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青藏高原雨季降水的水汽条件研究
段丽君1,2(), 申红艳1,2(), 余迪1,2, 马有绚1,2, 白文蓉1,2, 李万志1,2
Study on water vapor conditions of precipitation on the Tibetan Plateau during rainy season
Lijun DUAN1,2(), Hongyan SHEN1,2(), Di YU1,2, Youxuan MA1,2, Wenrong BAI1,2, Wanzhi LI1,2

图6. PC2负异常年从地面至300 hPa垂直积分的青藏高原雨季水汽通量(矢量,单位:kg·m-1·s-2)及散度(阴影,单位:10-5 kg·m-2·s-2)分布

Fig.6. The distribution of vertically integral water vapor flux (arrows, unit: kg·m-1·s-2) and divergence (shading, unit: 10-5 kg·m-2·s-2) of rainy season from surface to 300 hPa in Tibetan Plateau in negative years of the PC2