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Connections Between Climate and Desertification

Published online by Cambridge University Press:  24 August 2009

F. Kenneth Hare
F. Kenneth Hare
Affiliation:
University Professor and Director, Institute for Environmental Studies, University of Toronto, Toronto, Ontario, Canada; formerly President, Royal Meteorological Society and Director-General of Research Coordination, Department of the Environment, Canada; sometime Master of Birkbeck College, University of London.
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Extract

The widespread fear that the Earth's deserts are spreading was reawakened by the major 1968–73 drought in Sahelian West Africa, Sudan, Ethiopia, and parts of Kenya. There appears, however, to be no firm evidence that a permanent desiccation of the arid zone is in progress. Instead, the evidence suggests that ‘desertification’—defined as the spread of desert surfaces, regardless of cause—results more immediately from faulty land-use practices and their interaction with prolonged natural drought episodes.

Desertification appears to be a process of degradation of grassland, scrub, or savanna, ecosystems under the impact of overstocking or excessive cultivation. During periods of desiccation there is widespread destruction of perennial vegetation, compaction of soil (especially near watering places), and deflation of fine materials (wind erosion).

Such surfaces are lighter-coloured than native vegetation, and reflect more sunlight. This may enhance atmospheric subsidence, and hence intensify drought. Loss of surface organic litter may also act as a positive feedback for drought.

Prediction of such episodes is at least some years away, but three possibilities exist for such prediction: use of cyclical variations, where present; time-lagged teleconnections; and general circulation modelling.

Reduced infiltration in some arid areas, combined with excessive withdrawals in others, have lowered both shallow alluvial and deep fossil ground-water tables—in some areas to the point at which stock water-supply can no longer be maintained.

Information

Type
Main Papers
Information
Environmental Conservation , Volume 4 , Issue 2 , Summer 1977 , pp. 81 - 90
Copyright
Copyright © Foundation for Environmental Conservation 1977

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References

Anaya-Garduno, Manuel (1976). Technology and Desertification. Component review for U.N. Conference on Desertification, United Nations Environment Programme, Nairobi: without consecutive pagination (mimeogr.).Google Scholar
Bryson, Reid A. (1976). Some lessons of climatic history. Pp. 38–51 in Atmospheric Quality and Climatic Change (Ed. Kopec, Richard J.). University of North Carolina at Chapel Hill, N.C., Studies in Geography No. 9, iv + 167 pp., illustr. Published in substance earlier as ‘The lessons of climatic history’, Environmental Conservation, 2 (3), pp. 163–70, 8 figs, 1975.Google Scholar
Bryson, Reid A. & Baerreis, David (1967). Possibilities of major climatic modifications and their implications: northwest India, a case for study. Bull. Am. Met. Soc., 48, pp. 136–42.CrossRefGoogle Scholar
Budyko, Mikhail (1958). The Heat Balance of the Earth's Surface (transl. Stepanova, Nina A.). U.S. Department of Commerce, Washington: vi + 259 pp.Google Scholar
Budyko, Mikhail (1972). Climate and Life (Ed. Miller, David H.). Academic Press, London & New York: xvii + 508 pp.Google Scholar
Butzer, Karl (1971). Environment and Archaeology: An Ecological Approach to Prehistory (2nd ed.). Aldine, Chicago: 703 pp.Google Scholar
Charney, Jule (1975). Dynamics of deserts and drought in the Sahel. Quart. J. Roy. Met. Soc., 101, pp. 193–202.CrossRefGoogle Scholar
Ellsaesser, H. W., MacCracken, M. C., Potter, G. L. & Luther, F. M. (1976). An additional model test of positive feedback from high desert albedo. Quart. J. Roy. Met. Soc. 102, pp. 543–4.CrossRefGoogle Scholar
Flohn, Hermann (1971). Tropical circulation pattern. Bonner Meteorologische Abhandlungen, 15, 55 pp.Google Scholar
Geyh, M. A. & Jäkel, D. (1974). Spätpleistozäne und holozäne Klimageschicte der Sahara aufgrund zuganglicher C14-daten. Zeitschrift für Geomorphologie, 18, pp. 82–98.CrossRefGoogle Scholar
Gilchrist, A. (1975). Two climate change experiments. Met. O.20, Technical Note II/50, 14 pp. (mimeogr.).Google Scholar
Glantz, Michael H. (Ed.) (1976). Politics of Natural Disaster: The Case of the Sahel Drought. Praeger, New York: xix + 340 pp., illustr.Google Scholar
Grove, A. T. (1973). Desertification in the African environment. Pp. 33–45 in Drought in Africa, Report of the 1973 Symposium (Ed. Dalby, D. & Harrison-Church, R.). Centre for African Studies, University of London: 124 pp.Google Scholar
Hare, F. Kenneth (1942). Atlas lee-depressions and their significance for Scirocco. Air Ministry, Synoptic Divisions Technical Memoranda, London, No 43, 33 pp.Google Scholar
Hare, F. Kenneth (1943). Meteorological conditions along the Takoradi-Khartoum air-route. Air Ministry, Avidtion Meteorological Reports, London, MOM 365, 54 pp.Google Scholar
Hare, F. Kenneth (1961). The causation of the arid one. Pp. 25–30 in A History of Land Use in Arid Regions (Ed. Stamp, L. Dudley). UNESCO, Paris: 388 pp.Google Scholar
Hare, F. Kenneth (1976). Climate and Desertification (with appendices by Tzvi Gal-Chen and L. Keith Hendrie, and a chart of the Budyko-Lettau dryness ratio by Dieter Hunning). Component review for U.N. Conference on Desertification, United Nations Environment Programme, Nairobi: 189 pp., illustr. (mimeogr.).Google Scholar
Hastenrath, Stefan (1976). Variations in low-latitude circulation and extreme climatic events in the Tropical American. Journal of the Atmospheric Sciences, 33, pp. 202–15.2.0.CO;2>CrossRefGoogle Scholar
Hastenrath, Stefan & Heller, Leon (1977). Dynamics of climatic hazards in north-east Brazil. Quart. J. Roy. Met. Soc., 103, pp. 77–92.CrossRefGoogle Scholar
Henning, Dieter (1976). See Fig. 2 and Appendix I of Hare, 1976 (q.v.).Google Scholar
Kates, Robert W., Johnson, Douglas D. L. & Haring, K. Johnson (1976). Population Society and Desertification. Component review for U.N. Conference on Desertification, United Nations Environment Programme, Nairobi: 121 pp. plus four maps (mimeogr.).Google Scholar
Kovda, Viktor A. (1976). Land Aridization and Drought Control. Academy of Sciences of the U.S.S.R., Moscow: 277 pp. (typescript).Google Scholar
Landsberg, Helmut E. (1976). The definition and determination of climatic changes. Pp. 52–64 in Atmospheric Quality and Climatic Change (Ed. Kopec, Richard J.). University of North Carolina at Chapel Hill, N.C., Studies in Geography No. 9, pp. iv + 167, illustr.Google Scholar
Lovejoy, P. E. & Baier, S. (1976). The desert-side economy of the central Sudan. Pp. 145–75 in Glantz, 1976 (q.v.).Google Scholar
Markham, & McLain, [not available for checking] (1977).Google Scholar
Mason, B. John (1976). Towards the understanding and prediction of climatic variations. Quart. J. Roy. Met. Soc., 102, pp. 473–98.CrossRefGoogle Scholar
Pittock, A. B. (1975). Climatic change and the patterns of variation in Australian rainfall. Search, 6, pp. 498–504.Google Scholar
Prole, J. H. B. (1967). Pastoral land-use. Pp. 90–7 in Nairobi: City and Region (Ed. Morgan, W. T. W.). Oxford University Press, London: 154 pp.Google Scholar
Rapp, Anders (1974). A Review of Desertization in Africa— Water, Vegetation, and Man. Secretariat for International Ecology, Stockholm, SIES Report No. 1, 77 pp.Google Scholar
Rapp, Anders (1976). Regional studies and proposals for development… Sudan. Pp. 155–64 in Can Desert Encroachment be Stopped? A Study with Emphasis on Africa (Ed. Rapp, A., Le Houérou, H. N. & Lundholm, B.). (Ecological Bulletins No. 24.) Secretariat for International Ecology, Stockholm: 241 pp., illustr.Google Scholar
Rognon, P. (1976). Essai d'interprétation des variations climatiques au Sahara depuis 40,000 ans. Revue de Géographie Physique et de Geologie Dynamique, 18, pp. 251–82.Google Scholar
Schnell, R. C. (1975). Biogenic Ice Nucleus Removal by Overgrazing: A factor in the Sahelian Drought? Final report to directors, Rockefeller Foundation, National Center for Atmospheric Research, Boulder, Colorado: 12 pp. (mimeogr.).Google Scholar
Singh, Gurdip (1971). The Indus valley culture seen in the context of post-glacial and ecological studies in north-west India. Archaeology and Physical Anthropology in Oceania, 6, pp. 177–89.Google Scholar
Singh, Gurdip (1976). Stratigraphical and palynological evidence for desertification in the Great Indian Desert. Special Number of the Annals of the Arid Zone, Jodhpur, India, preprint, 16 pp.Google Scholar
Stebbing, E. P. (1935). The encroaching Sahara: the threat to the west African colonies. Geographical Journal, 85, pp. 506–24.CrossRefGoogle Scholar
Troup, A. J. (1965). The Southern Oscillations. Quart. J. Roy. Met. Soc., 91, pp. 490–506.CrossRefGoogle Scholar
Walker, Gilbert T. (1924). Correlations in seasonal variations of weather, IX. Memoirs of the Indian Meteorological Department, 24, pp. 333–45.Google Scholar
Walker, Julia & Rowntree, P. R. (1977). The effect of soil moisture on circulation and rainfall in a tropical model. Quart. J. Roy. Met. Soc., 103, pp. 29–46.CrossRefGoogle Scholar
Warren, Andrew & Maizels, J. K. (1976). Ecological Change and Desertification. Component review for the U.N. Conference on Desertification, United Nations Environment Programme, Nairobi: 198 pp. (mimeogr.).Google Scholar
Washington, Warren (1976). [Quoted by Tzvi Gal-Chen] in Hare, 1976 (q.v.).Google Scholar
Winstanley, Derek (1976). Climatic change and the future of the Sahel. Pp. 189–213 in Glantz, 1976 (q.v.).Google Scholar
Zipser, E. (1976). [Quoted by Tzvi Gal-Chen] in Hare, 1976 (q.v.).Google Scholar