Observational evidence on the effects of clouds and aerosols on net ecosystem exchange and evapotranspiration

Physics

Scientific paper

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Global Change: Biogeochemical Cycles, Processes, And Modeling (0412, 0414, 0793, 4805, 4912), Global Change: Land/Atmosphere Interactions (1218, 1843, 3322), Biogeosciences: Climate Dynamics (1620), Hydrology: Eco-Hydrology, Hydrology: Energy Budgets

Scientific paper

Clouds and aerosols control variations in the ratio of diffuse to total incident solar radiation (R d /R s ) and so determine to a large extent variations in both Light-Use Efficiency (LUE) and in the Evaporative Fraction (EF). Five years (2002-2007) of continuous ground measurements collected at twenty-three sites in the U.S. were analyzed to quantify this effect. Our results show that LUE is 19.4% and 203% larger for patchy clouds, and thick clouds than those for clear skies while LUE is about -6% for aerosols or thin clouds than those for clear skies. EF is 15.4%, 17.9% and 23.2% larger for aerosols or thin clouds, patchy clouds, and thick clouds than those for the clear sky when Eddy Covariance (ECOR) data are used, respectively. The values are 9.0%, 11.3% and 23.3% when Energy Balance Bowen Ratio (EBBR) data are used. This is the first systematic observational study on effects of R d /R s on EF and further study is needed.

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