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    Ray Tracing of Gravity Waves as a Possible Warning System for Tornadic Storms and Hurricanes

    Source: Journal of Applied Meteorology:;1978:;volume( 017 ):;issue: 001::page 3
    Author:
    Hung, R. J.
    ,
    Smith, R. E.
    DOI: 10.1175/1520-0450(1978)017<0003:RTOGWA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Gravity waves with wave periods of 13 to 15 min and horizontal phase velocities of 90 to 220 m s?1 were present in ground-based observations of the upper atmosphere during time periods when tornadoes were occurring and gravity waves with wave periods of 20 to 25 min and horizontal phase velocities of 100 to 200 m s?1 were detected when a hurricane was present. Combinations of available neutral atmosphere data and model parameter values were used with a group ray tracing technique in an attempt to locate the sources of these waves. Computed sources of the waves with periods of 13 to 15 min were located within 50 km of the locations where tornadoes touched down from 2 to 4 h later. In the case of the waves with periods of 20 to 25 min it was found that the computed location of the source was roughly where the hurricane would be located 3 h after the waves were excited. The applicability of the present study to a tornado and hurricane warning system is noted.
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      Ray Tracing of Gravity Waves as a Possible Warning System for Tornadic Storms and Hurricanes

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4232848
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    • Journal of Applied Meteorology

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    contributor authorHung, R. J.
    contributor authorSmith, R. E.
    date accessioned2017-06-09T17:39:15Z
    date available2017-06-09T17:39:15Z
    date copyright1978/01/01
    date issued1978
    identifier issn0021-8952
    identifier otherams-9368.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232848
    description abstractGravity waves with wave periods of 13 to 15 min and horizontal phase velocities of 90 to 220 m s?1 were present in ground-based observations of the upper atmosphere during time periods when tornadoes were occurring and gravity waves with wave periods of 20 to 25 min and horizontal phase velocities of 100 to 200 m s?1 were detected when a hurricane was present. Combinations of available neutral atmosphere data and model parameter values were used with a group ray tracing technique in an attempt to locate the sources of these waves. Computed sources of the waves with periods of 13 to 15 min were located within 50 km of the locations where tornadoes touched down from 2 to 4 h later. In the case of the waves with periods of 20 to 25 min it was found that the computed location of the source was roughly where the hurricane would be located 3 h after the waves were excited. The applicability of the present study to a tornado and hurricane warning system is noted.
    publisherAmerican Meteorological Society
    titleRay Tracing of Gravity Waves as a Possible Warning System for Tornadic Storms and Hurricanes
    typeJournal Paper
    journal volume17
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1978)017<0003:RTOGWA>2.0.CO;2
    journal fristpage3
    journal lastpage11
    treeJournal of Applied Meteorology:;1978:;volume( 017 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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