| THE FEATURES OF SEA-ICE COVER, SNOW DISTRIBUTION AND ITS DENSIFICATION IN THE CENTRAL ARCTIC OCEAN |
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| 作者姓名： | 效存德 秦大河 任贾文 |
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| 作者单位： | Laboratory of Ice Core and Cold Regions Environment，Lanzhou Institute of Gleriology and Geocryology，the Chinese Academy of Siences，Lanzhou 730000，P. R. China |
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| 摘 要： | I.INTKODUCTIONTheArcticOcean,withanareaofapproximately9.5X106krnZ,ispredominantlysea--icecoveredthroughouttheyearinitscentralarea,whilethesouthedgeofmarginalicezone(MIZ)variesseasonally.ThemaxinltlmofIcecoverextentoccursbetweenFebruaryandMarch,whilethemininlunlisbetweenAugustandseptember.Placingtheiceedgeto8%iceconcentration(percentarealcoveragesofseaice)isopleths,variationofextentofsea--icecoveroftheArcticOceanisI)etween9X106--16X106kmZIbytheobservationofasatellite--bornescanningm…
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| 收稿时间： | 18 November 1996 |
The features of sea-ice cover, snow distribution and its densification in the central arctic ocean |
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| Cunde Xiao,Dahe Qin,Jiawen Ren.THE FEATURES OF SEA-ICE COVER, SNOW DISTRIBUTION AND ITS DENSIFICATION IN THE CENTRAL ARCTIC OCEAN[J].Chinese Geographical Science,1997,7(4):317-327. |
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| Authors: | Cunde Xiao Dahe Qin Jiawen Ren |
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| Institution: | (1) Laboratory of Ice Core and Cold Regions Environment, Lanzhou Institute of Glaciology and Geocryology, the Chinese Academy of Sciences, 730000 Lanzhou, P. R. China |
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| Abstract: | Based on the observation of sea-ice cover and measurement of snow depths and stratigraphy during China's First North Pole Sientific Expedition, three types of surface topography of sea ice and correspondingly three categories of snow distribution in the central Arctic are classified. It is considered that the classification will help to determine the sites for snow depth measurement, stratigraphy Observation and snowpits sampling. The snow cover is slowly accumulated during the long Arctic winter, approximately from September to early May next year, while its ablation shows abrupt from south to north. By the end of August, the snow cover is alment totally removed. The spatial distribution of snow depth is characterized by a northwardly decreasing trend, which is proposed to result from the remote vapour sources, i. e., the major vapour over the Arctic regions is transported from mid-latitudes. The stratigraphy of the snompits are characterized by the extensively existed depth hoar at the deeper part of the pits, which is probably a signal of the beginning of the long Arctic winter.The present of infiltration-congelation ice adhering to sea ice surface at the end of the ablation indicates that the annual accumulation is approximately equals to the annual ablation near north pole. |
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| Keywords: | Arctic Ocean sea-ice cover snowpack snow stratigraphy |
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