Possible Impacts of Climate Change on Soil Moisture Availability in the Southeast Anatolia Development Project Region (GAP): An Analysis from an Agricultural Drought Perspective

被引:3
作者
Ali Umran Komuscu
Ayhan Erkan
Sukriye Oz
机构
[1] Turkish State Meteorological Service,Research Department
来源
Climatic Change | 1998年 / 40卷
关键词
Soil Moisture; Agricultural Drought; Soil Moisture Deficit; Soil Moisture Availability; Climate Change Analysis;
D O I
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中图分类号
学科分类号
摘要
This paper presents probable effects of climate change on soil moisture availability in the Southeast Anatolia Development Project (GAP) region of Turkey. A series of hypothetical climate change scenarios and GCM-generated IPCC Business-as-Usual scenario estimates of temperature and precipitation changes were used to examine implications of climate change for seasonal changes in actual evapotranspiration, soil moisture deficit, and soil moisture surplus in 13 subregions of the GAP. Of particular importance are predicted patterns of enhancement in summer soil moisture deficit that are consistent across the region in all scenarios. Least effect of the projected warming on the soil moisture deficit enhancement is observed with the IPCC estimates. The projected temperature changes would be responsible for a great portion of the enhancement in summer deficits in the GAP region. The increase in precipitation had less effect on depletion rate of soil moisture when the temperatures increase. Particularly southern and southeastern parts of the region will suffer severe moisture shortages during summer. Winter surplus decreased in scenarios with increased temperature and decreased precipitation in most cases. Even when precipitation was not changed, total annual surplus decreased by 4 percent to 43 percent for a 2°C warming and by 8 percent to 91 percent for a 4°C warming. These hydrologic results may have significant implications for water availability in the GAP as the present project evaluations lack climate change analysis. Adaptation strategies – such as changes in crop varieties, applying more advanced dry farming methods, improved water management, developing more efficient irrigation systems, and changes in planting – will be important in limiting adverse effects and taking advantage of beneficial changes in climate.
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页码:519 / 545
页数:26
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共 22 条
[1]  
Gleick P. H.(1986)Methods for Evaluating the Regional Hydrologic Effects of Global Climate Changes J. Hydrol. 88 97-116
[2]  
Gleick P. H.(1987)Regional Hydrologic Consequences of Increases in Atmospheric CO Clim. Change 10 137-161
[3]  
Hansen J.(1988) and other Trace Gases J. Geophys. Res. 93 9341-9364
[4]  
Fung I.(1993)Global Climate Changes as Forecast by Goddard Institute for Space Studies Three-Dimensional Model Water Res. Bull. 29 755-765
[5]  
Lacis A.(1980)Effects of Simulated Climate Change on Snowmelt Runoff Modelling in Selected Basins J. Atmos. Sci. 37 99-118
[6]  
Rind D.(1988)On the Distribution of Climate Change Resulting from an Increase in CO Effects of Changes in Stratospheric Ozone and Global Climate, Climate Change 3 251-271
[7]  
Lebedeff S.(1989)-Content of the Atmosphere Water Res. Bull. 25 1231-1241
[8]  
Ruedey R.(1981)Hydrologic Consequences of Increases in Trace Gases and CO J. Geophys. Res. 86 3135-3147
[9]  
Russel G.(1989) in the Atmosphere Scient. Amer. 9 70-79
[10]  
Katwijk V. F.(1988)Hydrologic Effects of Climate Change on Delawere River Basin Geogr. J. 154 221-233