Mathematics – Logic
Scientific paper
Aug 2006
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006georl..3315816c&link_type=abstract
Geophysical Research Letters, Volume 33, Issue 15, CiteID L15816
Mathematics
Logic
13
Atmospheric Composition And Structure: Aerosols And Particles (0345, 4801, 4906), Atmospheric Processes: Remote Sensing, Atmospheric Processes: Radiative Processes, Oceanography: Biological And Chemical: Aerosols (0305, 4906)
Scientific paper
Most assessments of the direct climate forcing (DCF) of anthropogenic aerosols are from numerical simulations. However, recent advances in remote sensing techniques allow the separation of fine mode aerosols (anthropogenic aerosol is mostly fine aerosol) from coarse mode aerosols (largely marine and dust, which are mostly natural) from satellite data such as the Moderate Resolution Imaging SpectroRadiometer (MODIS). Here, by combining MODIS narrowband measurements with broadband radiative flux data sets from the Clouds and the Earth's Radiant Energy System (CERES), we provide a measurement-based assessment of the global direct climate forcing (DCF) of anthropogenic aerosols at the top of atmosphere (TOA) only for cloud free oceans. The mean TOA DCF of anthropogenic aerosols over cloud-free oceans [60N-60S] is -1.4 +/- 0.9 Wm-2, which is in excellent agreement (mean value of -1.4 Wm-2) with a recent observational study by Kaufman et al. [2005].
Christopher Sundar A.
Kaufman Yoram J.
Remer Lorraine A.
Zhang Jianglong
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