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本文尝试讨论观测到的温逆增现象,并且提供了浙江近海沿岸上升流温逆增的概念模式。文中指出,强温逆增在近岸斜坡上出现和沿岸上升流的存在有关。
This paper attempts to discuss the observed phenomenon of temperature exponential increase and provide a conceptual model of the inverse increase of the temperature rise of Zhejiang offshore coast. It is pointed out in the paper that the advent of strong tem- perature inversion is related to the presence of upwelling on the coastline.