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عمران::
شار گرمای محسوس
Changing fractions of latent and sensible heat fluxes caused by soil moisture variations can affect both near-surface air temperature and precipitation.
This decline in latent heat flux causes an enhancement of the fraction of net radiation that goes into sensible heat flux, which means that latent and sen- sible heat fluxes are negatively coupled.
Consequently, more heat is transported to the atmosphere, eventually increasing near-surface air temperature (positive cou- pling between sensible heat flux and temperature).
Another metric that includes both anomalies of sensible heat flux and temperature anomalies was introduced by Miralles et al
This alters the partitioning of net radiation Rnet into sensible heat flux SH, latent heat flux LH, and ground heat flux
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