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adiative effect of mineral dust on East Asian summer monsoon during the Last Glacial Maximum: role of snow-albedo feedback

descriptionPublicationkeyboard_double_arrow_right Article 30 Aug 2019Publisher:Zenodo
Authors: Zhengguo Shi;

doi: 10.5281/zenodo.3381764 , 10.5281/zenodo.3381765

adiative effect of mineral dust on East Asian summer monsoon during the Last Glacial Maximum: role of snow-albedo feedback

Abstract

Output data (surface temperature, precipitation, wind vector, etc) from three CAM4-BAM experiments (LGMndu, PDndu, LGMdu). LGM means Last glacial maximum. PD means present day. ndu means no dust feedback and du means dust feedback is enabled. Please see more in the publication.

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selected citations
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This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
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popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
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