ANALYSIS OF THE RELATIONSHIP BETWEEN BARE SOIL EVAPORATION AND SOIL-MOISTURE SIMULATED BY 13 LAND-SURFACE SCHEMES FOR A SIMPLE NON-VEGETATED SITE

Atmospheric and land surface data collected from the HAPEX-MOBILHY fie ld experiment were used to compare the bare soil evaporation simulatio ns 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 e vaporation ranged between 100 and 250 mm. This large range in evaporat ion 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 evapor ation were in closer agreement with each other when they were allowed to select their own surface conditions than when they were forced to u se 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, T he range in bare soil evaporation is unlikely to be reduced by improvi ng the simulation of soil moisture and instead an assessment of why th e bare soil evaporation formulations are inconsistent is required.