Wszystkie pola: sea temperature - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Seasonal Variations of Sea Surface Temperature and Sea Current in the Celebes Sea
Autorzy:: Hapsari, Siti Nirmala
Syamsuddin, Mega Laksmini
Riyantini, Indah
Sunarto, Sunarto
Powiązania:: https://bibliotekanauki.pl/articles/1031483.pdf
Data publikacji:: 2021
Wydawca:: Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:: Celebes Sea
Sea Current
Sea Surface Temperature
Opis:: The waters of the Celebes Sea are an area that has quite complex dynamics because it is influenced by several factors, either regionally or globally. This influence certainly has an impact on variations in oceanographic conditions in waters such as Sea Surface Temperature (SST) and sea currents. Currently, there are many observations of oceanographic data, one of which is by using remote sensing methods. The purpose of this study was to determine the seasonal variations in sea surface temperature and sea surface currents in the Celebes Sea using a remote sensing system in a time series for 5 years (2014-2018). The results of this study indicate data on seasonal variation of SST and sea surface currents have an average maximum SST value for 5 years occurring in the eastern season and the second transitional season (May, June, July) with an average value range of 30.6 °C - 31.1 °C and the average maximum sea current velocity for 5 years occurs in the western monsoon with a value range of 0.72 m/s - 0.77 m/s. The high SST value and sea current velocity are caused by the influence of the season which causes variations in the ongoing rainfall, also presumably due to the opposite direction between the monsoon wind and the direction of the main current flowing in the Celebes Sea.
Źródło:: World News of Natural Sciences; 2021, 35; 135-143
2543-5426
Pojawia się w:: World News of Natural Sciences
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Influence of Indian Ocean Dipole Phenomena Towards the Eddy Variability in Southern Java Ocean
Autorzy:: Rachim, Fadliyan R.
Syamsudin, Mega L.
Riyantini, Indah
Yuliadi, Lintang P. S.
Powiązania:: https://bibliotekanauki.pl/articles/1065419.pdf
Data publikacji:: 2019
Wydawca:: Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:: Automated Eddy Detection
Eddies
IOD
SSH
Sea Temperature
Opis:: The phenomenon of Indian Ocean Dipole (IOD) can influence the variability of eddy in the Southern Java Ocean (SJO). The purpose of this research is to know the characteristics of eddy in the SJO at the time of the IOD condition. The research was conducted in Eastern Indian Ocean (EIO), South of the Java Island by coordinate 0º S – 15º S and 90º E – 120º E. The data used in this research is currents data, sea surface height (SSH) data, and temperature data from HYCOM, and Dipole Mode Index (DMI) data from Japan Marine Science and Technology (JAMSTEC). Methods used for detecting eddy is using the Automated Eddy Detection (AED) method. The results of this research show that the IOD phenomena affect the variability of eddies in the SJO, this is evidenced by the difference of the total eddies is generated at the time of normal conditions and at the time was going to the phenomenon of IOD. Total average eddies on IODM (+) conditions is 153 and on IODM (-) conditions is 144. IODM (+) conditions could cause the value of a central point of sea surface height (SSH) and sea temperature is lower than the normal conditions, the opposite IODM (-) conditions can cause the value of a central point of SSH and sea temperature is higher than the normal conditions.
Źródło:: World Scientific News; 2019, 132; 121-131
2392-2192
Pojawia się w:: World Scientific News
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Overview of Oceanic Eddies in Indonesia Seas Based on the Sea Surface Temperature and Sea Surface Height
Autorzy:: Purba, Noir P.
Faizal, Ibnu
Damanik, Finri S.
Rachim, Fadliyan R.
Mulyani, Putri G.
Powiązania:: https://bibliotekanauki.pl/articles/1031834.pdf
Data publikacji:: 2020
Wydawca:: Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:: Eddies
Indonesia Throughflow
Ocean Fronts
Water Mass
Opis:: One of the complexities of the ocean currents in the territorial waters of Indonesia is oceanic eddies form. Ocean eddy is one of the very crucial phenomena in the ocean due to its circulation and connection with the chemical and biological aspects in the water column. This study aimed to observe the distribution of oceanic eddies associated with the Sea Surface Temperature (SST) and Sea Surface Height (SSH) with the Automatic Eddy Detection (AED) method. The analysis included distribution and types correlated with seasons. The results showed that eddies occur in all regions in the Indonesian Seas except the Java Sea. In general, the occurrence of eddies every month does not differ significantly for both Ocean Cyclonic Eddies (OCE) and Ocean Anticyclonic Eddies (OAE). The total oceanic eddies in a year are around 1,149 events. A minimum radius of the ocean eddies found was about 5.08 km, and a maximum was around 386.76 km. Furthermore, the occurrence of OCE is mostly in locations that are almost the same as OAE. Both types of eddy are mostly in locations with the boundary of temperatures and the boundary of SSH. Several eddies exist every month and mostly change or move into other areas. Eddies in Indonesia seas are influenced by differences of SST and different SSH that form ocean currents. One of the complexities of the ocean currents in the territorial waters of Indonesia is oceanic eddies form. Ocean eddy is one of the very crucial phenomena in the ocean due to its circulation and connection with the chemical and biological aspects in the water column. This study aimed to observe the distribution of oceanic eddies associated with the Sea Surface Temperature (SST) and Sea Surface Height (SSH) with the Automatic Eddy Detection (AED) method. The analysis included distribution and types correlated with seasons. The results showed that eddies occur in all regions in the Indonesian Seas except the Java Sea. In general, the occurrence of eddies every month does not differ significantly for both Ocean Cyclonic Eddies (OCE) and Ocean Anticyclonic Eddies (OAE). The total oceanic eddies in a year are around 1,149 events. A minimum radius of the ocean eddies found was about 5.08 km, and a maximum was around 386.76 km. Furthermore, the occurrence of OCE is mostly in locations that are almost the same as OAE. Both types of eddy are mostly in locations with the boundary of temperatures and the boundary of SSH. Several eddies exist every month and mostly change or move into other areas. Eddies in Indonesia seas are influenced by differences of SST and different SSH that form ocean currents.
Źródło:: World Scientific News; 2020, 147; 166-178
2392-2192
Pojawia się w:: World Scientific News
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Sea surface temperature distribution during upwelling along the Polish Baltic coast
Autorzy:: Krezel, A.
Ostrowski, M.
Szymelfenig, M.
Powiązania:: https://bibliotekanauki.pl/articles/48583.pdf
Data publikacji:: 2005
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: advanced very high resolution radiometer
temperature
upwelling
coastal upwelling
coastal region
sea surface
Baltic Sea
Opis:: Among over 150 maps of sea surface temperature in the Polish Baltic coastal region derived from satellite data during the warm period of the year (April–October) in 2000–2002, 41 cases were noted where its distribution showed characteristic features indicating the occurrence of coastal upwelling. The fundamental parameters of range, probability of occurrence and temperature modification caused by water from deeper sea layers raised by an upwelling event and spreading across the surface were established for three regions (Hel, Łeba and Kołobrzeg). The Kołobrzeg upwelling region had the largest spatial range (up to 5000 km2). The region with the smallest spatial range (Hel, up to 1400 km2) had the largest surface temperature amplitude (to 14◦C), the largest maximum temperature gradient (5◦C km−1) and the largest average sea surface temperature decrease in the centre in relation to the background value.
Źródło:: Oceanologia; 2005, 47, 4
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 5.

Tytuł:: Recent sea surface temperature trends and future scenarios for the Red Sea
Autorzy:: Shaltout, M.
Powiązania:: https://bibliotekanauki.pl/articles/48804.pdf
Data publikacji:: 2019
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: sea surface
sea surface temperature
chlorophyll a
heat exchange
climate model
Red Sea
Źródło:: Oceanologia; 2019, 61, 4
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: Recent sea surface temperature trends and future scenarios for the Mediterranean Sea
Autorzy:: Shaltout, M.
Omstedt, A.
Powiązania:: https://bibliotekanauki.pl/articles/49032.pdf
Data publikacji:: 2014
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Mediterranean Sea
sea surface temperature
temporal distribution
spatial distribution
climate change
heat exchange
cloud cover
variation coefficient
Źródło:: Oceanologia; 2014, 56, 3
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 7.

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

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Skocz do pozycji: 8.

Tytuł:: Sea surface temperature development of the Baltic sea in the period 1990-2004
Autorzy:: Siegel, H.
Gerth, M.
Tschersich, G.
Powiązania:: https://bibliotekanauki.pl/articles/48942.pdf
Data publikacji:: 2006
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Sopot
regional variation
sea surface temperature
seasonal variation
conference
interannual variation
Baltic Sea
trend
Opis:: Sea Surface Temperature (SST) maps derived from NOAA weather satellites for the period 1990–2004 were used to investigate seasonal and inter-annual variations in the Baltic Sea. A comparison between monthly mean SST and in situ measurements at the MARNET station ‘Arkona Sea’ showed good agreement with differences in July and August. Monthly means reflect strong seasonal and interannual variations. The yearly means show a slight positive trend with an increase of 0.8 K in 15 years. In particular, summer and autumn months contribute to this positive trend, with stronger trends in the northern than in the southern Baltic. The winters are characterised by a slightly negative trend. The winter minimum SST in the Arkona Sea correlates best with the WIBIX climate index derived for the Baltic region.
Źródło:: Oceanologia; 2006, 48, S
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 9.

Tytuł:: Annual course of superficial water temperature in the Ezcurra Inlet, King George Island, Antarctica
Autorzy:: Gurgul, Henryk
Stochmal, Wiesław
Szymczak, Wiesław
Powiązania:: https://bibliotekanauki.pl/articles/2052577.pdf
Data publikacji:: 1996
Wydawca:: Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:: Antarctica
South Shetland Islands
sea water temperature
Źródło:: Polish Polar Research; 1996, 17, 1-2; 43-59
0138-0338
2081-8262
Pojawia się w:: Polish Polar Research
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 10.

Tytuł:: Spatial and interannual variations of seasonal sea surface temperature patterns in the Baltic Sea
Autorzy:: Bradtke, K.
Herman, A.
Urbanski, J.A.
Powiązania:: https://bibliotekanauki.pl/articles/48507.pdf
Data publikacji:: 2010
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: spatial variation
interannual variation
sea surface temperature
seasonality
global climate change
thermal season
annual cycle
transitional period
Baltic Sea
Opis:: On the basis of monthly averaged satellite data, this study examined how the annual cycle of the Baltic Sea surface temperature (SST) varied spatially and temporally during the period 1986–2005. We conclude that there are two main thermal seasons in the Baltic Sea separated only by short transitional periods – spring lasting about one month, and autumn lasting two months. Generally speaking, summer covers the part of the year from June to October with the highest monthly mean SST in August. Winter, with a minimum monthly mean SST in February in shallow waters or in March in deeper areas, lasts from December to April. As a result of climate changes over the Baltic Sea region, strong positive trends in SST occur in the summer months. In consequence, the period with extremely high sea surface water temperatures has become slightly longer in the central Baltic. In the last decade winter changes in SST display zero or even negative tendencies. The investigated period was characterized by an annual increase in mean temperatures of about 0.03–0.07◦C. However, the rates of monthly mean SST changes were sometimes more than three times as high.
Źródło:: Oceanologia; 2010, 52, 3; 345-362
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 11.

Tytuł:: Influence of density stratification on effluent plume dynamics
Autorzy:: Loncar, G.
Paklar, G.B.
Janekovic, I.
Powiązania:: https://bibliotekanauki.pl/articles/47653.pdf
Data publikacji:: 2011
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: 3D numerical model
Croatia
density stratification
numerical model
numerical simulation
Rijeka Bay
salinity
sea temperature
statistical analysis
submarine outfall
submarine sewage
Opis:: In this study we modelled sea temperature (T ), salinity (S) and density field dynamics using a 3D numerical model applied to Rijeka Bay (Croatia) in order to explore their effect on effluent plume dynamics in the vicinity of four submarine sewage outfalls when the bora wind (NE direction) is blowing. The vertical density stratification in the area studied is strongly related to the bora wind, which contributes significantly to the lowering of the pycnocline depth through enhanced mixing in the vertical, giving rise to changes in the neutral buoyancy level. The features of near-field plume dynamics were calculated with the use of a separate near-field numerical model, using information on the vertical density distribution previously calculated using a 3D numerical model. The results of the numerical simulations and statistical analysis of the wind data indicate a very low probability of complete water column homogenization and consequent effluent plume rise to the sea surface under the influence of the bora wind during the peak tourist season (May–September).
Źródło:: Oceanologia; 2011, 53, 2
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 12.

Tytuł:: Indian Ocean wind speed variability and global teleconnection patterns
Autorzy:: Sinha, M.
Jha, S.
Chakraborty, P.
Powiązania:: https://bibliotekanauki.pl/articles/2079299.pdf
Data publikacji:: 2020
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: wind speed
variability
sea surface temperature
remote sensing
Indian Ocean
Opis:: The influence of the local sea surface temperature (SST) and remote ENSO (El Niño-Southern Oscillation) indices on the wind speed (WS) data were explored for the Indian Ocean region. Relationships among the parameters were studied using spatial correlation plots and significant correlation ranges. Two months (July and January) representing opposite monsoon phases were selected for analysis for the period 1950–2016. There was a significant negative correlation between WS and SST over the Bay of Bengal (BOB) during July. Although different ENSO indices correlated differently in different areas of the Indian Ocean, the region off the coast of Sri Lanka was most significantly teleconnected. The southwest monsoon locally impacted the WS and SST relationship and the WS parameter was remotely teleconnected in both the monsoon seasons. Further empirical orthogonal function (EOF) analysis was applied on the 67 years WS data of the BOB region to extract the dominant mode representing maximum variability of the total variance. The temporal pattern of the first principal component (PC1) of WS data was linked to the North Atlantic Oscillations in January and the Atlantic Multidecadal Oscillation in July respectively. The continuous wavelet power spectra of the PC1 of WS showed significant regions in the 2–4-year band resembling the ENSO variability. Wavelet coherence applied between PC1 of WS and the ENSO indices showed greatest values for January in the 8–16-year band and for July in the 0–4-year band. A close relationship was established between the WS variability in BOB and the ENSO indices.
Źródło:: Oceanologia; 2020, 62, 2; 126-138
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 13.

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

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Skocz do pozycji: 14.

Tytuł:: Wpływ zmian temperatury wody powierzchniowej mórz Barentsa, Norweskiego i Grenlandzkiego na trend rocznej temperatury powietrza na Spitsbergenie
Influence of changes in sea surface temperature in the Barents, Norwegian and Greenland seas on the annual air temperature trend at Spitsbergen
Autorzy:: Styszyńska, A.
Powiązania:: https://bibliotekanauki.pl/articles/261025.pdf
Data publikacji:: 2011
Wydawca:: Stowarzyszenie Klimatologów Polskich
Tematy:: temperatura powietrza
temperatura powierzchni morza
Spitsbergen
air temperature
sea surface temperature
Opis:: Praca omawia wpływ zmian temperatury wód powierzchniowych (SST - sea surface temperature) mórz Barentsa, Norweskiego i Grenlandzkiego zachodzących w okresie zimowego wychładzania (styczeń-kwiecień) na roczne i sezonowe wartości temperatury powietrza na Spitsbergenie w okresie 1912-2010. Stwierdzono, że zimowa SST rozległej powierzchni mórz otaczających Spitsbergen jest silnie skorelowana z roczną temperaturą powietrza na Spitsbergenie przez kolejne trzy lata (k, k+1, k+2). Powierzchnia akwenów, na których występują opóźnione korelacje z temperaturą powietrza na Spitsbergenie stopniowo zmniejsza się, a siła związków słabnie. Obszary, na których w roku k+2 korelacje utrzymują najwyższą (p < 0.001) istotność odtwarzają szlaki przenosu prądowego. Akwen, na którym zmienność SST z roku k najsilniej koreluje z roczną i zimową temperaturą powietrza na Spitsbergenie w kolejnych trzech latach (k, k+1, k+2) nie zmienia swojego położenia - jest to obszar leżący na pograniczu N części Morza Norweskiego i W części Morza Barentsa - między Bjornoyą a Nordkapem. Długookresowe zmiany temperatury powierzchni mórz wokółspitsbergeńskich regulują długookresową zmienność temperatury powietrza na Spitsbergenie, a występujący w przebiegu rocznej temperatury powietrza trend ma swoją genezę w zmianach zasobów ciepła w wodach tych mórz.
This work discusses the influence of changes in SST (sea surface temperature) of the Barents, Norwegian and Greenland seas occurring during winter cooling (January-April) on annual and seasonal air temperatures at Spitsbergen during 1912-2010. It was found that the winter SST of vast seas surrounding the region of Spitsbergen is strongly correlated with annual and winter air temperature at Spitsbergen during the next three years (k, k+1, k+2). The sea areas, where the delayed correlations with air temperature at Spitsbergen are observed, gradually decrease, and the strength of the correlation decreases. The routes of moving current represent the areas where correlations maintain the highest significance (p <0.001) in the year k+2. The sea area, where variability of SST from year k is most strongly correlated with the annual and winter air temperature at Spitsbergen in the next three years (k, k+1, k+2) does not change its position - this is the area lying on the border of the north part of the Norwegian Sea and the west part of the Barents Sea - between Bjornoya and Nordkap. Long-term sea surface temperature changes of vast seas surrounding the region of Spitsbergen regulate the long-term variability of the air temperature on Spitsbergen, and appearing in the course of the annual air temperature trend has his own genesis in changes of resources of the warmth in waters of these seas.
Źródło:: Problemy Klimatologii Polarnej; 2011, 21; 115-131
1234-0715
Pojawia się w:: Problemy Klimatologii Polarnej
Dostawca treści:: Biblioteka Nauki