Further, they verify that high-latitude climate can transfer to East Asia monsoon region via the westerly and Mongolia and Siberian high pressure system.

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。

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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.

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。

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