NIGHTTIME EVAPOTRANSPIRATION VS DAYTIME AND 24-H EVAPOTRANSPIRATION

被引:36
作者
MALEK, E
机构
[1] Department of Plants, Soils and Biometeorology, Utah State University, Logan
关键词
D O I
10.1016/0022-1694(92)90159-S
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The continuous measurement of night-time ET(a,n) (sunset to sunrise), daytime ET(a,d) (sunrise to sunset) and 24 h ET(a,24 h) alfalfa evapotranspiration was carried out, using the Bowen ratio-energy balance method, in a closed mountainous semi-arid irrigated valley in northern Utah. The results indicate that ET(a,n)/ET(a,24 h) was 2.93 mm/173.87 mm, or about 1.7%, during a complete growing cycle of alfalfa in August and September 1991. The results also show that this ratio could be very high (about 14%) when the night-time wind speed is high.
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页码:119 / 129
页数:11
相关论文
共 11 条
[1]   The ratio of heat losses by conduction and by evaporation from any water surface [J].
Bowen, IS .
PHYSICAL REVIEW, 1926, 27 (06) :779-787
[2]  
BRUTSAERT W, 1988, EVAPORATION ATMOSPHE
[3]  
Hanks R. J., 1980, APPLIED SOIL PHYSICS
[4]  
Hill R. W., 1983, COMP EQUATIONS USED
[5]  
JENSEN ME, 1990, ASCE70 MAN REP ENG P
[6]   EVAPOTRANSPIRATION FROM THE MARGIN AND MOIST PLAYA OF A CLOSED DESERT VALLEY [J].
MALEK, E ;
BINGHAM, GE ;
MCCURDY, GD .
JOURNAL OF HYDROLOGY, 1990, 120 (1-4) :15-34
[7]  
MALEK E, 1992, IN PRESS BOUNDARY LA
[8]  
MALEK E, 1992, IN PRESS IRRIG SCI
[9]  
MONTEITH JL, 1990, PRINCIPLES ENV PHYSI
[10]  
OKE TR., 1987, BOUNDARY LAYER CLIMA, DOI DOI 10.4324/9780203407219