Bagnold, R. A., 1941, The physics of blown sand and desert dunes:
Methuen, London, 265 p.
- (A classic treatise concerning the
origin and evolution of dunes.)
- Breed, C. S., and others, 1979, Regional
studies of sand seas, using Landsat (ERTS) imagery: in McKee, E. D.,
ed., A study of global sand seas: U.S. Geological Survey Professional
Paper 1052, p. 305-397.
- (A study of selected sand seas based on
analysis of remote sensing images, surface wind summaries, and
available literature.)
- Cook, R. U., and Warren, Andrew, 1973,
Geomorphology in deserts: University of California Press, Berkeley,
California, 374 p.
- (Examines the nature of landforms,
soils, and geomorphological processes in the world's deserts.)
- Eigeland, Tor, and others, 1982, The
desert realm: National Geographic Society, Washington, 304 p.
- (A well illustrated discussion of
deserts of America, Africa, Asia, and Australia.)
- Ericksen, G. E., 1983, The Chilean
nitrate deposits: American Scientist, v. 71, p. 366-374.
- (A discussion of the origin of the
Chilean nitrate deposits which has puzzled scientists for more than
100 years.)
- Gerster, Georg, 1960, Sahara-desert of
destiny: Coward-McCann, New York, 302 p.
- (How plants, animals, and people survive
in the Sahara.)
- Greeley, Ronald, and Iversen, J. D.,
1985, Wind as a geological process on Earth, Mars, Venus and Titan:
Cambridge University Press, New York, 333 p.
- (Expands the classic work of Bagnold to
discuss eolian processes in a planetary context. Describes the
processes on all moons and terrestrial planets with atmospheres.)
- Hare, F. K., 1983, Climate on the desert
fringe: in Gardner, Ritz, and Scoging, Helen, eds.,
Mega-geomorphology: Clarendon Press, Oxford, p. 134-151.
- (The margins of many deserts are
affected by tension between society and environment. This paper
summarizes the climatology of arid zones.)
- MacMahon, James A., 1985, Deserts:
Alfred A. Knopf, Inc, New York, 640 p.
- (An Audubon Society Nature Guide to the
deserts of the United States, and their inhabitants.)
- McCauley, J. F., and others, 1984,
Remote monitoring of processes that shape desert surfaces: The Desert
Winds Project: U.S. Geological Survey Bulletin 1634, 19 p.
- (Describes a new study on collecting
weather data from solar-powered data-collection platforms in deserts.
The data are relayed by a GOES satellite to the USGS in Flagstaff,
Arizona, and converted to graphic form.)
- Meigs, Peveril, 1953, World distribution
of arid and semi-arid homoclimates: in Reviews of research on arid
zone hydrology: Paris, United Nations Educational, Scientific, and
Cultural Organization, Arid Zone Programme-1, p. 203-209.
- (Classifies arid lands according to
precipitation.)
- Nelson, R., 1988, Dryland management:
the desertification problem: Environmental Department Working Paper
No. 8, Washington: World Bank, 42 p. (An excellent review of the
present state of knowledge concerning desertification.) Tolba, M. K.,
1984, Desertification is stoppable: Arid Lands Newsletter No. 21, p.
2-9.
- (A discussion of the problems involved
in preventing desertification and reclaiming arid lands.)
- Walker, A.S., 1986, Eolian
geomorphology: in Short, N.M., and Blair, R.W., eds., Geomorphology
from space: a global overview of regional landforms: NASA SP-486, p.
447-520 (a brief review of desert processes). Warren, A. and Agnew,
C., 1988, An assessment of desertification and land degradation in
arid and semi-arid areas: International Institute for Environment and
Development, Drylands Programme, Paper 2, London: IIED, 103 p.
- (An evaluation of land degradation
problems.)
The metric units used in this publication can be converted to
English units by using the approximate conversions given below:
| Length |
Area |
Temperature |
| 1 kilometer - 0.6 of a mile |
1 sq. kilometer - 0.04 sq. mile |
To convert °Celsius to °Fahrenheit,
multiply °C by 1.8 and add 32.
To convert °Fahrenheit to °Celsius, subtract 32 from °F and
divide the result by 1.8. |
| 1 meter - 39.37 inches |
1 sq. meter - 1.2 sq. yards |
|
|
| 1 centimeter - 0.4 inch |
1 sq. centimeter - 0.155 sq. inch |
|
|
| 1 millimeter - 0.04 inch |
|
|
|
|