HR: 1340h
AN: B33D-1587    [Abstracts]
TI: Modeling the Hydrological Impact of Land-use Change in West Africa
AU: * Coe, M T
EM: mtcoe@whrc.org
AF: The Woods Hole Research Center, 149 Woods Hole Rd, Falmouth, MA 02540, United States
AU: Li, K
EM: likaiyuan@gmail.com
AF: Center for Sustainability and the Global Environment, University of Wisconsin-Madison, 1710 University Ave, Madison, WI 53726, United States
AU: Ramankutty, N
EM: navin.ramankutty@mcgill.ca
AF: McGill Univeristy, 805 Sherbrooke Street W, Montreal, QC H3A 2K6, Canada
AU: DeJong, R
EM: dejongr@agr.gc.ca
AF: Eastern Cereal and Oilseed Research Center, 960 Carling Avenue, Ottawa, ON K1A 0C6, Canada
AB: Numerical simulations of idealized deforestation and overgrazing are performed for the Niger and Lake Chad basins of West Africa with a terrestrial ecosystem model IBIS (Integrated Biosphere Simulator) and an aquatic transport model THMB (Terrestrial Hydrology Model with Biogeochemistry). The study reveals how land use changes affect hydrological regimes at the watershed scale. Tropical forests, due to being situated in the regions of highest rainfall and exerting strong influence on evapotranspiration, have a disproportionately large impact on the water balance of the entire basin. Total deforestation of tropical forests increases the simulated runoff ratio from 0.15 to 0.44, and the annual streamflow by 35% to 65%, depending on location in the basin, although forests occupy only a small portion (<5%) of the total basin area. Complete removal of grassland and savanna, which occupy much greater areas of the basins, result in an increase in simulated annual streamflow by 33% to 91%. The hydrological response to progressive land cover change is non-linear and exhibits a threshold effect. There is no significant impact on the water yield and river discharge when the deforestation (thinning) percentage is below 50% or the overgrazing percentage below 70% for savanna and 80% for grassland areas; however, the water yield is increased dramatically when land cover change exceeds these thresholds. This threshold effect is a combined result of the non-linearity of the separate response of transpiration and soil and canopy evaporation to the imposed land cover changes.
DE: 0495 Water/energy interactions (1878)
DE: 1622 Earth system modeling (1225)
DE: 1632 Land cover change
DE: 1655 Water cycles (1836)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting