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Nils Kadesjö1, Tufve Nyholm, Jörgen Olofsson

  • 1Department of Radiation Sciences, Radiation Physics, Umeå University, Östra Norrlandsgatan 62B, Umeå, Sweden. kadelake@gmail.com

Radiotherapy and Oncology : Journal of the European Society for Therapeutic Radiology and Oncology
|February 8, 2011
PubMed

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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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