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contributor authorSelvam, A. Mary
contributor authorManohar, G. K.
contributor authorKhemani, L. T.
contributor authorMurty, Bh V. Ramana
date accessioned2017-06-09T14:19:50Z
date available2017-06-09T14:19:50Z
date copyright1977/11/01
date issued1977
identifier issn0022-4928
identifier otherams-17378.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153265
description abstractSimultaneous measurements of raindrop charge, atmospheric electric field and rain intensity were made at Poona using fast response, continuous recording surface instruments during four types of rain: pre-monsoon (thunderstorm rain), monsoon rain type I (tight intermittent rain), monsoon rain type II (heavy continuous rain) and post-monsoon (thunderstorm rain). Measurements were also made of the conductivity of rainwater samples collected during the monsoon season. On some days of this period data on cloud thickness as obtained from the aircraft flights in the region were also available. The electric field associated with negatively charged raindrops was less negative than that associated with positively charged drops. The raindrop charge spectrum showed different characteristics during the four types of rain studied. It was broadest during the pre-monsoon rain when the convective activity was a maximum. It followed a log-normal distribution during the monsoon rain type I and it was peaked and skewed to the positive side during the monsoon rain type II. Rainwater conductivity was inversely correlated with the cloud vertical thickness. The results of the present study support the warm cloud charge generation mechanism proposed by Takahashi (1974).
publisherAmerican Meteorological Society
titleCharacteristics of Raindrop Charge and Associated Electric Field in Different Types of Rain
typeJournal Paper
journal volume34
journal issue11
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1977)034<1791:CORCAA>2.0.CO;2
journal fristpage1791
journal lastpage1796
treeJournal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 011
contenttypeFulltext


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