As to the formation of the South Asian anticyclone, it is partly due to monsoon condensation heating;and partly due to the sensible heating over the Tibetan Plateau.

• 对流层上层的南亚高压的形成既与季风降水的潜热释放有关，也与青藏高原的感热加热有关，两者均起着增强南亚高压的作用。