Combining the dissipation method and surface renewal analysis to estimate scalar fluxes from the time traces over rangeland grass near Ione (California)
- 14 January 2009
- journal article
- research article
- Published by Wiley in Hydrological Processes
- Vol. 23 (6) , 842-857
- https://doi.org/10.1002/hyp.7223
Abstract
No abstract availableKeywords
This publication has 67 references indexed in Scilit:
- Surface energy-balance closure over rangeland grass using the eddy covariance method and surface renewal analysisAgricultural and Forest Meteorology, 2008
- Processing and quality control of flux data during LITFASS-2003Boundary-Layer Meteorology, 2006
- 50 Years of the Monin–Obukhov Similarity TheoryBoundary-Layer Meteorology, 2006
- Monin–Obukhov Similarity Functions of the Structure Parameter of Temperature and Turbulent Kinetic Energy Dissipation Rate in the Stable Boundary LayerBoundary-Layer Meteorology, 2005
- Roughness layer corrections with emphasis on SVAT model applicationsAgricultural and Forest Meteorology, 2004
- Micrometeorological fluxes under the influence of regional and local advection: a revisitAgricultural and Forest Meteorology, 2004
- Estimation of Momentum and Heat Fluxes Using Dissipation and Flux‐Variance Methods in the Unstable Surface LayerWater Resources Research, 1996
- Flux-gradient relationships above tall plant canopiesAgricultural and Forest Meteorology, 1992
- Temperature Ramps in the Atmospheric Surface LayerJournal of the Atmospheric Sciences, 1979
- A new approach to the measurement of turbulent fluxes in the lower atmosphereJournal of Fluid Mechanics, 1961