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    An Undular Bore and Gravity Waves Illustrated by Dramatic Time-Lapse Photography

    Source: Journal of Atmospheric and Oceanic Technology:;2010:;volume( 027 ):;issue: 008::page 1355
    Author:
    Coleman, Timothy A.
    ,
    Knupp, Kevin R.
    ,
    Herzmann, Daryl E.
    DOI: 10.1175/2010JTECHA1472.1
    Publisher: American Meteorological Society
    Abstract: On 6 May 2007, an intense atmospheric undular bore moved over eastern Iowa. A ?Webcam? in Tama, Iowa, captured dramatic images of the effects of the bore and associated gravity waves on cloud features, because its viewing angle was almost normal to the propagation direction of the waves. The time lapse of these images has become a well-known illustration of atmospheric gravity waves. The environment was favorable for bore formation, with a wave-reflecting unstable layer above a low-level stable layer. Surface pressure and wind data are correlated for the waves in the bore, and horizontal wind oscillations are also shown by Doppler radar data. Quantitative analysis of the time-lapse photography shows that the sky brightens in wave troughs because of subsidence and darkens in wave ridges because of ascent.
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      An Undular Bore and Gravity Waves Illustrated by Dramatic Time-Lapse Photography

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4212976
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    contributor authorColeman, Timothy A.
    contributor authorKnupp, Kevin R.
    contributor authorHerzmann, Daryl E.
    date accessioned2017-06-09T16:37:21Z
    date available2017-06-09T16:37:21Z
    date copyright2010/08/01
    date issued2010
    identifier issn0739-0572
    identifier otherams-71119.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212976
    description abstractOn 6 May 2007, an intense atmospheric undular bore moved over eastern Iowa. A ?Webcam? in Tama, Iowa, captured dramatic images of the effects of the bore and associated gravity waves on cloud features, because its viewing angle was almost normal to the propagation direction of the waves. The time lapse of these images has become a well-known illustration of atmospheric gravity waves. The environment was favorable for bore formation, with a wave-reflecting unstable layer above a low-level stable layer. Surface pressure and wind data are correlated for the waves in the bore, and horizontal wind oscillations are also shown by Doppler radar data. Quantitative analysis of the time-lapse photography shows that the sky brightens in wave troughs because of subsidence and darkens in wave ridges because of ascent.
    publisherAmerican Meteorological Society
    titleAn Undular Bore and Gravity Waves Illustrated by Dramatic Time-Lapse Photography
    typeJournal Paper
    journal volume27
    journal issue8
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/2010JTECHA1472.1
    journal fristpage1355
    journal lastpage1361
    treeJournal of Atmospheric and Oceanic Technology:;2010:;volume( 027 ):;issue: 008
    contenttypeFulltext
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