无冰区

南极无冰区生态与环境变化在粪土层中的记录

Eco-environmental Change Records of Antarctic Ice-free Areas in Sediments Influenced by Marine Animals

南极无冰区古气候与冰盖进退历史研究进展

The Research Progress on the History of Palaeoclimate and Ice Sheet Advance and Recession in the Antarctic Ice-free Areas

特别是2007年和2008年，Beaufort海海冰边缘线一直向北退缩，在高纬度地区出现无冰区。

Especially in 2007 and 2008 , the marginal ice line retreat to high latitude at Beaufort sea and there is no ice in some marginal ice zone ( MIZ ) .

南极无冰区典型沉积环境石英砂表面结构特征及其在沉积环境识别中的应用

Characteristics of quartz grain surface textures in the Antarctic Ice-free area

南极无冰区生态地质学及其形成与发展

The Formation and Development of Eco-geology in Ice-free Area , Antarctica

南极洲为数不多的无冰区

the few parts of Antarctica that are ice-free

随着海水变暖，鱼类可能会迁徙到无冰区，捕捞船队可能会紧随其后。

Fish may migrate into the ice-free area as the ocean warms , tempting fishing fleets to follow .

结果表明，南极无冰区和近海磷的生物地球化学循环主要包括了磷在海洋-陆地-淡水湖泊/溪流-海洋的迁移过程。

Results showed that P biogeochemical cycle in Antarctica includes the migration and transformation of P in the sea-land-lakes / streams-sea .

南极洲最大的无冰区是一片寒风凛冽、地形崎岖的冰冻沙漠，该区域地形看起来就像是冥王星，而根本不是我们的地球。

The largest ice-free region in Antarctica is a windswept , frozen desert whose rugged terrain looks as if it belongs on Pluto rather than our planet .

环南极洲无冰区就是随着气候变暖、冰川后退而出现，是研究南极乃至全球的自然环境演化历史的理想场所。

The ice-free areas in circum Antarctica appear with the climate becoming warm and the ice sheet retreating , which are the ideal sites to study on the environmental evolutional history in Antarctica , even on the global environmental change .