FIELD: physics.
SUBSTANCE: radiant temperature of thermal flux from upper areas of the cloud cover, air temperature on the earth's surface and surface atmospheric pressure are measured and dew point is also determined. The obtained data are used to calculate air temperature in the convective cloud at heights with given sampling rate. The calculated temperature is compared with the measured radiant temperature of thermal flux from the upper areas of the cloud cover. If the radiant temperature of thermal flux from the upper areas of the cloud cover is equal to or higher than the calculated cloud air temperature at the given height, then the height of the upper boundary of the large convective cloud is the height of the cloud air at the given step.
EFFECT: simple method and wider spatial boundaries for application thereof.
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