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Wyszukujesz frazę "sea−ice" wg kryterium: Temat


Tytuł:
On the problem of sea ice mechanics
Autorzy:
Kleine, E.
Powiązania:
https://bibliotekanauki.pl/articles/972867.pdf
Data publikacji:
2001
Wydawca:
Instytut Morski w Gdańsku
Tematy:
sea ice
forecasting
structure
Opis:
In the context of short-tenn sea ice forecasting, the model should capture as many of the synoptic features and as much of their variability. as possible. We are interested in the meso-scale properties and processes, i.e. thickness, consolidation, compactness, smoothness, accumulation of ridges, formation of leads and ice edge, drift and displacement, etc. Modelling and forecasting of synoptic ice formation are of interest to shipping as it affects route planning and the operation of icebreakers. With a view to conventional ice charting, the forecast problem might read: Given today 's ice chart, what will tomorrow 's ice chart look like? The model has to return meso-scale features, while essential smaller-scale mechanisms have to be parameterised. The problem in a meso-scale model is to adequately take into account the governing fine-scale mechanisms. Pack ice is a crushable fragmented aggregate, characterized by point-like contacts and stress trajectories. In compressible loading, even local traction forces, causing brittle failure, may be induced. The localization of stress and strain is a considerable complication! By way of localization, critical phenomena at singular points, affect the entire structure. Meaningful characteristics are integrity, state of damage (flaws, cracks). fragmentation and skeletal structure (fabric of fragments, strength of the structure). Structural properties and their evolution dun·ng the material history could be represented by suitably chosen internal variables. To reflect the state of degradation, fragmentation, consolidation, etc., special concepts are required for the damage mechanics of fracturing pieces and fragmented aggregates. Using such a vehicle, the meso-scale mechanics of sea ice could be accommodated in a continuum mechanics model. More elements have been worked out in plasticity.
Źródło:
Biuletyn Instytutu Morskiego w Gdańsku; 2001, 28, 2; 17-21
1230-7424
2450-5536
Pojawia się w:
Biuletyn Instytutu Morskiego w Gdańsku
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
On the problem of sea ice mechanics
Autorzy:
Kleine, E.
Powiązania:
https://bibliotekanauki.pl/articles/1920616.pdf
Data publikacji:
2001
Wydawca:
Instytut Morski w Gdańsku
Tematy:
sea ice
forecasting
structure
Opis:
In the context of short-tenn sea ice forecasting, the model should capture as many of the synoptic features and as much of their variability. as possible. We are interested in the meso-scale properties and processes, i.e. thickness, consolidation, compactness, smoothness, accumulation of ridges, formation of leads and ice edge, drift and displacement, etc. Modelling and forecasting of synoptic ice formation are of interest to shipping as it affects route planning and the operation of icebreakers. With a view to conventional ice charting, the forecast problem might read: Given today 's ice chart, what will tomorrow 's ice chart look like? The model has to return meso-scale features, while essential smaller-scale mechanisms have to be parameterised. The problem in a meso-scale model is to adequately take into account the governing fine-scale mechanisms. Pack ice is a crushable fragmented aggregate, characterized by point-like contacts and stress trajectories. In compressible loading, even local traction forces, causing brittle failure, may be induced. The localization of stress and strain is a considerable complication! By way of localization, critical phenomena at singular points, affect the entire structure. Meaningful characteristics are integrity, state of damage (flaws, cracks). fragmentation and skeletal structure (fabric of fragments, strength of the structure). Structural properties and their evolution dun·ng the material history could be represented by suitably chosen internal variables. To reflect the state of degradation, fragmentation, consolidation, etc., special concepts are required for the damage mechanics of fracturing pieces and fragmented aggregates. Using such a vehicle, the meso-scale mechanics of sea ice could be accommodated in a continuum mechanics model. More elements have been worked out in plasticity.
Źródło:
Biuletyn Instytutu Morskiego w Gdańsku; 2001, 28, 2; 17-21
1230-7424
2450-5536
Pojawia się w:
Biuletyn Instytutu Morskiego w Gdańsku
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność pokrywy lodów morskich w okresie maksimum ich rozwoju na Morzu Grenlandzkim w i połowie XX wieku
Changes in the sea-ice cover during their maximum development in the Grenland Sea in the first half of the twentieth century
Autorzy:
Adrychowska, K.
Powiązania:
https://bibliotekanauki.pl/articles/261045.pdf
Data publikacji:
2015
Wydawca:
Stowarzyszenie Klimatologów Polskich
Tematy:
zasięg lodu morskiego
pokrywa lodowa
Morze Grenlandzkie
sea ice extent
sea ice cover
Greenland Sea
Opis:
Artykuł przedstawia zmiany powierzchni lodów występujące w okresie maksimum ich rozwoju (w kwietniu) w rejonie między Grenlandią, Islandią i Spitsbergenem w latach: 1901-1939 oraz 1946-1956 oparte na analizach map lodowych udostępnionych przez Duński Instytut Meteorologiczny. Obliczeń powierzchni lodów dokonano w programie ArcGis10.0 w układzie współrzędnych North Pole Lambert Azimuthal Equal Area. Przeprowadzone pomiary powierzchni zlodzonej wskazują na dużą zmienność powierzchni lodów na obszarze między Spitsbergenem, Grenlandią i Islandią. W tym rejonie największe powierzchnie lodów wystąpiły w 1905, 1906 i 1911 roku, a najmniejsze w latach 1925 i 1930. Znacznie mniejsze zmiany powierzchni lodów miały miejsce w rejonie Cieśniny Duńskiej i na wodach między Islandią i SE Grenlandią. W tym rejonie największy rozwój pokrywy lodowej miał miejsce w 1934, 1935 oraz 1952 roku, a najmniejszy w latach 1939, 1929 i 1903. Na całym badanym obszarze największy rozwój lodów miał miejsce w okresie 1905-1918 z maksimum w latach 1906 (1638 tys. km2), 1911 i 1918. Minimum rozwoju pokrywy lodowej wystąpiło w 1933 roku (1037 tys. km2). W okresie 1901-1939 zaznacza się istotny trend malejący powierzchni lodów. Zmiany powierzchni lodów w latach 1946-1956 charakteryzują się dużą stabilnością oscylującą między 1300 a 1500 tys. km2.
The article present changes of sea ice extent during a period of time when they developed most (April) in the geographical area located between Greenland, Iceland and Spitsbergen during years 1901-1939 and 1945-1956 based on data shared by Danish Meteorological Institute. Surface calculations were made by using ArcGis 10.0 software, using geographical coordinate system North Pole Lambert Azimuthal Equal Area. Results of the calculations show high deviations of sea ice extent at investigated area. Biggest surface area noted in 1905, 1906 and 1911 and smallest in 1925 and 1930. Much smaller changes were observed and at the sea between Iceland and South-Eastern Greenland. During the period 1901-1939 a diminishing trend was observed there considering ice surface area. Years 1946-1956 remain with a stable amount of ice surface.
Źródło:
Problemy Klimatologii Polarnej; 2015, 25; 239-248
1234-0715
Pojawia się w:
Problemy Klimatologii Polarnej
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Distribution of microflagellates and diatoms in the sea-ice zone between Elephant Island and the South Orkney Islands (December 1988 - January 1989)
Autorzy:
Kopczyńska, Elżbieta
Powiązania:
https://bibliotekanauki.pl/articles/2052789.pdf
Data publikacji:
1991
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctic
phytoplankton
sea-ice zone
Źródło:
Polish Polar Research; 1991, 12, 4; 515-528
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Environmental conditions and phytoplankton standing crop near pack-ice in the Scotia Sea (December 1988 - January 1989)
Autorzy:
Lipski, Maciej
Powiązania:
https://bibliotekanauki.pl/articles/2052791.pdf
Data publikacji:
1991
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctica
phytoplankton
sea-ice zone
Źródło:
Polish Polar Research; 1991, 12, 4; 507-513
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sea Ice Services in the Baltic Sea
Autorzy:
Sztobryn, M.
Powiązania:
https://bibliotekanauki.pl/articles/116094.pdf
Data publikacji:
2009
Wydawca:
Uniwersytet Morski w Gdyni. Wydział Nawigacyjny
Tematy:
Hydrometeorological Aspect
Baltic Sea
Sea Ice Services (SIS)
Ice Service
Baltic Winter Navigation
Ice Conditions
Baltic Sea Ice Code (BSIC)
Ice Chart
Opis:
The Baltic winter navigation depended always very much on the ice conditions in the sea. The sea ice occurs different in form and amount, depending on the sea area and the winter season. As the maritime traffic on the Baltic Sea constitutes a substantial amount in the whole of the Baltic countries transport, Sea Ice Services (SISs) have come into being. They constituted the Baltic Sea Ice Meeting (BSIM) – a body, which assembles the parties, which are interested in warnings against bad ice conditions, and in protection of navigation in ice in the Baltic Sea. An indispensable co-operator to this body was always the company “Baltic Icebreakers”. To-day within the BSIM operate by the SISs of Denmark, Sweden, Finland, Russia, Estonia, Latvia, Lithuania, Poland and Germany, Netherlands, Norway and the Baltic Icebreakers. The main statutory duties of the SISs is the acquisition, processing and dissemination of actual information on sea ice conditions and on obstructions to navigation due to sea ice. This is done by maintaining observing posts along the coast of those countries, in their ports and approaches to them, by gathering information from ships, from ice beakers, if possible – from reconnaissance flights or satellite images. Routine products of SISs are the ice reports, ice bulletins, ice charts, forecasts and warnings and other information broadcast by mass media, e.g. radio, internet, Navtex and on the national and Baltic SISs’ web sites etc.
Źródło:
TransNav : International Journal on Marine Navigation and Safety of Sea Transportation; 2009, 3, 4; 415-420
2083-6473
2083-6481
Pojawia się w:
TransNav : International Journal on Marine Navigation and Safety of Sea Transportation
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Patchiness of sympagic algae and meiofauna from the fast ice of North Open Water (NOW) Polynya
Autorzy:
Wiktor, Józef
Szymelfenig, Maria
Powiązania:
https://bibliotekanauki.pl/articles/2052126.pdf
Data publikacji:
2002
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic polynya
sea-ice
algae
meiofauna
Źródło:
Polish Polar Research; 2002, 23, 2; 175-184
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrology and hydrochemistry of the surface water layer near the sea-ice edge in the Scotia Sea (December 1988 - January 1989)
Autorzy:
Tokarczyk, Ryszard
Lipski, Maciej
Perez, Felix F.
Reboredo, Ricardo P.
Powiązania:
https://bibliotekanauki.pl/articles/2052792.pdf
Data publikacji:
1991
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctica
hydrology
hydrochemistry
sea-ice zone
Źródło:
Polish Polar Research; 1991, 12, 4; 495-505
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Microzooplankton in a Warming Arctic: A Comparison of Tintinnids and Radiolarians from Summer 2011 and 2012 in the Chukchi Sea
Autorzy:
Dolan, John R.
Yang, Eun Jin
Kim, Tae Wan
Kang, Sung-Ho
Powiązania:
https://bibliotekanauki.pl/articles/763780.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
Tematy:
Climate change, plankton, rhizaria, sea ice, Tintinnina
Opis:
The Chukchi Sea was sampled in August of 2011, a year of near-normal sea ice among recent years, and again in August 2012, a year of all time record low sea ice. We exploited this sampling to test the hypothesis that different sea ice conditions are associated with differences in abundances or species composition of microzooplankton through an examination of tintinnids and radiolarians. From 18 stations in 2011, and 19 stations in 2012, organisms were enumerated in plankton net tow material, and chlorophyll determinations made (total and ≤ 20 μm) from discrete depth samples. We found that the low sea ice conditions of 2012 were associated with higher chlorophyll concentrations (both total and the ≤ 20 μm size fraction), compared to 2011. However, tintinnid ciliates and radiolarians were much lower in concentration, by about an order of magnitude, compared to 2011. In both years the radiolarian assemblage was dominated by Amphiselma setosa. The species composition of the tintinnid ciliates was similar in the two years, but there were distinct differences in the relative abundances of certain species. The 2012, low sea ice assemblage, was dominated by small forms in contrast to 2011, when large species were the most abundant. We present these findings in detail and discuss possible explanations for the apparent differences in the microzooplankton communities associated with distinct sea ice conditions in the Chukchi Sea.
Źródło:
Acta Protozoologica; 2014, 53, 1
1689-0027
Pojawia się w:
Acta Protozoologica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sea ice microalgae community of the floating ice in the Admiralty Bay (South Shetland Islands)
Autorzy:
Ligowski, Ryszard
Powiązania:
https://bibliotekanauki.pl/articles/2053243.pdf
Data publikacji:
1987
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctica
King George Island
sea ice microalgae
Źródło:
Polish Polar Research; 1987, 8, 4; 367-380
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł

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