...西风急流 降水模拟 [gap=1234]ords】: Regional climate model,Radiative transfer scheme,Temperature simulation,Westerly jet,Precipitation simulation ...
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如果大气是静力稳定的,且静力稳定度不变,则垂直风切大的空域,有较小 的Ri ,所以〝西风喷流(westerly jet)处易生乱流。由于高度大,相对温度小, 该处空域通常没有云,所以该乱流称为「晴空乱流Clear Air Turbulence,CAT.
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upper-level westerly jet 高空西风急流
double westerly jet 双西风急流
westerly jet stream 西风急流
westerly jet in winter 冬季西风急流
westerly jet over east asia 东亚西风急流
During the monsoon onset period, the westerly jet becomes weaker due to its moving away from Gaize to the north.
季风爆发阶段西风急流逐渐离开改则地区并向高原北部移动,在该地区表现为减弱。
We study the interannual variability of the extratropical westerly jet over East Asian (EAJS), its impacts and possible mechanisms.
探讨了东亚地区副热带西风急流(EAJS)位置的年际变化特征、影响及其可能机制。
The evolution and enhancement of occluded frontal circulation in upper-level westerly jet and lower-level southerly jet are discussed by using a dry primitive equation model.
利用原始方程模式探讨了高空西风急流和低空南风急流中锢囚锋环流的演变和增强机制。
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