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Physical scientist from NASA said that the result of Gravity Recovery And Climate Experiment, the whole Greenland island lost half of the land ice in the past five years and the water it forms can fill eleven Chesapeake Bay , the largest bay in United States,165 thousand square kilometers.

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According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.

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The main is focused on the discussion on the crystal structure, porosity, temperature profiles, thermal conductivity, salinity and density of sea ice in Liaodong Bay based on the author's research on ice temperature profile in field, thermal conductivity coefficients in field and in laboratory, and the ice structures studied under the computerized tomography scanner.

重點(diǎn)以作者完成的海冰現(xiàn)場溫度場www.99热.com、現(xiàn)場冰層導(dǎo)熱系數(shù)和實(shí)驗(yàn)室導(dǎo)熱系數(shù)以及應(yīng)用正交偏光和CT掃描研究冰組構(gòu)等研究成果為主體欧美性爱人人操人人射，討論了遼東灣海冰的晶體結(jié)構(gòu)、孔隙率黄色视频在线免费观看操使劲不要高潮、溫度場和導(dǎo)熱系數(shù)国产久一黄色网站、鹽度、密度等工程海冰指標(biāo)欧美男女性爱视频网站。

The design on two types of icebreaking cone for platform jacket for Jinzhou 21-2 and Jinzhou 9-3E WHPA in Liaodong bay heavy ice zone of Bohai Bay are presented in this paper,and the advice on design of icebreaking cone on jacket platform for heavy ice zone of Bohai Bay has also been put forward.

主要闡述了渤海遼東灣重冰區(qū)海域錦州21-1 BOP和錦州9-3E WHPA平臺(tái)導(dǎo)管架破冰錐體的設(shè)計(jì)實(shí)踐国产吧在线视频，并對(duì)渤海重冰區(qū)平臺(tái)導(dǎo)管架破冰錐體的設(shè)計(jì)提出了建議。

Third, based on the spreading and floading prediction result of spilled oil at Liaodong Bay ice field, the paper establishes spilled oil damage factors index system and their quantization standard combining with damage factors of the natural environment and natural resource conditions of oil spill sea field , spilled oil characteristics and spilled oil quantity and so on.

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According to the heat balance at the bottom of sea ice, sea ice thickness in the Liaodong Bay was simulated with the alterative Stefan analytical model. The biggest ice thickness is 13cm, and the average is 8.35cm. The spatial difference is small and no thick ice regions exist.

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Photo Gallery: Extreme Ice Survey This doughy-looking iceberg in western Greenland's Disko Bay was once part of the enormous Jakobshavn ice stream, a river of ice four miles wide and several thousand feet thick.

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The investigations included the following:（1） estimation of sea ice distribution by ship-based observations between Middle Weddell Sea and Prydz Bay;（2） estimation of sea ice distribution by aerial photography in the Prydz Bay;（3） direct measurements of fast ice thickness and snow cover, as well as ice core sampling in Nella Fjord;（4） estimation of melting sea ice patterns near the ZhongShan Station; and （5） observation of sea ice early freezing near the ZhongShan Station.

包括：（1）基于走航觀測的威德爾海至普利茨灣之間海冰分布研究；（2）基于航空拍攝的普利茨灣海冰分布研究在线视频欧美专区；（3）納拉海峽固定冰和上浮雪厚度鉆孔測量以及冰心鉆染镁肧e精品一区二区影院。唬?）中山站附近融化冰的分布研究以及（5）中山站附近海冰早期凍結(jié)過程觀測研究91肉色长靴丝袜国产在线。

Which by their causes, and the water depth can be divided into two parts, one is basically the edge of the continental shelf sea (such as the Kara Sea, Laptev Sea, East Siberian Sea, Chukchi Sea, Beaufort Sea, Baffin Bay, Hudson Bay, etc.); Second, the central part of the Arctic Ocean, all kinds of ice widespread, most of the waters as "permanent ice zone" of biological resources than the poor.

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