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Cloud and aerosol contributions to variation in shortwave surface irradiance over East Asia in July during 2001 and 2007
It is important to clarify the contributions of clouds and aerosols to the variation of surface shortwave irradiance ( S) for climatological studies. This study examined the contributions of clouds and aerosols to the variation in S over East Asia (75–135°E, 20–55°N) in July during 2001 and 2007 usi...
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Published in: | Journal of quantitative spectroscopy & radiative transfer 2011, Vol.112 (2), p.329-337 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | It is important to clarify the contributions of clouds and aerosols to the variation of surface shortwave irradiance (
S) for climatological studies. This study examined the contributions of clouds and aerosols to the variation in
S over East Asia (75–135°E, 20–55°N) in July during 2001 and 2007 using the index of potential radiative forcing (PRF) to characterize the temporal and geographical variations. After confirming the validity of PRF for multiyear analyses, we performed several temporal analyses of clouds and aerosols over the whole research domain. Changes in the geographical distribution, contribution histograms, and averaged values were studied. In agreement with previous studies that treated single-year cases, we confirmed that the magnitudes of the temporal changes in
S variations due to clouds and aerosols were highly variable geographically. As for domain-averaged
S variations, we did not observe defined trends for the research period. It was also found that the temporal variation between one parameter and its
S variation was negatively correlated, from the point analyses at two locations. Based on these results, we concluded that PRF is a promising tool for research into long-term
S variations. This kind of information will be quite valuable as basic data for use in climate modeling. |
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ISSN: | 0022-4073 1879-1352 |
DOI: | 10.1016/j.jqsrt.2010.08.002 |