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(qiáng)的能量鋒區(qū)、高濕區(qū)和水汽通量輻合區(qū)內(nèi)。
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(wú)論旱澇年，青海高原空中凈水汽通量均呈正值，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(duì)流活動(dòng)的發(fā)展，水汽通量和水汽輻合都向高層發(fā)展，濕層明顯增厚。