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example, the released latent heat is one of the major sources driving the atmospheric general circulation as well as the circulation within the tropics (e.g., Ramage 1968 ; Chang and Lau 1982 ), and the Rossby wave trains that emanate from the convection distort atmospheric flow patterns at higher latitudes (e.g., Stan et al. 2017 ; Yang et al. 2019 ). Numerous field experiments have been conducted that have greatly improved understanding of the convective activity and associated circulations over
example, the released latent heat is one of the major sources driving the atmospheric general circulation as well as the circulation within the tropics (e.g., Ramage 1968 ; Chang and Lau 1982 ), and the Rossby wave trains that emanate from the convection distort atmospheric flow patterns at higher latitudes (e.g., Stan et al. 2017 ; Yang et al. 2019 ). Numerous field experiments have been conducted that have greatly improved understanding of the convective activity and associated circulations over
passage of the MJO. They partitioned the heating into convective, stratiform, and radiative components, and found that with the onset of the MJO, the stratiform rainfall anomalies lagged the convective anomalies by a few days. In most numerical weather or climate models, the diabatic heating is calculated as an explicit potential temperature tendency. Depending on the formulation of the model, the heating will arise from the microphysics scheme, the cumulus scheme, the planetary boundary layer scheme
passage of the MJO. They partitioned the heating into convective, stratiform, and radiative components, and found that with the onset of the MJO, the stratiform rainfall anomalies lagged the convective anomalies by a few days. In most numerical weather or climate models, the diabatic heating is calculated as an explicit potential temperature tendency. Depending on the formulation of the model, the heating will arise from the microphysics scheme, the cumulus scheme, the planetary boundary layer scheme
