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contributor authorTsai, Jeng-Lin
contributor authorTsuang, Ben-Jei
contributor authorLu, Po-Sheng
contributor authorChang, Ken-Hui
contributor authorYao, Ming-Hwi
contributor authorShen, Yuan
date accessioned2017-06-09T16:30:14Z
date available2017-06-09T16:30:14Z
date copyright2010/04/01
date issued2009
identifier issn1525-755X
identifier otherams-69046.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210672
description abstractThe aerodynamic roughness, Bowen ratio, and friction velocity were measured over a rice paddy using tethersonde and eddy covariance (EC) systems. In addition, the height ranges of the atmospheric inertial sublayer (ISL) were derived using the tethersonde data. Comparison of the friction velocity, latent and sensible heat fluxes, and Bowen ratio estimated from these systems show their correlation coefficients to be >0.7. This difference between the observational systems can be associated with their respective footprint areas. The aerodynamic roughness was observed to be about 0.03 m for wind blowing from a paddy-dominated area (PDA) and about 0.37 m from a rice paddy interspersed with buildings (PIB) based on the ISL profile. Results are close to the effective roughness length model of Mason, having the same shear stresses at the blending height. In contrast, both the geometric mean model of Taylor and the arithmetic mean model of Tsai and Tsuang underestimate the effective roughness over the PIB. During daylight hours, the height range of the ISL ranged from a few meters to 25 m above ground level (AGL) for wind blowing from the PDA and 14?42 m for wind blowing from the PIB.
publisherAmerican Meteorological Society
titleMeasurements of Aerodynamic Roughness, Bowen Ratio, and Atmospheric Surface Layer Height by Eddy Covariance and Tethersonde Systems Simultaneously over a Heterogeneous Rice Paddy
typeJournal Paper
journal volume11
journal issue2
journal titleJournal of Hydrometeorology
identifier doi10.1175/2009JHM1131.1
journal fristpage452
journal lastpage466
treeJournal of Hydrometeorology:;2009:;Volume( 011 ):;issue: 002
contenttypeFulltext


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