Climate Change Impacts on Hydrology
7.10 Projected Hydroclimatological changes
7.10.5 changes in Water resources availability
The major water uses are for irrigation, domestic, and the environmental requirements. Irrigation requires 1026.4 m3/month, while the environment flow requirements are 10% of the mean annual flow [13]. With the projected climate change, the availability of water resources availability will decrease by about 15.4%. This has adverse implications on irrigation water supply, environmental water require-ments, domestic water use, watering animals, and other uses. Table 7.3 shows the changes in water resources availability under climate change impacts.
7.11 Summary and conclusions
Global warming, due to the enhanced greenhouse effect, is likely to have significant effects on the hydro-logical cycle. The hydrohydro-logical cycle will be intensified, with more evaporation and more precipitation, but the extra precipitation will be unequally distributed around the globe. Some parts of the world may expe-rience significant reductions in precipitation, or major alterations in the timing of wet and dry seasons.
Assessing the implications of climate change on hydrology is essential for planning future water resources activities on a regional scale. This chapter analyzed the potential effects of climate change on the hydrology and water resources in general and the Nyanyadzi River catchment in eastern Zimbabwe in particular. The impacts of climate change on the hydrology of the Nyanyadzi River catchment were examined using the CSIRO climate model projections, two SRES emission scenarios (A2a and B2a), three points in time (2020, 2050, and 2080), and the 1961–1990 baseline climate data. Both scenarios predict increases in mean monthly temperature, rainfall, and evapotranspiration.
TABLE 7.3 Changes in Monthly Water Resources Availability (103 m3) for Different Uses Scenario Baseline 2020A2a 2020B2a 2050A2a 2050B2a 2080A2a 2080B2a
Runoff 3169.2 2612.8 2609.7 2669.4 2589.6 2560.9 2672.6
Environment 316.9 261.3 261.0 266.9 259.0 256.1 267.3
Irrigation 1026.4 1026.4 1026.4 1026.4 1026.4 1026.4 1026.4
Others 1852.8 1325.1 1322.3 1376.0 1304.2 1278.4 1378.9
20
15
10
5
0 2020A2a 2020B2a 2050A2a 2050B2a 2080A2a 2080B2a Scenario
Runoff (%)
FIGuRE 7.5 Percentage changes in runoff relative to the 1961–1990 baseline.
Climate Change Impacts on Hydrology and Water Resources 125
Significant reductions of runoff are expected for all time periods under the two climate change scenarios. Changes in river flows the availability of water use in the catchment. Thus, sound water man-agement strategies need to be put in place.
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127 AuTHORS
Mohammad Reza Farzaneh was born in Iran in March 1986. He is currently a PhD student of Water Resources in Tarbiat Modarres University, Tehran, Iran. His scientific experiences include being author and coauthor for two international handbooks, adviser for six master theses, more than 40 under-review and published papers in conferences and journals; collaboration in national and international proj-ects such as study of climate change impact on African water resources; teaching climate change, GIS, hydrology, and water resources; and registration of four inventions.
Saeid Eslamian received his PhD from the University of New South Wales, Australia, with Professor David Pilgrim. He was a visiting professor in Princeton University, USA, and ETH Zurich, Switzerland.
He is currently an associate professor of hydrology in Isfahan University of Technology. He is founder and chief editor of Journal of Flood Engineering and International Journal of Hydrology Science and Technology. He has published more than 200 publications mainly in statistical and environmental hydrology and hydrometeorology.
Seyed Jalal E. Mirnezami was born in July 1987 in Iran. He received his BS degree in 2009 in agricultural-water engineering from University of Tehran, Iran. Jalal studied agricultural-water resources engineering in the same university and received his MSc in 2011. During this period, he studied modeling water resources and created a model for optimizing allocation of water in river basins. Following a desire to work on