By Paulo Moutinho
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Additional info for Deforestation around the world
M. (2007). Deforestation in Amazonia. Encyclopedia of Earth. Eds. J. Cleveland (General Editor) & M. Hall-Beyer (Topic Editor). A. H. Costa. (2002). The El Niño-Southern Oscillation and the climate ecosystem and river of Amazonia. G. 1132-1144. Kannan, N. , (2007). Hydrological modelling of a small catchment using SWAT-2000 – Ensuring correct flow partitioning for contaminant modeling. J. Hydrology, Vol. 3(34) pp. 64-72. W. (2005). Manual for the SLURP hydrological model. 236 p. , and P. Droogers.
E deforest –forest) for South Asia (a,d), Sri Lanka (b,e) and Southeast Asia (c,f) for 1988. Evaporation is in millimeters (mm) with a contour interval of 200 mm for annual plot and 50 mm for the seasonal plot. The Climatic Effects of Deforestation in South and Southeast Asia 17 4. Discussion Deforestation leads to warmer and drier climatic conditions. As a result of deforestation less moisture is available at the land surface, leading to a reduction in evapotranspiration. This in turn leads to an increase in temperature and a decrease in precipitation over land.
Obviously it is expected that the use of a denser network of precipitation within a basin simulation results in improvements, since the data quality is consistent, but it was not clear if the model would accept the manual modification. Fig. 2. 94 Table 3. 1%), respectively. 3). The verification of the model efficiency criteria indicates that the values are acceptable during both the calibration and validation period. (Table 3), but it is clear that the model did better with the inclusion of climatic stations.
Deforestation around the world by Paulo Moutinho