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contributor authorGedzelman, Stanley David
contributor authorLawrence, James R.
date accessioned2017-06-09T13:59:02Z
date available2017-06-09T13:59:02Z
date copyright1982/10/01
date issued1982
identifier issn0021-8952
identifier otherams-10352.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145460
description abstractThe deuterium/hydrogen ratios δD of sequential samples of precipitation at Palisades, New York were measured during four separate storms during January 1978. The values ranged from a low of ?177? to a high of ?30?. For each of the storms there was a general increase of δD values with time. The changes of δD values are explained by means of detailed meteorological analysis assuming that the precipitation derives from a Rayleigh condensation process in which all condensation in the air column directly above the station is assumed to fall immediately to the ground. The resulting calculated values of δD usually agree to within 5? of the observed measured values.
publisherAmerican Meteorological Society
titleThe Isotopic Composition of Cyclonic Precipitation
typeJournal Paper
journal volume21
journal issue10
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1982)021<1385:TICOCP>2.0.CO;2
journal fristpage1385
journal lastpage1404
treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 010
contenttypeFulltext


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