Tw. Giambelluca et al., SOIL-VEGETATION-ATMOSPHERE PROCESSES - SIMULATION AND FIELD MEASUREMENT FOR DEFORESTED SITES IN NORTHERN THAILAND, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D20), 1996, pp. 25867-25885
In recent efforts to predict the climatic impacts of tropical deforest
ation an extreme scenario of impoverished grassland has been used to r
epresent the future deforested landscape. Currently, deforested areas
of the tropics are composed of a mosaic of crops, bare soil, grassland
, and secondary vegetation of various ages. The dominant feature of de
forested land is often secondary vegetation. Parameter values for impo
rtant forest replacement land covers, including secondary vegetation,
have been shown to differ from those of forest much less than that ass
umed in general circulation model (GCM) deforestation experiments. For
this study, the biosphere-atmosphere transfer scheme (BATS) is run in
uncoupled mode using measured input data in place of GCM forcing and
using the same parameter settings employed in recent deforestation exp
eriments. Model output is compared with measurements taken over seven
different deforested land surfaces in northern Thailand. Comparisons r
eveal that the simulation of deforested land overestimates reflected s
hortwave radiation, the diurnal range of surface temperature for secon
dary vegetation, surface soil moisture loss during periods without rai
n, and surface soil moisture increase at the start of a rainy period a
nd underestimates net radiation, the diurnal range of surface temperat
ure on recently used land surfaces, and root zone soil moisture increa
se at the start of a rainy period at most sites. Most deforested land
surfaces, especially intermediate and advanced secondary vegetation, a
re more similar, in terms of land surface-atmosphere interaction, to t
he model simulation of forest than of deforested land as depicted in G
CM experiments. These comparisons suggest that modelers aspiring to ma
ke realistic simulations of deforestation should adopt parameter setti
ngs representative of the diverse range of forest replacement land cov
ers, instead of again using the grassland scenario.