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AGU: Water Resources Research

 

Index Terms

  • Meteorology and Atmospheric Dynamics: Boundary layer processes
  • Meteorology and Atmospheric Dynamics: Land/atmosphere interactions
  • Hydrology: Evapotranspiration

Abstract

WATER RESOURCES RESEARCH, VOL. 38, 1084, 9 PP., 2002
doi:10.1029/2001WR000486

A method based on high-frequency temperature measurements to estimate the sensible heat flux avoiding the height dependence

F. Castellví

Department de Medi Ambient i Cienciès del Sòl, E.T.S. Enginyeria Agrària, Universitat de Lleida, Lleida, Spain

P. J. Perez

Department de Medi Ambient i Cienciès del Sòl, E.T.S. Enginyeria Agrària, Universitat de Lleida, Lleida, Spain

M. Ibañez

Department de Medi Ambient i Cienciès del Sòl, E.T.S. Enginyeria Agrària, Universitat de Lleida, Lleida, Spain

A new method to estimate the sensible heat flux H using high-frequency temperature data has been proposed. The new method proposes to scale the mean eddy vertical velocity responsible for the air parcels renewal using similarity formulae. It is shown that the empirical coefficient resulting from this scaling (apparently height dependant) is relatively constant with height when comparing estimated versus measured H over half hour periods. This work suggests that the coefficient is universal. This allows to us to propose a new method that provides useful advantages for field applications.

Published 25 June 2002.

Citation: Castellví, F., P. J. Perez, and M. Ibañez (2002), A method based on high-frequency temperature measurements to estimate the sensible heat flux avoiding the height dependence, Water Resour. Res., 38(6), 1084, doi:10.1029/2001WR000486.

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