Inversion of temperature exists too ahead of warm fronts, and around thunderstorms'cold pool.
2.
This situation can be found with inversions of temperature aloft or rapid decrease of moisture with height.
3.
However, inversion of temperature exists ahead of warm fronts and the abnormal propagation echoes are then mixed with real rain.
4.
One can also observe sharp contrast between temperatures of the sunny and shady slopes, high diurnal range of temperature, inversion of temperature, and variability of rainfall based on altitude.
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