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Stephen E. Lang and Wei-Kuo Tao

AGL. Fig . 16. As in Fig. 14 , but for heating rates at 7 km AGL. b. Heat balance and error estimation Without direct measurements of cloud heating, it can be difficult to validate the heating retrievals. Retrievals can be compared against heating budgets derived from intensive sounding networks associated with field campaigns, but these tend to be sporadic and there can be issues with sufficient satellite sampling within the sounding array. In the past, self-consistency checks have also been

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