z-logo
Premium
Intercalibration of CERES, MODIS, and MISR reflected solar radiation and its application to albedo trends
Author(s) -
Zhan Yizhe,
Davies Roger
Publication year - 2016
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2016jd025073
Subject(s) - spectroradiometer , moderate resolution imaging spectroradiometer , radiance , remote sensing , environmental science , shortwave , albedo (alchemy) , satellite , radiant energy , meteorology , radiative transfer , radiation , reflectivity , geography , physics , art , astronomy , performance art , optics , art history , quantum mechanics
Abstract Measurements on the Terra satellite by the Cloud and the Earth's Radiant Energy System (CERES), the Moderate Resolution Imaging Spectroradiometer (MODIS), and the Multiangle Imaging Spectroradiometer (MISR), between 2001 and 2015 over the polar regions, are analyzed in order to investigate the intercalibration differences between these instruments. Direct comparisons of colocated near‐nadir radiances from CERES, MODIS, and MISR show relative agreement within 2.4% decade −1 . By comparison with the CERES shortwave broadband, MODIS Collection 6 is getting brighter, by 1.0 ± 0.7% decade −1 in the red band and 1.4 ± 0.7% decade −1 in the near infrared. MISR's red and near‐infrared bands, however, show darkening trends of −1.0 ± 0.6% decade −1 and −1.1 ± 0.6% decade −1 , respectively. The CERES/MODIS or CERES/MISR visible and near IR radiance ratio is shown to have a significant negative correlation with precipitable water content over the Antarctic Plateau. The intercalibration results successfully correct the differential top‐of‐atmosphere trends in zonal albedos between CERES and MISR.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here