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contributor authorYi, Yonghong
contributor authorKimball, John S.
contributor authorJones, Lucas A.
contributor authorReichle, Rolf H.
contributor authorMcDonald, Kyle C.
date accessioned2017-06-09T16:40:05Z
date available2017-06-09T16:40:05Z
date copyright2011/08/01
date issued2011
identifier issn0894-8755
identifier otherams-71872.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213812
description abstracthe authors evaluated several land surface variables from the Modern-Era Retrospective Analysis for Research and Applications (MERRA) product that are important for global ecological and hydrological studies, including daily maximum (Tmax) and minimum (Tmin) surface air temperatures, atmosphere vapor pressure deficit (VPD), incident solar radiation (SWrad), and surface soil moisture. The MERRA results were evaluated against in situ measurements, similar global products derived from satellite microwave [the Advanced Microwave Scanning Radiometer for Earth Observing System (EOS) (AMSR-E)] remote sensing and earlier generation atmospheric analysis [Goddard Earth Observing System version 4 (GEOS-4)] products. Relative to GEOS-4, MERRA is generally warmer (~0.5°C for Tmin and Tmax) and drier (~50 Pa for VPD) for low- and middle-latitude regions (<50°N) associated with reduced cloudiness and increased SWrad. MERRA and AMSR-E temperatures show relatively large differences (>3°C) in mountainous areas, tropical forest, and desert regions. Surface soil moisture estimates from MERRA (0?2-cm depth) and two AMSR-E products (~0?1-cm depth) are moderately correlated (R ~ 0.4) for middle-latitude regions with low to moderate vegetation biomass. The MERRA derived surface soil moisture also corresponds favorably with in situ observations (R = 0.53 ± 0.01, p < 0.001) in the midlatitudes, where its accuracy is directly proportional to the quality of MERRA precipitation. In the high latitudes, MERRA shows inconsistent soil moisture seasonal dynamics relative to in situ observations. The study?s results suggest that satellite microwave remote sensing may contribute to improved reanalysis accuracy where surface meteorological observations are sparse and in cold land regions subject to seasonal freeze?thaw transitions. The upcoming NASA Soil Moisture Active Passive (SMAP) mission is expected to improve MERRA-type reanalysis accuracy by providing accurate global mapping of freeze?thaw state and surface soil moisture with 2?3-day temporal fidelity and enhanced (≤9 km) spatial resolution.
publisherAmerican Meteorological Society
titleEvaluation of MERRA Land Surface Estimates in Preparation for the Soil Moisture Active Passive Mission
typeJournal Paper
journal volume24
journal issue15
journal titleJournal of Climate
identifier doi10.1175/2011JCLI4034.1
journal fristpage3797
journal lastpage3816
treeJournal of Climate:;2011:;volume( 024 ):;issue: 015
contenttypeFulltext


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