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contributor authorRichard M. Schulte
contributor authorChristian D. Kummerow
contributor authorChristian Klepp
contributor authorGerald G. Mace
date accessioned2023-04-12T18:26:10Z
date available2023-04-12T18:26:10Z
date copyright2022/09/01
date issued2022
identifier otherJAMC-D-21-0158.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289661
description abstractA significant part of the uncertainty in satellite-based precipitation products stems from differing assumptions about drop size distributions (DSDs). Satellite radar-based retrieval algorithms rely on DSD assumptions that may be overly simplistic, whereas radiometers further struggle to distinguish cloud water from rain. We utilize the Ocean Rainfall and Ice-phase Precipitation Measurement Network (OceanRAIN), version 1.0, dataset to examine the impact of DSD variability on the ability of satellite measurements to accurately estimate rates of warm rainfall. We use the binned disdrometer counts and a simple model of the atmosphere to simulate observations for three satellite architectures. Two are similar to existing instrument combinations on the GPM
publisherAmerican Meteorological Society
titleHow Accurately Can Warm Rain Realistically Be Retrieved with Satellite Sensors? Part I: DSD Uncertainties
typeJournal Paper
journal volume61
journal issue9
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/JAMC-D-21-0158.1
journal fristpage1087
journal lastpage1105
page1087–1105
treeJournal of Applied Meteorology and Climatology:;2022:;volume( 061 ):;issue: 009
contenttypeFulltext


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