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Dry-to-Wet Soil Gradients Enhance Convection and Rainfall over Subtropical South America

dc.contributor.authorChug, Divyansh
dc.contributor.authorDominguez, Francina
dc.contributor.authorTaylor, Christopher M.
dc.contributor.authorKlein, Cornelia
dc.contributor.authorNesbitt, Stephen W.
dc.date.accessioned2024-12-24T15:01:17Z
dc.date.available2024-12-24T15:01:17Z
dc.date.copyright01 Sep. 2023
dc.date.issued2023
dc.identifier.otherhydr-JHM-D-23-0031.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4301691
dc.languageEnglish
dc.publisherAmerican Meteorological Society
dc.titleDry-to-Wet Soil Gradients Enhance Convection and Rainfall over Subtropical South America
dc.typeJournal Paper
dc.journal.volume24
dc.journal.issue9
dc.journal.titleJournal of Hydrometeorology
dc.identifier.doi10.1175/JHM-D-23-0031.1
dc.journal.fristpage1563
dc.journal.lastpage1581
dc.treeJournal of Hydrometeorology:;2023:;volume( 024 ):;issue: 009
dc.contenttypeFulltext


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