this dissipation process limits the maximum surface change density on a planar surface to 30μc/. 这种耗散作用限制着物体平面的最大表面电荷密度为30c。
2.
Frictional dissipation and cutting off the water supply in the boundary layer by downslope adiabstic warming air are main mechanisms of terrain affecting tc intensity 而摩擦耗散作用和绝热增温的下坡干空气对边界层水汽的切断作用则是引起热带气旋减弱的主要机制。