进一步证实高北纬极地气候可以通过西风带和蒙古、西伯利亚高压系统传输到东亚东亚季风区。
Further, they verify that high-latitude climate can transfer to East Asia monsoon region via the westerly and Mongolia and Siberian high pressure system.
对此类黄土剖面的进一步发掘、研究将有助于探讨东亚季风区气候变化的一些细节与机制问题。
To explore and study those loess profiles with high resolution and sedimentary rate would be helpful to investigate some problems about mechanism of climate change in East Asia monsoon region.
西风带作为北大西洋气候区和东亚季风气候区之间的联系纽带，对东亚季风气候和西风带气候具有重要影响，西风带在一定意义上控制着东亚季风的北界。
Westerly wind as a link between the climates of the North Atlantic and East Asian monsoon area, has great effect on the climates of East Asian monsoon area and westerly wind area.
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