water vapor flux

基本解释

Torrential storm occurs in stronger frontal zone of energy, high humid region and water vapor flux convergence region.
大暴雪发生在较强的能量锋区、高湿区和水汽通量辐合区内。
The net water vapor flux is positive always, but its content is low about 21.88% than average state in dry year, and is high about 53.99% in wet year.
无论旱涝年，青海高原空中净水汽通量均呈正值，但旱年比平均状况偏少21.88%，涝年偏多53.99%。
With the development of convective activity, the water vapor flux and water vapor convergence develop toward high-level and the wet layer obviously thickens.
随着对流活动的发展，水汽通量和水汽辐合都向高层发展，湿层明显增厚。