行星风系
- 网络planetary wind system
行星风系-
推测可可西里地区中新世早-中期海拔高度已超过了2000m，并已超过影响行星风系的临界值，阻挡了来自海洋湿润气流进入内陆，导致气候变干。
The altitude of Hoh Xil region might have exceeded 2000m in early-middle Miocene . Thus the higher altitude influenced the planetary system of winds , which in turn prevented the moist air into the inland from the ocean and caused the dry climate .
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季风看来具有受行星总风系的不同性质和不同程度的影响，这比以往更为可信。
To a greater extent than was formerly thought to be the case the monsoons appear to be in the nature of various kinds and degrees of modification of the general planetary wind system .