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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:
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:
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
Tytuł:
Distribution of net phytoplankton in the sea-ice zone between Elephant Island and the South Orkney Islands (December 1988 - January 1989)
Autorzy:
Ligowski, Ryszard
Kopczyńska, Elżbieta
Powiązania:
https://bibliotekanauki.pl/articles/2052790.pdf
Data publikacji:
1991
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctic
Weddell Sea
net phytoplankton
sea ice edge
diatoms
Źródło:
Polish Polar Research; 1991, 12, 4; 529-546
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Algae of drifting sea ice north of Elephant Island (BIOMASS III, October 1986)
Autorzy:
Ligowski, Ryszard
Lipski, Maciej
Zieliński, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/2053179.pdf
Data publikacji:
1988
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Antarctica
sea ice algae
chlorophyll α
drifting ice
BIOMASS III
Źródło:
Polish Polar Research; 1988, 9, 2-3; 217-229
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Algae in the annual sea ice at Hooker Island, Franz Josef Land, in August 1991
Autorzy:
Okolodkov, Yuri B.
Powiązania:
https://bibliotekanauki.pl/articles/2052736.pdf
Data publikacji:
1993
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Franz Josef Land
phycology
sea-ice algae
Źródło:
Polish Polar Research; 1993, 14, 1; 25-32
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sea ice mechanics
Autorzy:
Paul, Felix
Schwarz, Carina
Audh, Riesna Reuben
Bluhm, J.
Johnson, Siobhan
MacHutchon, Keith
Mielke, Tommy
Mishra, A.
Rampai, Tokoloho
Ricken, Tim
Schwarz, Alexander
Skatulla, Sebastian
Thom, Andrea
Verrinder, Robyn
Schröder, Jörg
Vichi, Marcello
Lupascu, Doru C.
Powiązania:
https://bibliotekanauki.pl/articles/29519762.pdf
Data publikacji:
2023
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
sea ice mechanics
polar regions
review
Antarctic MIZ
Opis:
Earth System Models (ESM), simulating sea ice and its interaction with the atmosphere and open ocean, require reliable physical, chemical, and biological input from measurements. There is limited data available from the Marginal Ice Zone of the Antarctic, where sea ice growth mechanisms differ from the Arctic. The main objective of this study is to review existing work related to Antarctic sea ice and highlight gaps in the available literature. The mechanical properties of sea ice and the numerical modeling of sea ice across all scales are covered. We summarize the genesis, physical mechanics, static and dynamic properties, strength, toughness, and transport of young sea ice as well as medium to large scale observation. On the computational mechanics side large- and small-scale modeling, ocean-sea ice and atmosphere-sea ice models, as well as sea ice rheology models, sea ice fracture mechanics, and bio-geo-chemical interaction processes are captured. The synergy between the physical and computational mechanics brings to light missing information from both fields. Plain language summary (PLS) Sea ice determines the interaction of the ocean with the atmosphere in both the southern and northern hemispheres. Its formation and annual development is subject to mechanical interaction with ocean currents and winds. This review covers the mechanics of sea ice in the Antarctic and its relation to the Arctic covering experiment and modelling. Impact on the climate is discussed.
Źródło:
Computer Methods in Materials Science; 2023, 23, 3; 5-53
2720-4081
2720-3948
Pojawia się w:
Computer Methods in Materials Science
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Consequences of global warming in cryosphere
Autorzy:
Jania, Jacek A.
Powiązania:
https://bibliotekanauki.pl/articles/703326.pdf
Data publikacji:
2008
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
cryosphere
climate warming
sea ice
glacier dynamics
sea level rise
Opis:
Scale of changes of particular components of cryosphere due to global warming is presented. Cryosphere diminishes its spatial extend and the total volume of all kinds of ice is reduced. The Arctic sea ice cover has recently diminished most intensely. It reached its minimal extend (4.28 mln km2) in September 2007. One expects accelerated disintegration of sea ice of the Arctic as a result of coadjuvancy of oceanic and atmospheric factors. In consequence, more intense warming of climate coming from warmer ocean water is predicted in the Arctic basin. Increase of melting of glaciers during the last three decades results in decrease of their extend and thickness. Additionally, more meltwater is reaching bed of glaciers and is accelerating their flow velocity due to faster basal sliding. Such processes result in more intense breaking off the icebergs from fronts of glaciers terminating into the sea. Dynamic response of Greenland outlet tidewater glaciers has been detected after 2000 and it affects significantly global ocean level rise by ca 0.5 mm/yr. The Antarctic Ice Sheet is actually only insignificantly reacting to global warming. The paper discusses possible scenarios of the consequences of dynamic reaction of the West Antarctic Ice Sheet for increasing warming and slow sea level rise. Permafrost is reacting in a less distinct but detectable scale. The paper is giving not only description of consequences of climate warming for cryosphere, important impact of its spatial extend and features on atmosphere and oceans are considered either. A series of positive feedacks between  warming climate and cryosphere are listed. Described evolution of cryosphere is suggesting that distinct trend of climate warming is irreversible for the next centuries. One can also expect systematic rise of global ocean level as the consequence of glacier melting and dynamic transfer of ice masses based on land to the sea.
Źródło:
Nauka; 2008, 3
1231-8515
Pojawia się w:
Nauka
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Numerical simulations of sea ice conditions in the Baltic Sea for 2010–2016 winters using the 3D CEMBS model
Autorzy:
Janecki, M.
Nowicki, A.
Kańska, A.
Golenko, M.
Dzierzbicka-Głowacka, L.
Powiązania:
https://bibliotekanauki.pl/articles/260518.pdf
Data publikacji:
2018
Wydawca:
Politechnika Gdańska. Wydział Inżynierii Mechanicznej i Okrętownictwa
Tematy:
Baltic Sea
sea ice
numerical modelling
remote sensing
climate change
Opis:
Sea ice conditions in the Baltic Sea during six latest winters – 2010/2011 to 2015/2016 are analysed using coupled ice– ocean numerical model 3D CEMBS (3D Coupled Ecosystem Model of the Baltic Sea). Simulation results are compared with observations from monitoring stations, ice charts and satellite data. High correlation between model results and observations has been confirmed both in terms of spatial and temporal approach. The analysed period has a high interannual variability of ice extent, the number of ice days and ice thickness. Increasing number of relatively mild winters in the Northern Europe directly associated with climate change results in reduced ice concentration in the Baltic Sea. In this perspective, the implementation and development of the sea ice modelling approach (in addition to standard monitoring techniques) is critical to assess current state of the Baltic Sea environment and predict possible climate related changes in the ecosystem and their influence for human marine–related activities, such as fishery or transportation.
Źródło:
Polish Maritime Research; 2018, 3; 35-43
1233-2585
Pojawia się w:
Polish Maritime Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Measurements of light transfer through drift ice and landfast ice in the Northern Baltic Sea
Autorzy:
Kari, E.
Jutila, A.
Friedrichs, A.
Lepparanta, M.
Kratzer, S.
Powiązania:
https://bibliotekanauki.pl/articles/2079188.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:
light transfer
measurement
sea ice
landfast ice
coloured dissolved organic matter
Baltic Sea
Opis:
The aim of this study was to investigate the light transfer through sea ice with a focus on bio-optical substances both in fast ice and in the drift ice zones in the northern Baltic Sea. The measurements included snow and ice structure, spectral irradiance and photosynthetically active radiation below the sea ice. We also measured the concentrations of the three main bio-optical substances which are chlorophyll-a, suspended particulate matter, and coloured dissolved organic matter (CDOM). These bio-optical substances were determined for melted ice samples and for the underlying sea water. The present study provides the first spectral light transfer data set for drift ice in the Baltic Sea. We found high CDOM absorption values typical to the Baltic Sea waters also within sea ice. Our results showed that the transmittance through bare ice was lower for the coastal fast ice than for the drift ice sites. Bio-optical substances, in particular CDOM, modified the spectral distribution of light penetrating through the ice cover. Differences in crystal structure and the amount of gas inclusions in the ice caused variation in the light transfer. Snow cover on ice was found to be the dominant factor influencing the light field under ice, confirming previous studies. In conclusion, snow cover dominated the amount of light under the ice, but did not modify its spectral composition. CDOM in the ice absorbs strongly in the short wavelengths. As pure water absorbs most in the long wavelengths, the light transfer through ice was highest in the green (549–585 nm).
Źródło:
Oceanologia; 2020, 62, 3; 347-363
0078-3234
Pojawia się w:
Oceanologia
Dostawca treści:
Biblioteka Nauki
Artykuł

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