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contributor authorSantanello, Joseph A.
contributor authorPeters-Lidard, Christa D.
contributor authorKumar, Sujay V.
contributor authorAlonge, Charles
contributor authorTao, Wei-Kuo
date accessioned2017-06-09T16:30:07Z
date available2017-06-09T16:30:07Z
date copyright2009/06/01
date issued2009
identifier issn1525-755X
identifier otherams-69007.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210629
description abstractLand?atmosphere interactions play a critical role in determining the diurnal evolution of both planetary boundary layer (PBL) and land surface temperature and moisture states. The degree of coupling between the land surface and PBL in numerical weather prediction and climate models remains largely unexplored and undiagnosed because of the complex interactions and feedbacks present across a range of scales. Furthermore, uncoupled systems or experiments [e.g., the Project for the Intercomparison of Land-Surface Parameterization Schemes (PILPS)] may lead to inaccurate water and energy cycle process understanding by neglecting feedback processes such as PBL-top entrainment. In this study, a framework for diagnosing local land?atmosphere coupling is presented using a coupled mesoscale model with a suite of PBL and land surface model (LSM) options along with observations during field experiments in the U.S. Southern Great Plains. Specifically, the Weather Research and Forecasting Model (WRF) has been coupled to the Land Information System (LIS), which provides a flexible and high-resolution representation and initialization of land surface physics and states. Within this framework, the coupling established by each pairing of the available PBL schemes in WRF with the LSMs in LIS is evaluated in terms of the diurnal temperature and humidity evolution in the mixed layer. The coevolution of these variables and the convective PBL are sensitive to and, in fact, integrative of the dominant processes that govern the PBL budget, which are synthesized through the use of mixing diagrams. Results show how the sensitivity of land?atmosphere interactions to the specific choice of PBL scheme and LSM varies across surface moisture regimes and can be quantified and evaluated against observations. As such, this methodology provides a potential pathway to study factors controlling local land?atmosphere coupling (LoCo) using the LIS?WRF system, which will serve as a test bed for future experiments to evaluate coupling diagnostics within the community.
publisherAmerican Meteorological Society
titleA Modeling and Observational Framework for Diagnosing Local Land–Atmosphere Coupling on Diurnal Time Scales
typeJournal Paper
journal volume10
journal issue3
journal titleJournal of Hydrometeorology
identifier doi10.1175/2009JHM1066.1
journal fristpage577
journal lastpage599
treeJournal of Hydrometeorology:;2009:;Volume( 010 ):;issue: 003
contenttypeFulltext


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