Field measurements of radiative flux divergence by means of direct method
Presented for the first time received direct method the original results of episodic and periodic measurements of longwave radiation flux divergence in natural conditions in the surface layer of the atmosphere. The measurements were made by the original divergence meter in the air a few inches thick layer in stable and unstable stratification, weak winds and low cloud cover, subject to the availability of meteorological support, during the expeditions of MGO.