Keywords
atmosphere
satellite
radiative forcing
How to Cite
Abstract
We describe the results of the study of aerosol optical depth (AOD) and Direct Radiative Forcing (DRF) at the top of the atmosphere (TOA), obtained in the period 2004 using the MODIS sensor of the TERRA satellite for Peru. Where it is observed that the AOD value can take maximum values around 0.5, resulting in aerosol DRF in the upper part of the atmosphere. The results indicate that the FRD is between [-5 0] W / m2.
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Copyright (c) 2022 Roberto Julio Angeles Vasquez, Julio Miguel Angeles Suazo, Nataly Angeles Suazo, Arlitt Lozano, Jose Flores Rojas