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close this bookFreshwater Resources in Arid Lands (UNU, 1997, 94 p.)
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close this folderWelcoming address
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close this folder1: Fresh water - A scarce resource in arid lands
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View the documentFresh water - A limited resource
View the documentA personal history
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View the documentProblems of major continental aquifers
View the documentThe Aral crisis - Ecocide in arid lands
View the documentHydropolitics along the Jordan river basin and the Dead Sea
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close this folder2: Negev: land, water, and civilization in a desert environment
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close this folder3: The future of freshwater resources in the Arabian peninsula
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close this folder4: Water resources and agricultural environment in arid regions of China
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View the documentImproving water management for sustainable agricultural development
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close this folder5: The development of groundwater resources on the Miyakojima Islands
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View the documentOutline of the Miyakojima Islands
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View the documentThe construction and concept of the underground dam
View the documentThe Construction of the Cut-off Walls
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View the documentThe storage situation of the Sunagawa underground dam
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close this folder6: Global warming and groundwater resources in arid lands
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View the documentQuaternary climate history
View the documentGlobal warming and desertification
View the documentCharacteristics of groundwater in arid lands
View the documentUtilization and conservation of groundwater
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View the document7: Sustainable development of freshwater resources in arid lands: Panel discussion
close this folder8: Closing remarks
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Conclusions

1. A history of the climate indicates that the present interglacial period corresponds to a desertification period in arid lands. There is much evidence that the climate of arid lands has been very variable since the last glacial maximum. Climatic changes are different from region to region, as indicated by changes in precipitation in the Dead Sea and the Indus River basin.

2. The SST has increased markedly in the low latitude ocean during the past 60 years. The global energy and water cycle has intensified in response to the increase in SST, resulting in an increase in precipitation in some regions and a decrease in other regions. Generally speaking, the precipitation in arid lands seems to be on a decreasing trend.

3. The residence time of groundwater in arid lands is very long, which suggests a relatively small amount of natural recharge compared with the huge amount of groundwater reserve. High salinity in groundwater is a result of long residence time in the aquifer but, in arid lands, shallow groundwater with shorter residence time is also highly saline in some cases.

4. Basic scientific research is needed for the proper management of soil and water in arid lands. Recently, interesting results about the role of surface dry layer that reduces evaporation loss from the soil surface have been obtained.