Description Usage Arguments Examples
lfc: Level of Free Convection el: Equilibrium Level Because shallow convection mixes the boundry layer before afternoon convection is initiated, it makes sense to graphically estimate mean values of mixing ratio and potential temperature and to use them to determine the LCL, LFC, and EL.
1 | thermodynamics.lfcel(Twbp, plcl, T, p)
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Twbp |
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plcl |
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T |
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p |
1 |
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