FIELD: instrumentation.
SUBSTANCE: least radiation temperature is measured (Tr) for thermal radiation leaving upper areas of cloud cover, and also air temperature near Earth surface corresponding to the same area. They compare value of temperature Tr with the value of temperature (TI) of the sought-for isotherm. If Tr≤TI, then they additionally measure near-surface atmospheric pressure and determine dew point temperature. Using the produced data, they calculate air temperature (TA) in a convective cloud by altitudes with specified discrecity. The calculated value of temperature TA is compared with the value of temperature TI of the sought-for isotherm. If TA≤TI, then isotherm altitude is altitude of cloud air location at this step.
EFFECT: possibility to determine altitude of any isotherm in convective clouds, possibility to use the method for various areas and seasons without clarification of empirical coefficients.
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Authors
Dates
2015-04-27—Published
2013-05-06—Filed