On the other hand, the formation of the western Pacific subtropical anticyclone is mainly due to condensation heating associated with monsoon deep convection.Sensible heating decreases its intensity.

• 另一方面中低对流层西太平洋副高的形成则主要是由于季风降水引起的凝结潜热的作用，表面感热加热对其起着减弱的作用。