Abstract
Hydrology is the science that describes the occurrence of water on earth, its areal and temporal distribution, and its quantitative and qualitative aspects. It is estimated that approximately 97% of all the water in the world -1.2 × 1018 m3—is in the oceans. The remaining 3%, or about 4 × 1016 m3, is fresh water that may be usable for irrigating lands. More than 3/4 of the fresh water cannot be developed and utilized with the current technology: 3 × 1016 m3 is frozen into polar ice caps and mountain glaciers, and more than 4 × 1015 m3 is estimated to lie in aquifers at depths exceeding 800 m below the ground surface, leaving only about 4.4 × 1015 m3 that could be used each year for the benefit of mankind. The available amount is divided between surface water (rivers, streams, freshwater lakes), groundwater (to a depth of 800 m below the ground surface), and atmospheric water (atmospheric moisture, clouds, etc.) as follows:
Surface water | 0.13 × 1015 m3 |
Groundwater | 4.27 × 1015 m3 |
Atmospheric water | 0.01 × 1015 m3 |
Total | 4.41 × 1015 m3 |
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© 1973 Springer-Verlag Berlin · Heidelberg
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Buras, N. (1973). Hydrologic Fundamentals. In: Yaron, B., Danfors, E., Vaadia, Y. (eds) Arid Zone Irrigation. Ecological Studies, vol 5. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-65570-8_3
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DOI: https://doi.org/10.1007/978-3-642-65570-8_3
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