This improvement exhibits their nonlinear relationship with the large-scale atmospheric circulation.
Źródło:
Oceanologia; 2020, 62, 2; 226-242
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Diurnal and seasonal DOC and POC variability in the land-locked sea
Autorzy:
Szymczycha, B.
Winogradow, A.
Kulinski, K.
Koziorowska, K.
Pempkowiak, J.
Powiązania:
https://bibliotekanauki.pl/articles/48956.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
marine environment
organic matter
seasonal change
diurnal change
particulate organic carbon
dissolved organic carbon
chlorophyll a
salinity
pH
temperature
Baltic Sea
Opis:
Organic matter is a minor yet important component of the marine environment. The aim of this study was to investigate the diurnal and seasonal changes in dissolved and particulate organic carbon (DOC and POC, respectively). Thus, DOC and POC as well as chlorophyll a (Chl a), δ13C, NO3−, NO2−, NH4+, PO43−, salinity, pH, and temperature were regularly measured in samples collected for 24 h (2-h resolution) in the Gdańsk Deep (54°44.730′N, 19°08.531′E) at three water depths (1, 10, and 40 m) during sampling campaigns in 2011 (May), 2014 (May), and 2015 (January, March, May, July, September, November). Seasonal variations in DOC and POC followed the seasonality of Chl a (proportional trend) and nutrients (reverse trend) concentrations. Diurnal oscillations were detected in six out of the eight measurement series. The strongest diurnal variability in both POC and DOC occurred in May 2011 and March 2015, when phytoplankton activity was highest (high Chl a). The surprisingly low δ13C values (range: −28‰ to −24‰) measured over the course of the study revealed the gaps in our knowledge of the isotopic characteristics of terrestrial- vs. marine-derived particulate organic matter.
Źródło:
Oceanologia; 2017, 59, 3
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 135

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