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The Impact of Desertification as Revealed by Mapping

Published online by Cambridge University Press:  24 August 2009

John A. Mabbutt
Affiliation:
Professor of Geography, University of New South Wales, P.O. Box 1, Kensington, New South Wales 2033, Australia; Senior Consultant, United Nations, Conference on Desertification.

Extract

Maps prepared for the United Nations Conference on Desertification are critically reviewed and parts of selected maps are illustrated.

The World Map of Desertification, called for by the United Nations General Assembly, delineates areas at risk of desertification as determined by bioclimatic stress, the inherent vulnerability of the land, and pressure of land-use. Areas of very high desertification hazard are shown to be those arid and semiarid regions with very heavy pressure of land-use. The threat of desertification is shown to be highest beyond the margins of the full deserts, but the risk extends wherever drought marks the seasonal or periodic extension of aridity. The term ‘drylands’ is used to define areas in which this risk occurs.

Alternative maps at global scale include the Climate Aridity Index map based on the Budyko Ratio, which is the ratio between annual net radiation and mean annual precipitation. This allows a more sensitive depiction of aridity gradients and reveals that larger areas are under drought-stress than were previously recognized.

The map of Experimental World Scheme of Aridity and Drought Probability uses soil features as an integrative record of past and present environmental conditions, including ‘land aridity’, but is constrained by the concept of soil zonality, without sufficient consideration of topographic and inherited factors which determine soil properties.

The map of the Status of Desertification in the Hot Arid Regions shows the existing degree of desertification as judged by the difference between former (in the pristine state) and existing productivity. This is revealed as increasing outwards from the desert cores into the semi-arid lands, but the map does not extend into the sub-humid zone. However, it usefully depicts desertification as an expression of human impact on the land. Only very restricted areas are shown as having undergone very serious or irreversible desertification.

Global maps are too generalized to depict actual desertification in quantitative terms, but the continental scale of the unpublished Desertification Hazards Map of Africa North of the Equator allows this to be done, in addition to depiction of the degree of vulnerability to desertification. Areas shown as already degraded occur mainly in the arid zone, whereas those of very high vulnerability lie mainly in the semi-arid zones.

The U.N. Conference on Desertification recommended the compilation of an atlas of desertification to depict the state of the world's drylands and to serve as a cartographic basis for planning combative programmes. Regional maps of this kind, as exemplified in the synoptic maps accompanying the Case Studies of Desertification presented to the Conference, range in scale from 1:1,000,000 to 1:100,000—depending on the type of desertification portrayed—with the smaller scales for pastoral lands and more detailed scales for irrigation projects.

Type
Main Papers
Copyright
Copyright © Foundation for Environmental Conservation 1978

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References

Arnon, I. (1972). Crop Production in Dry Regions, Vol. I: Background and Principles: Vol. II: Systematic Treatment of the Principal Crops. Leonard Hill, London, England: Vol. I, pp. xxii+650, 36 plates, 99 text figs & xxx tables; Vol. II, pp. xxvi+683, 33 plates, 116 text figs & xxiv tables.Google Scholar
Budyko, M. I. (1958). The Heat Balance of the Earth's Surface (Transl. Stepanova, N. A.). U.S. Department of Commerce, Washington, D.C.: vi+259 pp.Google Scholar
Dregne, H. E. (1977). Status of Desertification in the Hot Arid Regions. United Nations Conference on Desertification, Nairobi, Kenya: A/CONF. 74/31, pp. 46, mimeogr.Google Scholar
FAO, UNESCO & WMO (1977). World Map of Desertification at a Scale of 1: 25,000,000. United Nations Conference on Desertification, Nairobi, Kenya: A/CONF. 74/2, 11 pp., mimeogr.Google Scholar
FAO/UNESCO (1971–). Soil Map of the World, 1: 5,000,000. Published jointly by FAO and UNESCO, Rome, Italy, & Paris, France.Google Scholar
Hare, F. K. (1977). Climate and desertification. Pp. 63–167 in Desertification: its Causes and Effects. (United Nations: Compiled and Edited by the Secretaiiat of the United Nations Conference on Desertification.) Pergamon, Oxford, England: v+448 pp., illustr. See also his ‘Connections Between Climate and Desertification’ (Environmental Conservation, 4 (2), pp. 8190, 5 figs, 1977).Google Scholar
Henning, D. & Flohn, H. (1977). Climate Aridity Index (Budyko Ratio). United Nations Conference on Desertification, Nairobi, Kenya: A/CONF. 74/31, pp. 79, mimeogr.Google Scholar
Kovda, V. A., Rozanov, B. G. & Onischenko, S. K. (1977). Experimental World Scheme of Aridity and Drought Probability. United Nations Conference on Desertification, Nairobi, Kenya: A/CONF. 74/31, pp. 1015, mimeogr.Google Scholar
Meigs, P. (1953). World distribution of arid and semi-arid homoclimates. Pp. 203–10 in Reviews of Research on Arid Zone Hydrology. (UNESCO, Arid Zone Programme I.) UNESCO, Paris: [not available for checking].Google Scholar
Penman, H. L. (1963). Vegetation and Hydrology. Commonwealth Bureau of Soils, Harpenden, England: Tech. Comm. 53, 124 pp.Google Scholar
Thornthwaite, C. W. (1948). An approach toward a rational classification of climate. Geog. Rev., 38, pp. 5594.CrossRefGoogle Scholar
UNESCO (1977). Map of World Distribution of Arid Regions. UNESCO, Paris, France: [not available for checking].Google Scholar
United Nations (1977a). Desertification: an overview. Pp. 161 in Desertification: its Causes and Effects. (United Nations: Compiled and Edited by the Secretariat of the United Nations Conference on Desertification.) Pergamon, Oxford, England: v+448 pp., illustr.Google Scholar
United Nations (1977b). Draft Plan of Action to Combat Desertification. United Nations Conference on Desertification, Nairobi, Kenya: A/CONF.74/31 [not available for checking].Google Scholar