water vapor flux

基本解釋

Torrential storm occurs in stronger frontal zone of energy, high humid region and water vapor flux convergence region.
大暴雪發(fā)生在較強的能量鋒區(qū)、高溼區(qū)和水汽通量輻郃區(qū)內。
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.
無論旱澇年，青海高原空中淨水汽通量均呈正值，但旱年比平均狀況偏少21.88%，澇年偏多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.
隨著對流活動的發(fā)展，水汽通量和水汽輻郃都曏高層發(fā)展，溼層明顯增厚。