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    Martian Windchill in Terrestrial Terms

    Source: Bulletin of the American Meteorological Society:;2013:;volume( 095 ):;issue: 004::page 533
    Author:
    Osczevski, Randall
    DOI: 10.1175/BAMS-D-12-00158.1
    Publisher: American Meteorological Society
    Abstract: verage temperature of ?63°C and winter lows of ?120°C, Mars sounds far too cold for humans. However, thermometer readings from Mars are highly misleading to terrestrials who base their expectations of thermal comfort on their experience in Earth's much thicker atmosphere. The two-planet model of windchill described here suggests that Martian weather is much less dangerous than it sounds because in the meager atmosphere of Mars, convection is a comparatively feeble heat transfer mechanism. The windchill on Mars is expressed as the air temperature on Earth that produces the same cooling rate in still air, in Earth's much denser atmosphere. Because Earth equivalent temperature (EET) is identical to the familiar wind chill equivalent temperature (WCET) that is broadcast across much of North America in winter, it provides a familiar context for gauging the rigors of weather on another planet. On Earth, WCET is always lower than the air temperature, but on Mars the equivalent temperature can be 100°C higher than the thermometer reading. Mars is much colder for thermometers than for people. Some frontier areas of Earth are at least as cold as midlatitude Mars is, year round. Summer afternoons in the tropics of Mars might even feel as comfortable as an average winter day in the south of England. Sunshine on Mars should be about as warm as it is on Earth. Heat balance and clothing emissivity are also briefly discussed.
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      Martian Windchill in Terrestrial Terms

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    contributor authorOsczevski, Randall
    date accessioned2017-06-09T16:44:41Z
    date available2017-06-09T16:44:41Z
    date copyright2014/04/01
    date issued2013
    identifier issn0003-0007
    identifier otherams-73332.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215435
    description abstractverage temperature of ?63°C and winter lows of ?120°C, Mars sounds far too cold for humans. However, thermometer readings from Mars are highly misleading to terrestrials who base their expectations of thermal comfort on their experience in Earth's much thicker atmosphere. The two-planet model of windchill described here suggests that Martian weather is much less dangerous than it sounds because in the meager atmosphere of Mars, convection is a comparatively feeble heat transfer mechanism. The windchill on Mars is expressed as the air temperature on Earth that produces the same cooling rate in still air, in Earth's much denser atmosphere. Because Earth equivalent temperature (EET) is identical to the familiar wind chill equivalent temperature (WCET) that is broadcast across much of North America in winter, it provides a familiar context for gauging the rigors of weather on another planet. On Earth, WCET is always lower than the air temperature, but on Mars the equivalent temperature can be 100°C higher than the thermometer reading. Mars is much colder for thermometers than for people. Some frontier areas of Earth are at least as cold as midlatitude Mars is, year round. Summer afternoons in the tropics of Mars might even feel as comfortable as an average winter day in the south of England. Sunshine on Mars should be about as warm as it is on Earth. Heat balance and clothing emissivity are also briefly discussed.
    publisherAmerican Meteorological Society
    titleMartian Windchill in Terrestrial Terms
    typeJournal Paper
    journal volume95
    journal issue4
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-D-12-00158.1
    journal fristpage533
    journal lastpage541
    treeBulletin of the American Meteorological Society:;2013:;volume( 095 ):;issue: 004
    contenttypeFulltext
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