![]() | Freshwater Resources in Arid Lands (UNU, 1997, 94 p.) |
![]() | ![]() | (introduction...) |
![]() | ![]() | Preface |
![]() | ![]() | Opening address |
![]() | ![]() | (introduction...) |
![]() | ![]() | References |
![]() | ![]() | Welcoming address |
![]() | ![]() | (introduction...) |
![]() | ![]() | Reference |
![]() | ![]() | 1: Fresh water - A scarce resource in arid lands |
![]() | ![]() | (introduction...) |
![]() | ![]() | Introduction |
![]() | ![]() | International efforts |
![]() | ![]() | Fresh water - A limited resource |
![]() | ![]() | A personal history |
![]() | ![]() | Traditional wisdom |
![]() | ![]() | Problems of major continental aquifers |
![]() | ![]() | The Aral crisis - Ecocide in arid lands |
![]() | ![]() | Hydropolitics along the Jordan river basin and the Dead Sea |
![]() | ![]() | Conclusions |
![]() | ![]() | References |
![]() | ![]() | 2: Negev: land, water, and civilization in a desert environment |
![]() | ![]() | (introduction...) |
![]() | ![]() | Introduction |
![]() | ![]() | Civilization in the Negev |
![]() | ![]() | Freshwater utilization |
![]() | ![]() | Conclusions |
![]() | ![]() | Bibliography |
![]() | ![]() | 3: The future of freshwater resources in the Arabian peninsula |
![]() | ![]() | (introduction...) |
![]() | ![]() | Introduction |
![]() | ![]() | Water resources |
![]() | ![]() | Water requirements |
![]() | ![]() | Management options |
![]() | ![]() | Conclusions |
![]() | ![]() | References |
![]() | ![]() | 4: Water resources and agricultural environment in arid regions of China |
![]() | ![]() | (introduction...) |
![]() | ![]() | Introduction |
![]() | ![]() | Water resources |
![]() | ![]() | Water utilization and agricultural environment |
![]() | ![]() | Improving water management for sustainable agricultural development |
![]() | ![]() | Conclusions |
![]() | ![]() | References |
![]() | ![]() | 5: The development of groundwater resources on the Miyakojima Islands |
![]() | ![]() | (introduction...) |
![]() | ![]() | Introduction |
![]() | ![]() | Outline of the Miyakojima Islands |
![]() | ![]() | Geology and the hydrological cycle |
![]() | ![]() | Outline of the irrigation project on Miyakojima |
![]() | ![]() | The construction and concept of the underground dam |
![]() | ![]() | The Construction of the Cut-off Walls |
![]() | ![]() | The construction of the intake facilities |
![]() | ![]() | The storage situation of the Sunagawa underground dam |
![]() | ![]() | Conclusion |
![]() | ![]() | Bibliography |
![]() | ![]() | 6: Global warming and groundwater resources in arid lands |
![]() | ![]() | (introduction...) |
![]() | ![]() | Quaternary climate history |
![]() | ![]() | Global warming and desertification |
![]() | ![]() | Characteristics of groundwater in arid lands |
![]() | ![]() | Utilization and conservation of groundwater |
![]() | ![]() | Conclusions |
![]() | ![]() | References |
![]() | ![]() | 7: Sustainable development of freshwater resources in arid lands: Panel discussion |
![]() | ![]() | 8: Closing remarks |
![]() | ![]() | (introduction...) |
![]() | ![]() | References |
![]() | ![]() | Contributors |
![]() | ![]() | Other titles of interest |
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.