Impact of the ongoing Amazonian deforestation on local precipitation - a GCM simulation study

@article{Jnl651496699, abstract = {Numerical simulation experiments were conducted to delineate the influence of in situ deforestation data on episodic rainfall by comparing two ensembles of five 5-day integrations performed with a recent version of the Goddard Laboratory for Atmospheres GCM that has a simple biosphere model (SiB). The first set, called control cases, used the standard SiB vegetation cover (comprising 12 biomes) and assumed a fully forested Amazonia, while the second set, called deforestation cases, distinguished the partially deforested regions of Amazonia as savanna. Except for this difference, all other initial and prescribed boundary conditions were kept identical in both sets of integrations. The differential analyses of these five cases show the following local effects of deforestation. 1) A discernible decrease in evapotranspiration of about 0.80 mm d(-1) (roughly 18\%) that is quite robust in the averages for 1-, 2-, and 5-day forecasts. 2) A decrease in precipitation of about 1.18 mm d(-1) (roughly 8\%) that begins to emerge even in 1-2-day averages and exhibits complex evolution that extends downstream with the winds. A larger decrease in precipitation as compared to evapotranspiration produces some drying and warming. The precipitation differences are consistent with the decrease in atmospheric moisture flux convergence and are consistent with earlier simulation studies of local climate change due to large-scale deforestation. 3) A significant decrease in the surface drag force (as a consequence of reduced surface roughness of deforested regions) that, in turn, affects the dynamical structure of moisture convergence and circulation. The surface winds increase significantly during the first day, and thereafter the increase is well maintained even in the 2- and 5-day averages.}, author = {Walker, G. K. and Sud, Y. C. and Atlas, R. }, citeulike-article-id = {730894}, journal = {Bulletin of the American Meteorological Society}, key = {Key651496699}, keywords = {amazon, deforestation, gcms, mdb, precipitation, sib}, number = {3}, pages = {346--361}, posted-at = {2006-07-02 15:07:00}, priority = {2}, title = {Impact of the ongoing Amazonian deforestation on local precipitation - a GCM simulation study}, volume = {76}, year = {1995} }

TY - JOUR ID - Jnl651496699 L3 - citeulike-article-id:730894 TI - Impact of the ongoing Amazonian deforestation on local precipitation - a GCM simulation study JF - Bulletin of the American Meteorological Society VL - 76 IS - 3 SP - 346 EP - 361 N2 - Numerical simulation experiments were conducted to delineate the influence of in situ deforestation data on episodic rainfall by comparing two ensembles of five 5-day integrations performed with a recent version of the Goddard Laboratory for Atmospheres GCM that has a simple biosphere model (SiB). The first set, called control cases, used the standard SiB vegetation cover (comprising 12 biomes) and assumed a fully forested Amazonia, while the second set, called deforestation cases, distinguished the partially deforested regions of Amazonia as savanna. Except for this difference, all other initial and prescribed boundary conditions were kept identical in both sets of integrations. The differential analyses of these five cases show the following local effects of deforestation. 1) A discernible decrease in evapotranspiration of about 0.80 mm d(-1) (roughly 18%) that is quite robust in the averages for 1-, 2-, and 5-day forecasts. 2) A decrease in precipitation of about 1.18 mm d(-1) (roughly 8%) that begins to emerge even in 1-2-day averages and exhibits complex evolution that extends downstream with the winds. A larger decrease in precipitation as compared to evapotranspiration produces some drying and warming. The precipitation differences are consistent with the decrease in atmospheric moisture flux convergence and are consistent with earlier simulation studies of local climate change due to large-scale deforestation. 3) A significant decrease in the surface drag force (as a consequence of reduced surface roughness of deforested regions) that, in turn, affects the dynamical structure of moisture convergence and circulation. The surface winds increase significantly during the first day, and thereafter the increase is well maintained even in the 2- and 5-day averages. KW - amazon KW - deforestation KW - gcms KW - mdb KW - precipitation KW - sib AU - Walker, GK AU - Sud, YC AU - Atlas, R PY - 1995/// ER -