A comparison of new and existing equations for estimating sensible heat flux using surface renewal and similarity concepts

被引:19
作者
Castellvi, F.
Snyder, R. L.
Baldocchi, D. D.
Martinez-Cob, A.
机构
[1] Univ Lleida, Dept Medi Ambient & Ciencies Sol, E-25198 Lleida, Spain
[2] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA
[3] Univ Calif Berkeley, Dept Environm Sci Policy & Management, Berkeley, CA 94720 USA
[4] CSIC, Dept Genet & Prod Vegetal, Estac Expt Aula Dei, E-50080 Zaragoza, Spain
关键词
D O I
10.1029/2005WR004642
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
[ 1] This paper describes two approaches for estimating sensible heat flux, using surface renewal and similarity concepts. One approach depends on a temperature structure function parameter and is valid in the inertial sublayer. The other approach depends on the temperature standard deviation and operates when measurements are made above the canopy top, either in the roughness or inertial sublayer. The approaches were tested over grass, rangeland grass, wheat, grape vineyard, and nectarine and olive orchards. It is shown that the free convection limit expression for the standard deviation method holds for slightly unstable conditions. When surface homogeneity and fetch requirements are not fully met in the field, the results show that the equations based on surface renewal principles are more robust and accurate than equations exclusively based on similarity backgrounds. It is likely that the two methods are less sensitive to site-specific adjustment of the similarity relationships unless the canopy is rather heterogeneous. Under unstable conditions, the free convection limit equation, which depends on the temperature standard deviation, can provide online sensible heat flux estimates using affordable battery-powered data logger with temperature data as the only input. The approach performed well when measuring above the canopy in the roughness and inertial sublayers, thus suggesting that the method is useful for long-term monitoring over growing vegetation.
引用
收藏
页数:18
相关论文
共 50 条
[1]  
Allen R. G., 1998, FAO Irrigation and Drainage Paper
[2]  
ALLEN RG, 1996, HYDROLOGY HDB ASCE M, V28, P125
[3]   A micrometeorological investigation of a restored California wetland ecosystem [J].
Anderson, FE ;
Snyder, RL ;
Miller, RL ;
Drexler, J .
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2003, 84 (09) :1170-1172
[4]  
[Anonymous], AGR FOREST METEOROL, DOI DOI 10.1016/0168-1923(94)02182-J
[5]   TEMPERATURE STRUCTURE IN THE ATMOSPHERIC SURFACE-LAYER .2. THE BUDGET OF MEAN CUBE FLUCTUATIONS [J].
ANTONIA, RA ;
CHAMBERS, AJ ;
BRADLEY, EF .
BOUNDARY-LAYER METEOROLOGY, 1981, 20 (03) :293-307
[6]   Flux footprints within and over forest canopies [J].
Baldocchi, D .
BOUNDARY-LAYER METEOROLOGY, 1997, 85 (02) :273-292
[7]   How plant functional-type, weather, seasonal drought, and soil physical properties alter water and energy fluxes of an oak-grass savanna and an annual grassland [J].
Baldocchi, DD ;
Xu, LK ;
Kiang, N .
AGRICULTURAL AND FOREST METEOROLOGY, 2004, 123 (1-2) :13-39
[8]  
Brutsaert W., 1982, Evaporation into the atmosphere: Theory, history, and applications, DOI [DOI 10.1007/978-94-017-1497-6, 10.1007/978-94-017-1497-6]
[9]  
BUSINGER JA, 1971, J ATMOS SCI, V28, P181, DOI 10.1175/1520-0469(1971)028<0181:FPRITA>2.0.CO
[10]  
2