The Impact of Cloud Optical Properties on Longwave Radiation in the Arctic

The surface energy budget of the Arctic is largely controlled by the net flow of solar and terrestrial radiation. Shortwave and longwave radiative fluxes are modulated by the surface properties, the vertical profiles of aerosols, water vapor, and, most importantly, clouds. The influence of a cloud o...

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Bibliographic Details
Main Authors: J. S. Delamere, E. J. Mlawer, S. A. Clough, K. H. Stamnes
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.298.2228
http://www.arm.gov/publications/proceedings/conf10/extended_abs/delamere_js.pdf
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Summary:The surface energy budget of the Arctic is largely controlled by the net flow of solar and terrestrial radiation. Shortwave and longwave radiative fluxes are modulated by the surface properties, the vertical profiles of aerosols, water vapor, and, most importantly, clouds. The influence of a cloud on the surface and top-of-the-atmosphere (TOA) irradiance is controlled by the cloud’s physical characteristics