Summation principle: Difference between revisions
From Glossary of Meteorology
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The principle that the [[sky cover]] at any level is equal to the summation of the sky cover in the lowest layer, plus the additional sky cover in all successively higher layers up to and including the layer in question. | |||
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Latest revision as of 08:32, 30 March 2024
The principle that the sky cover at any level is equal to the summation of the sky cover in the lowest layer, plus the additional sky cover in all successively higher layers up to and including the layer in question.