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dc.contributor.authorBraham, Roscoe R.
dc.date.accessioned2017-06-09T14:10:35Z
dc.date.available2017-06-09T14:10:35Z
dc.date.copyright1952/08/01
dc.date.issued1952
dc.identifier.issn0095-9634
dc.identifier.otherams-13916.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149419
dc.description.abstractA quantitative estimate, based upon data from the Thunderstorm Project, is made of the various water sources and sinks and the energy sources and sinks of an average thunderstorm cell. It is found that a large fraction of the water carried into the storm in vapor form is used to maintain the cold downdraft inside the storm, and that the energy restratification accompanying this downdraft is a major source of energy to the storm. From the estimates of the water and energy budgets, the following hypothesis is tested by means of radar measurements: the net energy available (energy sources minus energy sinks) is related to the amount of development of convective rainstorms.
dc.publisherAmerican Meteorological Society
dc.titleTHE WATER AND ENERGY BUDGETS OF THE THUNDERSTORM AND THEIR RELATION TO THUNDERSTORM DEVELOPMENT
dc.typeJournal Paper
dc.journal.volume9
dc.journal.issue4
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1952)009<0227:TWAEBO>2.0.CO;2
dc.journal.fristpage227
dc.journal.lastpage242
dc.treeJournal of Meteorology:;1952:;volume( 009 ):;issue: 004
dc.contenttypeFulltext


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