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contributor authorKustas, W. P.
contributor authorJackson, T. J.
contributor authorSchmugge, T. J.
contributor authorParry, R.
contributor authorGoodrich, D. C.
contributor authorAmer, S. A.
contributor authorBach, L. B.
contributor authorKeefer, T. O.
contributor authorWeltz, M. A.
contributor authorMoran, M. S.
contributor authorClarke, T. R.
contributor authorPinter, P. J.
contributor authorClaassen, H.
contributor authorRiggs, A. C.
contributor authorStannard, D. I.
contributor authorHipps, L. E.
contributor authorSwiatek, E.
contributor authorBlanford, J. H.
contributor authorShutko, A. M.
contributor authorDoraiswamy, P. C.
contributor authorDaughtry, C. S. T.
contributor authorPerry, E. M.
contributor authorNichols, W. D.
contributor authorPinker, R. T.
contributor authorHuete, A. R.
contributor authorQi, J.
contributor authorvan Leeuwen, J. D.
contributor authorHumes, K. S.
contributor authorWashburne, J.
contributor authorChehbouni, A.
contributor authorVidal, A.
contributor authorGellman, D. I.
contributor authorClements, W. E.
contributor authorGrant, T. A.
contributor authorDubois, P.
contributor authorvan Zyl, J.
date accessioned2017-06-09T14:40:56Z
date available2017-06-09T14:40:56Z
date copyright1991/11/01
date issued1991
identifier issn0003-0007
identifier otherams-24370.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161035
description abstractArid and semiarid rangelands comprise a significant portion of the earth's land surface. Yet little is known about the effects of temporal and spatial changes in surface soil moisture on the hydrologic cycle, energy balance, and the feedbacks to the atmosphere via thermal forcing over such environments. Understanding this interrelationship is crucial for evaluating the role of the hydrologic cycle in surface-atmosphere interactions. This study focuses on the utility of remote sensing to provide measurements of surface soil moisture, surface albedo, vegetation biomass, and temperature at different spatial and temporal scales. Remote-sensing measurements may provide the only practical means of estimating some of the more important factors controlling land surface processes over large areas. Consequently, the use of remotely sensed information in biophysical and geophysical models greatly enhances their ability to compute fluxes at catchment and regional scales on a routine basis. However, model calculations for different climates and ecosystems need verification. This requires that the remotely sensed data and model computations be evaluated with ground-truth data collected at the same areas scales. The present study (MONSOON 90) attempts to address this issue for semiarid rangelands. The experimental plan included remotely sensed data in the visible, near-infrared, thermal, and microwave wavelengths from ground and aircraft platforms and, when available, from satellites. Collected concurrently were ground measurements of soil moisture and temperature, energy and water fluxes, and profile data in the atmospheric boundary layer in a hydrologically instrumented semiarid rangeland watershed. Field experiments were conducted in 1990 during the dry and wet or ?monsoon season? for the southwestern United States. A detailed description of the field campaigns, including measurements and some preliminary results are given.
publisherAmerican Meteorological Society
titleAn Interdisciplinary Field Study of the Energy and Water Fluxes in the Atmospheric-Biosphere System over Semiarid Rangelands: Description and Some Preliminary Results
typeJournal Paper
journal volume72
journal issue11
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/1520-0477(1991)072<1683:AIFSOT>2.0.CO;2
journal fristpage1683
journal lastpage1705
treeBulletin of the American Meteorological Society:;1991:;volume( 072 ):;issue: 011
contenttypeFulltext


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