Over the Bay of Bengal, summertime latent heat release associated with deep convection exceeds longwave radiative cooling, resulting in intense heating in almost the whole troposphere.

• 夏季孟加拉湾地区的深对流凝结潜热释放远大于长波辐的冷却作用，因而整个对流层几乎都保持较强的非绝热加热。