On Bouchet's complementary hypothesis

被引:38
作者
Szilagyi, J [1 ]
机构
[1] Univ Nebraska, Div Conservat & Survey, Lincoln, NE 68588 USA
关键词
complementary hypothesis; areal evaporation; potential evaporation; wet surface evaporation;
D O I
10.1016/S0022-1694(01)00367-5
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Morton's proof of Bouchet's complementary hypothesis has been revisited. The proof's central assumption is that an increase in sensible heat from the surface to the air induces a similar increment in the sensible heat transfer from the air to a hypothetical potential evaporimeter. It is shown that this assumption is not necessary in thr derivation. Instead, the complementary hypothesis under simplified conditions can be obtained with the help of the mass conservation equation for water vapor. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:155 / 158
页数:4
相关论文
共 13 条
[1]  
[Anonymous], 1965, J HYDRAUL DIV, DOI DOI 10.1061/JYCEAJ.0001378
[2]  
BOUCHET R. J., 1963, Publ. Int. Ass. sci. Hydrol. 62 gen. Assembly Berkeley, P134
[3]   ADVECTION-ARIDITY APPROACH TO ESTIMATE ACTUAL REGIONAL EVAPOTRANSPIRATION [J].
BRUTSAERT, W ;
STRICKER, H .
WATER RESOURCES RESEARCH, 1979, 15 (02) :443-450
[4]   Hydrologic cycle explains the evaporation paradox [J].
Brutsaert, W ;
Parlange, MB .
NATURE, 1998, 396 (6706) :30-30
[5]  
Brutsaert W., 2013, Evaporation into the Atmosphere: Theory, History and Applications
[6]  
GOTZ G, 1981, DINAMIKUS METEOROLOG
[7]   Examination of two methods for estimating regional evaporation using a coupled mixed layer and land surface model [J].
Kim, CP ;
Entekhabi, D .
WATER RESOURCES RESEARCH, 1997, 33 (09) :2109-2116
[9]   AN ADVECTION-ARIDITY EVAPORATION MODEL [J].
PARLANGE, MB ;
KATUL, GG .
WATER RESOURCES RESEARCH, 1992, 28 (01) :127-132
[10]   NATURAL EVAPORATION FROM OPEN WATER, BARE SOIL AND GRASS [J].
PENMAN, HL .
PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1948, 193 (1032) :120-&