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contributor authorRoman, Jacola
contributor authorKnuteson, Robert
contributor authorAckerman, Steve
date accessioned2017-06-09T17:09:43Z
date available2017-06-09T17:09:43Z
date copyright2014/11/01
date issued2014
identifier issn0894-8755
identifier otherams-80361.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223244
description abstracthis study determined the theoretical time-to-detect (TTD) global climate model (GCM) precipitable water vapor (PWV) 100-yr trends when realistic measurement errors are considered. Global trends ranged from 0.055 to 0.072 mm yr?1 and varied minimally from season to season. Global TTDs with a 0% measurement error ranged from 3.0 to 4.8 yr, while a 5% measurement error increased the TTD by almost 6 times, ranging from 17.6 to 22.0 yr. Zonal trends were highest near the equator; however, zonal TTDs were nearly independent of latitude when 5% measurement error was included. Zonal TTDs are significantly reduced when the trends are analyzed by season. Regional trends (15° ? 30°) show TTDs close to those in the 15° latitude zones (15° ? 360°). Detailed case study analysis of four selected regions with high population density?eastern United States, Europe, China, and India?indicated that trend analysis on regional spatial scales may provide the most timely information regarding highly populated regions when comparing detection time scales to global and zonal analyses.
publisherAmerican Meteorological Society
titleTime-to-Detect Trends in Precipitable Water Vapor with Varying Measurement Error
typeJournal Paper
journal volume27
journal issue21
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-13-00736.1
journal fristpage8259
journal lastpage8275
treeJournal of Climate:;2014:;volume( 027 ):;issue: 021
contenttypeFulltext


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