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Using spatially and temporally collocated data sets from the Clouds and Earth's Radiant Energy System (CERES) and Moderate‐Resolution Imaging Spectroradiometer (MODIS) instruments on the Terra satellite, a new strategy is presented for studying the Shortwave Aerosol Radiative Forcing (SWARF) over the global oceans. Using collocated data, for September 2000, the global averaged optical thickness (τ 0.55 ) for cloud‐free CERES pixels is 0.07 with a SWARF of −6 Wm −2 . The τ 0.55 and SWARF values derived from two independent instruments are in excellent agreement with the following relationship: SWARF = 0.35 −105.34τ 0.55 +61.47τ 0.55 2 (0 ≤ τ 0.55 ≤ 0.7) Wm −2 . The synergistic use of the MODIS and CERES data sets can be used to provide independent estimates of SWARF, and can be used as a validation tool for studies that attempt to model the role of aerosols on climate.
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Christopher et al. (2002) studied this question.
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