2010
DOI: 10.13031/2013.30081
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Surface Aerodynamic Temperature Modeling over Rainfed Cotton

Abstract: Evapotranspiration (ET) or latent heat flux (LE) can be spatially estimated as an energy balance (EB) residual for land surfaces using remote sensing inputs. The EB equation requires the estimation of net radiation (R n), soil heat flux (G), and sensible heat flux (H). R n and G can be estimated with an acceptable accuracy. In computing H, radiometric surface temperature (T s) is often used instead of surface aerodynamic temperature (T o), as T o is neither measured nor easily estimated. This may cause an unde… Show more

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Cited by 14 publications
(2 citation statements)
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“…In a study over rainfed cotton subjected to a highly advective environment, in the Texas High Plains, near Bushland, Texas, USA, Chávez et al (2010) , or -4.9±16.3%); which resulted in an improvement of the estimation of latent heat fluxes (error -6±35 W m -2 , or -1.8±9.7%). It seems that incorporating the interactions between the crop row layout and wind direction, in the modelling of T o , better describes the dynamic turbulent mixing for the generation of H.…”
Section: Cotton T O Modelling-dryland Agriculture Casementioning
confidence: 99%
“…In a study over rainfed cotton subjected to a highly advective environment, in the Texas High Plains, near Bushland, Texas, USA, Chávez et al (2010) , or -4.9±16.3%); which resulted in an improvement of the estimation of latent heat fluxes (error -6±35 W m -2 , or -1.8±9.7%). It seems that incorporating the interactions between the crop row layout and wind direction, in the modelling of T o , better describes the dynamic turbulent mixing for the generation of H.…”
Section: Cotton T O Modelling-dryland Agriculture Casementioning
confidence: 99%
“…Some of the fundamental challenges in ET mapping through SEB models have evolved due to, (i) the inequality between LST and the aerodynamic temperature (T 0 ), which is essentially responsible for the exchanges of H [124,125,148,149]; (ii) a non-unique relationship between T 0 and LST due to differences between the roughness lengths (i.e., effective source/sink heights) for momentum (z 0M ) and heat (z 0H ) within vegetation canopy and substrate complex [124,[150][151][152]; (iii) the unavailability of a universally agreed model to estimate spatially explicit T 0 [125,153]; (iv) the lack of a physical-based or analytical g A model as a true representative for spatial application [124,125]; (v) complexities in g A parameterization to accommodate the differences between the scalar roughness lengths of heat (z 0H ) and momentum (z 0M ) transfer. Such parameterizations are significantly affected by land-surface heterogeneity and could cause the ET severely overestimated in the semi-arid or arid ecosystems.…”
Section: Et Modelingmentioning
confidence: 99%