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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
Artykuł
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
Artykuł
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
Artykuł
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
Artykuł
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
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:
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
Artykuł
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
Artykuł
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
Artykuł
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
Artykuł
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
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:
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
Artykuł
Tytuł:
Influence of the parametrization of water optical properties on the modelled sea surface temperature in the Baltic Sea
Autorzy:
Stramska, M.
Zuzewicz, A.
Powiązania:
https://bibliotekanauki.pl/articles/49070.pdf
Data publikacji:
2013
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
Baltic Sea
sea surface temperature
parametrization
optical property
water column
biogeochemical modelling
light propagation
vertical distribution
spectral range
photosynthetically available radiation
Źródło:
Oceanologia; 2013, 55, 1
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Validation and statistical analysis of the group for high resolution sea surface temperature data in the Arabian Gulf
Autorzy:
Nesterov, O.
Temimi, M.
Fonseca, R.
Nelli, N.R.
Addad, Y.
Bosc, E.
Abida, R.
Powiązania:
https://bibliotekanauki.pl/articles/2078874.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
validation
statistical analysis
sea surface temperature
annual variability
seasonal variability
Arabian Gulf
Oman Sea
Opis:
The combined effect of climate change and steadily increasing seawater demand for industrial and domestic purposes in the Arabian Gulf region has a significant impact on the ecosystem in this region. Additionally, this effect may reduce the efficiency and increase the operating costs of industrial facilities that utilize seawater for cooling and other purposes. In this context, it is important to know various statistical characteristics of the sea surface temperature (SST) and their trends, in addition to the mean climatological characteristics. The analysis conducted in this study utilized a 17-year Group for High Resolution Sea Surface Temperature Level 4 dataset of 0.01 × 0.01° spatial resolution. First, the dataset was compared against a 2-year seawater temperature measurements at the ten offshore buoys in the relatively shallow coastal waters of the United Arab Emirates between Ras Ghumais and Dubai, which showed a reasonably good agreement between the two datasets, with the estimated root mean square deviations ranging from 0.5 to 0.9°C. Subsequently, several statistical SST characteristics were calculated. The trend analysis showed not only positive tendencies in the mean SSTs of up to 0.08°C/year in the northern Gulf, but also the trends in the annual percentile exceedances, particularly the 95th percentiles (near-maximum SSTs), which increased by approximately 0.07°C/year in the western United Arab Emirates and eastern Qatar waters. On the contrary, the 5th percentiles (near-minimum SSTs) decreased by up to 0.1°C/year, especially in the waters around Bahrain, Qatar, and the western United Arab Emirates. These results indicate that extreme hot and cold SST events in the Gulf are becoming more frequent and more extreme than before.
Źródło:
Oceanologia; 2021, 63, 4; 497-515
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zlodzenie Hornsundu i jego przedpola (SW Spitsbergen) w sezonie zimowym 2006/2007
Sea-ice cover in Hornsund and its foreshore (SW Spitsbergen) during winter season 2006/2007
Autorzy:
Styszyńska, A.
Rozwadowska, A.
Powiązania:
https://bibliotekanauki.pl/articles/260707.pdf
Data publikacji:
2008
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
Hornsund
Spitsbergen
lód morski
sezon lodowy
sea ice
winter season
sea water temperature
Opis:
W sezonie zimowym 2006/2007 przebieg zlodzenia Hornsundu był odmienny od przeciętnego. Od listopada do marca średnia miesięczna temperatura powietrza była o 3.6–6.3 deg wyższa od średniej klima-tycznej (1978–2006). Ujemna temperatura wody powierzchniowej przy brzegu Isbjornhamny występowała od 28 IX 2006 do 27 V 2007 r. Najniższe wartości temperatury wody mierzono w drugiej i trzeciej dekadzie października (–1.8°C). Latem i jesienią 2006 r. dochodziło do bardzo intensywnego obłamywania się lodu lodowcowego, który okresowo tworzył zwarte skupienia wzdłuż brzegu. Rozwój lodu morskiego w Isbjornhamnie cechuje się stadial-nością. Pierwszy okres tworzenia się lodu morskiego miał miejsce między 6 października a 3 listopada, drugi – od połowy stycznia. W tym samym czasie dryfujący lód allochtoniczny pojawił się również na przedpolu fiordu. Od trzeciej dekady lutego do drugiej dekady kwietnia prawie cała powierzchnia Hornsundu pokryta była lodem dryfu-jącym o zmiennej zwartości. Na osiowej partii fiordu lód morski zanikł po 25 kwietnia, a w Brepollen – w trzeciej dekadzie czerwca 2007 r. Maksymalna wysokość wału lodu nabrzegowego w Isbjornhamnie osiągnęła 2.5 m.
This article presents the development of sea ice cover in the waters of central and western part of the Hornsund Fjord, as well as in its foreshore during winter season 2006–2007. Due to long lasting (November-March) high air temperatures (Fig. 1) the sea ice cover development of Hornsund was different from the average one. Significant decrease in air temperature was observed only in April (mean monthly –8.7°C). In such thermal conditions the maximum thickness of sea ice which might have been formed in the outer, sheltered from high seas areas of the fjord, estimated with the help of Zubov formula, could reach 47cm in January, 58cm in February, 66cm in March, up to 77–80cm in the period from April to May 2007 (Tab.1). In summer and autumn 2006 only brash glacier ice and small icebergs broken off the glaciers endings on the sea in Hornsund drifted in the waters of the fjord. At this time brash glacier ice and growlers broken off the Hans Glacier periodically concentrated densely along the coast of Isbjorhamna. The first forms of new ice (slush and grease ice as well as shuga) were observed close to the west coast of Isbjornhamna from 6th October till 3rd November. The second period of sea ice formation started on 7th December. However, the ice disappeared quickly because of strong winds. Not sooner than in the middle of January when severe frost was noted, a permanent ice cover was formed (young ice). But also this ice was broken and diverged in most part of the fjord. Fast ice was only observed in the internal waters of Hornsund, in the Brepollen, Burgerbukta and Samarinvagen bays. From the third decade of February till the end of April the ice cover of Hornsund experienced large fluctuations. During that period the entire area of Hornsund was covered with sea ice a few times. This phenomenon was noted when the allochtonic ice drifting in the waters of the Sorkapp Current entered western and central part of the fjord and when the central and inner parts were covered with ice formed in situ. This sea ice cover was several times destroyed by very strong east winds causing that most of ice was moved outside the fjord. At the beginning of May very strong E and SE winds caused ice removal from the axial part of Hornsund. Later, apart from two short episodes (19-29 May and 22-23 June) when open strips of allochtonic ice entered west and central part of the fjord, only single floes of broken-off the fast ice from Brepollen, Burgerbukta and Samarinvagen drifted in the waters of Hornsund. The ice season 2006/2007 ended on 19th July when the last floes of very rotten ice were observed drifting from the inside of the fjord with the tidal stream to its foreshore.
Źródło:
Problemy Klimatologii Polarnej; 2008, 18; 141-160
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ zmian temperatury powierzchni oceanu na Morzu Norweskim na temperaturę powietrza na Svalbardzie i Jan Mayen (1982-2002)
The influence of the changes in sea surface temperature of the Norwegian Sea on the air temperature at Svalbard and Jan Mayen (1982-2002)
Autorzy:
Kruszewski, G.
Marsz, A. A.
Zblewski, S.
Powiązania:
https://bibliotekanauki.pl/articles/260931.pdf
Data publikacji:
2003
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
temperatury powietrza
temperatury powierzchni oceanu
Morze Norweskie
air temperature
sea surface temperature
Norwegian Sea
Opis:
This work deals with correlations between SST in the Norwegian Sea and air temperature at selected stations located in the Atlantic sector of Arctic (Bjornoya, Hornsund, Svalbard-Lufthavn, Ny Alesund and Jan Mayen). The southern and central parts of the Norwegian Sea show the strongest correlation with the air temperature at the above mentioned stations, whereas the northern parts of this sea show weaker correlation. Apart from synchronic correlations (occurring in the same months) asynchronic correlations have been found. The latter are generally much stronger than the synchronic ones. The predominant influence on the changes in air temperature at the stations have the winter SST (JFMA) in the central part of the Norwegian Sea (grid 2° x 2°, 67°N, 010°E). These winter SST show quite strong correlations with monthly air temperature at Bjornoya, Hornsund, Svalbard-Lufthavn and Jan Mayen in July, August and September. At Ny Alesund station the period with statistically significant correlation between the air temperature and the winter SST is limited to September. The strongest correlation can be observed in August (see Table 4). The observed correlations result from modification in atmospheric circulation, caused by increased heat volume in the Norwegian Sea. Such modification is reflected in the increased frequency of occurrence of meridional atmospheric circulation, which is accompanied by the increase in the frequency of air advection from the S to this sector of Arctica. Some correlations which show more significant time shift have also been observed (see Table 5). Winter SST indicate positive correlations with air temperature observed at Bjornoya and Horn-sund in August and September the following year and at Svalbard-Lufthavn in September. At Ny Alesund station the coefficients of correlation with the air temperature in the following year are increased but they do not reach the statistically significant level. Another period with statistically significant correlations is November and December the following year; significant correlations with winter SST occur at Bjornoya (r = 0.71) and all stations located on Spitsbergen (r = 0.57). The correlations of SST with air temperature observed at Jan Mayen the following year are different, i.e. the presence of strong correlations is limited to summer season - July, August and September (r ~ 0.6). The correlations with winter SST occurring in November and December the following year is connected with warm masses carried to this region together with waters with the West Spitsbergen Current. Correlations between SST and air temperature present in summer and at the end of summer the following year may probably be influenced by the modification of atmospheric circulation. The only significant correlation with summer (July and August) SST indicates the temperature of February the following year at stations located on Spitsbergen and Jan Mayen. These correlations are negative (r ~ -0.55 - -0.50). The reason for occurrence of such correlations is not clear. The changeability of winter SST in the central part of the Norwegian Sea explains from 20% (Hornsund) to 32% (Bjornoya) of changeability in annual air temperature at the above mentioned stations in the same year and from 34% (Jan Mayen) to 41% (Hornsund) of changeability in annual air temperature in the following year. The increased level of explanation of changeability in air temperature the following year influenced by winter SST is connected with the delayed flowing of the Atlantic waters to high latitudes carried with the Norwegian Current and the West Spitsbergen Current.
Źródło:
Problemy Klimatologii Polarnej; 2003, 13; 59-78
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Stan termiczny wód powierzchniowych Bałtyku a temperatura powietrza w Polsce
Sea surface temperature in Baltic and air temperature in Poland
Autorzy:
Styszynska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2084511.pdf
Data publikacji:
2011
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
Baltyk
morza
wody powierzchniowe
stan termiczny
temperatura powietrza
Polska
korelacja
Opis:
The influence of sea surface temperature (SST) changeability of the Baltic Sea on the monthly and seasonal air temperature in Poland has been examined here. Spatial variability of these correlations was analyzed in the period 1950-2009, and temporal changes - in the years 1854-2009. A significant influence of changes in SST of the Baltic on air temperature in Poland at the end of winter (February-March) and in the middle of summer (Juty-August) was indicated. The correlations between SST and the air temperature are stable both in space and time. In fact the same correlation coefficients are noted at particular stations both for 155-year and for 60-year periods.
Źródło:
Prace i Studia Geograficzne; 2011, 47; 159-167
0208-4589
Pojawia się w:
Prace i Studia Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Spatial and temporal variability of sea surface temperature in the Baltic Sea based on 32-years (1982–2013) of satellite data
Autorzy:
Stramska, M.
Bialogrodzka, J.
Powiązania:
https://bibliotekanauki.pl/articles/48273.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
satellite data
sea surface temperature
Baltic Sea
annual cycle
climate change
spatial variability
temporal variability
Źródło:
Oceanologia; 2015, 57, 3
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Comparison of direct and inverse methods of satellite observations downscaling for the coastal zone area
Autorzy:
Chybicki, A.
Łubniewski, Z.
Powiązania:
https://bibliotekanauki.pl/articles/331736.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Akustyczne
Tematy:
Earth observation
land surface temperature
sea surface temperature
PBIM downscaling method
surface effective emissivity
Opis:
The Earth observation satellite imaging systems have known limitations, especially regarding their spatial and temporal resolution. Therefore, approaches which aim to combine data retrieved from sensors of higher temporal and lower spatial resolution with the data characterized by lower temporal but higher spatial resolution are of high interest. This allows for joint utilization of the advantages of both these types of sensors. As there are several ways to achieve this goal, in this paper two approaches, direct and inverse, of downscaling the land surface temperature (LST) derived from low resolution imagery acquired by the Advanced Very High Resolution Radiometer (AVHRR) were evaluated. The applied downscaling methods utilize biophysical properties of the surface sensed using short wave infrared and thermal band. The presented algorithm evaluation was performed on the basis of a specific test case: the coastal zone area of the Gulf of Gdańsk, Poland. In this context, the objective presented in the study was to compare two methods of downscaling for a specific test case in order to evaluate how the proposed approaches cope with the specific conditions of the coastal zone area.
Źródło:
Hydroacoustics; 2016, 19; 55-64
1642-1817
Pojawia się w:
Hydroacoustics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Summer distribution patterns of Trichodesmium spp. in the Changjiang (Yangtze River) Estuary and adjacent East China Sea shelf
Autorzy:
Jiang, Z.
Chen, J.
Zhou, F.
Zhai, H.
Zhang, D.
Yan, X.
Powiązania:
https://bibliotekanauki.pl/articles/47907.pdf
Data publikacji:
2017
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
Trichodesmium
Yangtze River
estuary
China Sea
trichome
biogeochemistry
environment parameter
sea surface temperature
salinity
Opis:
To examine the distribution of Trichodesmium relative to physicochemical factors during summer in the Changjiang (Yangtze River) Estuary and adjacent East China Sea shelf, three cruises were conducted separately in June 2009, July 2011, and August 2009. Trichodesmium species found were T. thiebautii, T. erythraeum, and T. hildebrandtii. The population was dominated by T. thiebautii, which accounted for >85% of the samples found. Most of them were free trichomes. Colonial forms were rarely observed (approximately 10% of our samples), occurring only in offshore waters. The depth integrated abundances of Trichodesmium were 308 × 103, 1709 × 103, and 3448 × 103 trichomes m−2 in June, July, and August, respectively. Trichodesmium was distributed abundantly in the southern or southeastern part of our study area, where nutrients were low and light penetration, temperature, and salinity were high, which were influenced by the Taiwan Warm Current (TWC) and Kuroshio. Trichodesmium was found in low abundance in inshore, eutrophic, low-salinity waters, which were mainly controlled by the Changjiang Diluted Water (CDW) and coastal current. These results suggest that spatiotemporal changes in the summer Trichodesmium distribution correlate highly with the variations in physicochemical properties that are primarily controlled by the TWC, Kuroshio, and CDW. The summer N2 fixation rate of Trichodesmium was estimated at 12.3 μmol N m−2 d−1 in our study area, contributing >50% of biological N2 fixation.
Źródło:
Oceanologia; 2017, 59, 3
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Variability in fish catch rates associated with Sea Surface Temperature Anomaly (Niño 3.4 index) in the West of Java Sea
Autorzy:
Syamsuddin, Mega
Sunarto, Sunarto
Yuliadi, Lintang
Harahap, Syawaludin
Powiązania:
https://bibliotekanauki.pl/articles/1076099.pdf
Data publikacji:
2019
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Catch rates
El Niño
Java Sea
La Niña
oceanographic conditions
Opis:
The remotely derived oceanographic variables included sea surface height anomaly (SSHA), sea surface temperature (SST), chlorophyll-a (Chl a) and fish catches are used as a combined dataset to understand the ocean climate variability and further addresses their relations with the fish catches in the West-Java Sea. Fish catches and remotely sensed data are analyzed for the 5 years datasets from 2010-2014 and emphasized the differences of climate conditions during El Niño Southern Oscillation (ENSO) events. Here, we demonstrate the prominent annual variation of two species small pelagic fish catches (Euthynus affinis and Scomberomorus commerson) and one demersal species (Netuma thallasina) as representative of dominant catch in the region. Small pelagic catches had significant increment during El Niño compared to during La Niña events. Changes in oceanographic conditions during ENSO events resulted in perceivable variations in catches, with an average catches of 839.6 t (E. affinis) and 273,7 t (S. commerson) during El Niño. During La Niña event catch rates were reduced with an average catches of 602.6 t (E. affinis) and 210.3 t (S. commerson). During the La Niña event was less favorable for small pelagic catches. In contrast, N. thallasina does not seem to be directly affected by the ENSO. The average catches of N. thallasina during El Niño (182.17 t) lower than during La Niña (250.14 t). This inferred that different climate events might cause different oceanographic conditions that related to fish biodiversity. Our results would benefit the fish biodiversity-management to reduce risks due to climate regimes.
Źródło:
World Scientific News; 2019, 117; 175-182
2392-2192
Pojawia się w:
World Scientific News
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zlodzenie Hornsundu i wód przyległych (Spitsbergen) w sezonie zimowym 2010-2011
Ice conditions in Hornsund and adjacent waters (Spitsbergen) during winter season 2010-2011
Autorzy:
Kruszewski, G.
Powiązania:
https://bibliotekanauki.pl/articles/260971.pdf
Data publikacji:
2012
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
lód morski
temperatura wody morskiej
Hornsund
Spitsbergen
sea ice
ice season
sea surface temperature
Opis:
Sezon lodowy 2010/2011 zaczął się w połowie października. Pierwsze postacie autochtonicz-nego lodu morskiego zaobserwowano w strefie brzegowej Isbjornhamny 15.10. po spadku dobowej temperatury powietrza poniżej poziomu temperatury zamarzania wody morskiej. Zbliżone do średnich wieloletnich wartości temperatury powietrza okresu listopad – styczeń sprzyjały tworzeniu się lodu w strefie brzegowej Hornsundu. Lód morski o zwartości do 4/10 pojawił się w Hornsundzie w końcu października i utrzymywał w listopadzie. Prze-bieg warunków lodowych w rejonie południowego Spitsbergenu – zbliżony do normalnego z wielolecia – umoż-liwiał napływ lodu do fiordu z zewnątrz od połowy grudnia. W tym też okresie w wewnętrznych partiach fiordu zaczął się formować lód stały brzegowy, którego pokrywa w sposób ciągły występowała w N części Brepollen do końca drugiej dekady lipca 2011 (około 7 miesięcy). W okresie maksymalnego rozwoju (druga dekada lutego) lód stały lub całkowicie zwarty pokrywał około 2/3 powierzchni fiordu.
This paper presents the ice conditions in the Hornsund Fjord (Svalbard) during expedition season 2010/2011. Sea ice season started in the mid of October, after clear air temperature drop (Fig. 2). Since this time forms of locally formed ice were present, mainly in coastal zone. To the end of November concentration of ice did not exceed 4/10 (very open drift ice). Close to mean thermal conditions in Hornsund area during winter months (Fig.1, Tab. 1) were favourable for ice development in this region. Theoretical sea ice thickness at the end of the Year 2010 could reach about 50 cm, and close to 1 m at the end of ice season. Close and very close pack ice (7-10/10) drifting outside the fjord were present since December (Fig. 7). Easternmost inner part of the Hornsund was covered by fast (consolidated) ice since mid of December to the mid of July 2011. During its maximum development in February fast ice covered over 70% of Hornsund area. Close and very close pack ice were present at Hornsund waters in January, February, three weeks of March, second half of April and first week of May – all together over three and half months. Periods of time with smaller ice concentration were connected with strong easterly air circulation. In May and June ice concentration in SW Svalbard area decrease significantly. Last two episodes the very close ice pack flowed into the Hornsund took place in first days and in second half of July 2011 (Fig. 8).
Źródło:
Problemy Klimatologii Polarnej; 2012, 22; 69-82
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
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