Cb capillatus

Cloud with huge streaky mass. The all-day cumulogenesis formation was primarily due to an upper cut off low unable to move eastwards due to an anticyclone over Eastern Europe generating storm clouds from the still warm sea. The maritime nature of these clouds has been noted. This meant rapid decay upon moving over land due to these clouds being cut from their main source of energy and moisture. The following day also feautured the same weather.

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