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Observations have suggested that the 550‐nm aerosol optical depth (AOD) decreases over East Asia (EA) but increases over eastern United States (EUS) in boreal spring. Based on the NCEP CFSR reanalysis and TRMM 3A25 data set, the present work indicates that this asymmetry can be ascribed to the distinct feedback of general circulation and atmospheric heat source (AHS) between the two regions. In April...
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