当低涡远离高原后,非绝热加热减弱。
The diabatic heating decreased when the vortex moving away from the plateau.
这个定常解描述了非绝热加热、耗散、非线性平流和线性频散共同作用所形成的阻塞流型。
It describes a local blocking flow pattern developed under the joint action of nonadiabatic heating, dissipation, nonlinear advection and the linear dispersion.
在不考虑非绝热加热作用而只考虑地形的模拟实验中,索马里低空气流不能完整地模拟出来。
The experiment with only topography can not reproduce the Somali Jet fairlv, it further proves the relative importance of diabatic heating over the topography.
Now to make that happen, it's not adiabatic, right. If I wanted to do that, I'd need a heating element or something to cool, so I could make that temperature change happen, right.
要实现这点,它就不会是绝热的,对吧,如果我想做到这点,我需要一个加热元件或什么制冷的东西,这样我才能让温度变化。
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