摘要
本文用相关分析的方法,讨论了引起北太平洋中纬度地区冬半年月平均海温变化的两类过程。第一类过程是通过海洋向大气的潜热、感热输送,引起海洋混合层中热贮存量的变化。第二类过程发生在海洋内部。分析表明,这两类过程对海温变化都有比较重要的作用。
Based on linear correlation techniques, the SST changes due to two categories of processes have been discussed. The first one acts through the ocean surface such as latent heat transfer and sensible heat transfer which induce the change of the heat storage in the oceanic mixed layer. The second process acts whthin the water mass. The results show that two processes a relatively significant role in the SST changes.
出处
《热带气象》
CSCD
1991年第1期26-32,共7页
基金
高等学校博士学科点专项科研基金资助
