文中根据线性化的大气方程组求得了城市热岛环流的理论模式。
The linearized atmospheric equation system is solved analytically to obtain a theoretical model of the urban heat island circulation.
结果表明，纯粹的海陆风环流或热岛环流触发对流天气的可能性不大。
The result indicates that the probability of causing strong convective activity both in pure sea breeze and pure UHI is small.
本文提出了城市次生热岛效应可导致局地次生尺度环流结构，形成区域性辐合或辐散结构。
Effect of urban heat island can produce local secondary circulation and form regional convergence and divergence structure.
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