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dc.contributor.authorJoseph A. Finlon
dc.contributor.authorLynn A. McMurdie
dc.contributor.authorRandy J. Chase
dc.date.accessioned2023-04-12T18:35:04Z
dc.date.available2023-04-12T18:35:04Z
dc.date.copyright2022/10/14
dc.date.issued2022
dc.identifier.otherJAS-D-21-0311.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289919
dc.description.abstractMultifrequency airborne radars have become instrumental in evaluating the performance of satellite retrievals and furthering our understanding of ice microphysical properties. The dual-frequency ratio (DFR) is influenced by the size, density, and shape of ice particles, with higher values associated with the presence of larger ice particles that may have implications regarding snowfall at the surface. The Investigation of Microphysics and Precipitation for Atlantic Coast-Threatening Snowstorms (IMPACTS) field campaign involves the coordination of remote sensing measurements above winter midlatitude cyclones from an ER-2 aircraft to document the fine-scale precipitation structure spanning four radar (X-, Ku-, Ka-, and W-band) frequencies and in situ microphysical measurements from a P-3 aircraft that provide additional insight into the particle size distribution (PSD) behavior and habits of the hydrometeors related to the DFR. A novel approach to identify regions of prominently higher Ku- and Ka-band DFR at the P-3 location for five coordinated flights is presented. The solid-phase mass-weighted mean diameter (
dc.publisherAmerican Meteorological Society
dc.titleInvestigation of Microphysical Properties within Regions of Enhanced Dual-Frequency Ratio during the IMPACTS Field Campaign
dc.typeJournal Paper
dc.journal.volume79
dc.journal.issue10
dc.journal.titleJournal of the Atmospheric Sciences
dc.identifier.doi10.1175/JAS-D-21-0311.1
dc.journal.fristpage2773
dc.journal.lastpage2795
dc.page2773–2795
dc.treeJournal of the Atmospheric Sciences:;2022:;volume( 079 ):;issue: 010
dc.contenttypeFulltext


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