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contributor authorShinoda, M.
contributor authorYamaguchi, Y.
date accessioned2017-06-09T16:17:34Z
date available2017-06-09T16:17:34Z
date copyright2003/04/01
date issued2003
identifier issn1525-755X
identifier otherams-65147.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206340
description abstractThe influence of the Sahelian drought and resultant soil moisture deficit on air temperature is explored, using a simple water balance model that was validated with multiyear observations of the root-zone soil moisture. A comparison between wet soil years in the 1950s to 1960s and dry soil years in the 1970s to 1980s demonstrated a series of processes by which precipitation anomalies during the rainy season of a few months influence the time-lagging temperature through soil moisture. These processes were clearly seen only during the beginning 1 or 2 months of the dry season, and then both the concurrent soil moisture and temperature anomalies disappeared. Thus, the timescale of the drying up of root-zone soil moisture anomalies was determined to be approximately 1.5 months. This suggests that the root-zone soil moisture does not act as a memory of rainfall anomaly into the following rainy season and is not related to the long-term persistence of the drought.
publisherAmerican Meteorological Society
titleInfluence of Soil Moisture Anomaly on Temperature in the Sahel: A Comparison between Wet and Dry Decades
typeJournal Paper
journal volume4
journal issue2
journal titleJournal of Hydrometeorology
identifier doi10.1175/1525-7541(2003)4<437:IOSMAO>2.0.CO;2
journal fristpage437
journal lastpage447
treeJournal of Hydrometeorology:;2003:;Volume( 004 ):;issue: 002
contenttypeFulltext


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