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contributor authorReinhart, Brad
contributor authorFuelberg, Henry
contributor authorBlakeslee, Richard
contributor authorMach, Douglas
contributor authorHeymsfield, Andrew
contributor authorBansemer, Aaron
contributor authorDurden, Stephen L.
contributor authorTanelli, Simone
contributor authorHeymsfield, Gerald
contributor authorLambrigtsen, Bjorn
date accessioned2017-06-09T17:30:55Z
date available2017-06-09T17:30:55Z
date copyright2014/02/01
date issued2013
identifier issn0027-0644
identifier otherams-86554.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230125
description abstracthis study explores relationships between lightning, cloud microphysics, and tropical cyclone (TC) storm structure in Hurricane Karl (16 September 2010) using data collected by the NASA DC-8 and Global Hawk (GH) aircraft during NASA?s Genesis and Rapid Intensification Processes (GRIP) experiment. The research capitalizes on the unique opportunity provided by GRIP to synthesize multiple datasets from two aircraft and analyze the microphysical and kinematic properties of an electrified TC. Five coordinated flight legs through Karl by the DC-8 and GH are investigated, focusing on the inner-core region (within 50 km of the storm center) where the lightning was concentrated and the aircraft were well coordinated. GRIP datasets are used to compare properties of electrified and nonelectrified inner-core regions that are related to the noninductive charging mechanism, which is widely accepted to explain the observed electric fields within thunderstorms. Three common characteristics of Karl?s electrified regions are identified: 1) strong updrafts of 10?20 m s?1, 2) deep mixed-phase layers indicated by reflectivities >30 dBZ extending several kilometers above the freezing level, and 3) microphysical environments consisting of graupel, very small ice particles, and the inferred presence of supercooled water. These characteristics describe an environment favorable for in situ noninductive charging and, hence, TC electrification. The electrified regions in Karl?s inner core are attributable to a microphysical environment that was conducive to electrification because of occasional, strong convective updrafts in the eyewall.
publisherAmerican Meteorological Society
titleUnderstanding the Relationships between Lightning, Cloud Microphysics, and Airborne Radar-Derived Storm Structure during Hurricane Karl (2010)
typeJournal Paper
journal volume142
journal issue2
journal titleMonthly Weather Review
identifier doi10.1175/MWR-D-13-00008.1
journal fristpage590
journal lastpage605
treeMonthly Weather Review:;2013:;volume( 142 ):;issue: 002
contenttypeFulltext


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