From October to February the next year, the net surface heat flux is negative and net lateral heat transport is positive, but there is more heat lose than heat gain, then heat content in this area decreases.
从10月到次年2月,表面净热通量为负,中国东部近海从海表面失去的热量多于通过侧向输送净得到的热量,使得这些时间段内该海域的热收支为失多于收,热含量减少。
参考来源 - 中国东部近海热含量变化分析·2,447,543篇论文数据，部分数据来源于NoteExpress
The sea surface wind stress and net heat flux in the PN section affect the seasonal variation of the barrier layer depth by changing the mixed layer depth every season.
海面风场和净热通量场通过改变混合层的深度影响障碍层深度的季节变化，而海面降水对于季节平均的障碍层分布和变化都没有显著的影响。
The sea surface wind stress and net heat flux affect the seasonal variation of water mass character in the PN section by changing the mixed layer depth every season.
海面风场和净热通量场通过改变混合层的深度影响障碍层深度的季节变化，而海面降水对于季节平均的障碍层分布和变化都没有显著的影响。
应用推荐