大气输送 meaning in Chinese

atmospheric transport

It can be found that a great quantity of vapor is transported to atmosphere from arctic ocean open sea in summer , which is very important to concerns on season change of heat budget on arctic ocean
由此可见，在北冰洋夏季，无冰海面有大量的水汽向大气输送，这对研究北冰洋地区大气边界层的季节变化过程是至关重要的。
Then basing the empirical formal proposed by weng burning , a method for reckon the average flux of energy transfer from ground surface to the air of a day according albedo and terrain parameters was put forwarded . it is considered that the flux is a proper index to decide if the area is a hot source or a cold source
然后，在翁笃鸣等提出的有关半经验公式的基础上，提出了根据反照率和地形参数计算高原地面向大气输送能量的日平均通量的算法，并以此作为判定冷热源的标准。