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通过简化原始运动方程，得到南海北部季风逆风流诊断方程，对季风逆风流诊断方程进行必要的数学处理后，导出南海北部产生季风逆风流的必要条件和诊断判据；指出南海北部季风逆风流由风生直接逆风流与风生间接逆风流叠加而成，风生间接过风流由风生间接正压地转逆风流与风生间接斜压地转逆风流组成，还导出风致巴士海峡以东的黑潮水影响季风逆风流的判据，在合适的风向及适当的摩擦系数情况下，黑潮水可成为间接逆风流的热源。并首次提出风生直接逆风流、风生间接逆风流、正压逆风流、斜压逆风流、风生间接正压地转逆风流和风生间接斜压地转逆风流概念。
By simplifying the original equations of motion, the monsoon inverse wind flow diagnosis equation is obtained in the northern South China Sea. After the necessary mathematical treatment of the monsoon inverse wind flow diagnosis equation is derived, the necessary conditions and diagnostic criteria for the generation of the monsoon upwind flow in the northern South China Sea are derived. The windward direct reverse wind and the windward indirect windward superposition, the wind indirect indirect windward windward indirect positive pressure reverse windward and wind indirect indirect pressure turnaround windward composition, but also leads to wind to the east of the Strait of Strait The Kuroshio water influences the criterion of the monsoon upwind, and the Kuroshio can become a source of indirect reverse wind flow in proper wind direction and proper friction coefficient. And for the first time put forward the wind and wind direct reverse winds, wind indirect indirect wind flow, positive pressure inverse wind flow, baroclinic wind flow, wind indirectly positive pressure reverse wind and indirect wind pressure indirect wind flow concept.