Abstract
IN many deserts the surface is heated to high temperatures by the Sun each day. In the Sonoran Desert at Yuma, Arizona, for example, the mean surface temperature exceeds 40° C for 10 h and exceeds 50° C for 4 h on an average summer day1. The highest recorded temperature is 65° C. These temperatures are not extreme; they are typical of fairly large areas of the Earth's surface today. Surface temperatures have been recorded in excess of 75° C in Death Valley, California, on a summer afternoon (W. Fuller and R. Sanchez, unpublished results). The maximum surface temperature recorded on the Earth, outside volcanoes or hot springs, is 82° C2.
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References
Dodd, A. V., and McPhilimy, H. S., Yuma Summer Microclimate, Quartermaster Research and Engineering Center, Natick, Massachusetts, Technical Report EP-120 (1959).
Quoted in Chang, Jen Hu, Ground Temperature (Blue Hill Meteorological Observatory, Harvard University, 1958).
See, for example, Duvdevani, S., in Desert Research (Research Council of Israel Special Publication No. 2, Jerusalem, 1953).
Lohrmann, R., and Orgel, L. E., Science, 171, 490 (1971).
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BISHOP, M., LOHRMANN, R. & ORGEL, L. Prebiotic Phosphorylation of Thymidine at 65° C in Simulated Desert Conditions. Nature 237, 162–164 (1972). https://doi.org/10.1038/237162a0
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DOI: https://doi.org/10.1038/237162a0
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