Disclaimer: This material is being kept online for historical purposes. Though accurate at the time of publication, it is no longer being updated. The page may contain broken links or outdated information, and parts may not function in current web browsers. Visit https://espo.nasa.gov for information about our current projects.


Comparison of MISR and CERES top-of-atmosphere albedo

Sun, W., N. Loeb, R. Davies, C. Loukachine, and W. F. Miller (2006), Comparison of MISR and CERES top-of-atmosphere albedo, Geophys. Res. Lett., 33, L23810, doi:10.1029/2006GL027958.

The Clouds and the Earth’s Radiant Energy System (CERES) and the Multi-angle Imaging SpectroRadiometer (MISR) on Terra satellite measure the Earth’s top-ofatmosphere (TOA) albedo in broadband and narrowband, respectively. This study presents the first direct comparison of the CERES and MISR albedos. An algorithm for converting the MISR spectral albedos to broadband is derived. The MISR and CERES albedos for overcast ocean scenes are compared between 75°S – 75°N for solar zenith angles 75°. For overcast 1° × 1° ocean regions, the relative differences and the relative root-mean-square (RMS) differences between the MISR and CERES albedos are ~0.8% and ~4.3%, respectively. Accounting for a ~2.0% error in the MISR albedos due to narrowto-broadband albedo conversion errors, the RMS difference between the MISR and CERES albedos due to angular distribution model (ADM) differences is estimated to be ~3.8%. The remarkable consistency between the CERES and MISR albedos for overcast oceans suggests that both instrument teams have derived accurate corrections for the radiance anisotropy of cloud scenes. This consistency will strongly enhance the confidence in the temporal trends of cloud albedo measured by the CERES and have significant impact on climate studies.

PDF of Publication: 
Download from publisher's website.
Research Program: 
Radiation Science Program (RSP)