Analysis of the relationship between bare soil evaporation and soil moisture simulated by 13 land surface schemes for a simple non-vegetated site

被引:43
作者
Desborough, CE [1 ]
Pitman, AJ [1 ]
Irannejad, P [1 ]
机构
[1] MACQUARIE UNIV,SCH EARTH SCI,CLIMAT IMPACTS CTR,N RYDE,NSW 2109,AUSTRALIA
基金
澳大利亚研究理事会;
关键词
D O I
10.1016/0921-8181(95)00036-4
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Atmospheric and land surface data collected from the HAPEX-MOBILHY field experiment were used to compare the bare soil evaporation simulations of 13 land surface schemes and to examine the relationship between differences in evaporation and differences in soil moisture. For a 120-day period in which there was no vegetation present, computed total evaporation ranged between 100 and 250 mm. This large range in evaporation was not related to soil moisture differences. Prescribing surface soil moisture and temperature did not reduce the range in evaporation and instead the range was increased. The models' predictions of evaporation were in closer agreement with each other when they were allowed to select their own surface conditions than when they were forced to use the same conditions. The bare soil evaporation formulations used by the land-surface schemes are not consistent with each other and these inconsistencies produce widely-varying bare soil evaporation rates, The range in bare soil evaporation is unlikely to be reduced by improving the simulation of soil moisture and instead an assessment of why the bare soil evaporation formulations are inconsistent is required.
引用
收藏
页码:47 / 56
页数:10
相关论文
共 47 条
[1]  
[Anonymous], 1965, 19 S SOC EXPT BIOL
[2]  
[Anonymous], 1993, SCALING PHYSL PROCES
[3]  
[Anonymous], MON WEATHER REV
[4]  
DICKINSON RE, 1986, TN275PLUSSTR NCAR
[5]  
DICKINSON RE, 1993, TN383PLUSSTR NCAR
[6]  
DUCOUDRE NI, 1993, J CLIMATE, V6, P248, DOI 10.1175/1520-0442(1993)006<0248:SANSOP>2.0.CO
[7]  
2
[8]  
GOUTORBE JP, 1992, LAND SURFACE EVAPORA, P403
[9]  
HANSEN J, 1983, MON WEATHER REV, V111, P609, DOI 10.1175/1520-0493(1983)111<0609:ETDGMF>2.0.CO
[10]  
2