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    MEASUREMENT OF WINDS AT ELEVATIONS OF 30 TO 80 KILOMETERS BY THE ROCKET-GRENADE EXPERIMENT

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 001::page 30
    Author:
    Weisner, Allan G.
    DOI: 10.1175/1520-0469(1956)013<0030:MOWAEO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Thirty-two values of wind velocity between 30 and 80 kilometers have been obtained from six Aerobee rocket flights made at night at White Sands Proving Ground, New Mexico (32°N), between July 1950 and November 1951. The average wind velocity in a horizontal layer at a particular altitude was determined from the effect of the wind on a sound wave traveling downward through the layer. The sources of the sound waves were grenades, ejected and exploded along the upward path of the rocket. The positions of the grenades, the travel times of the sound waves to a point of the ground almost directly underneath the grenades, and the angles of arrival of the waves at the ground are the data required for the calculations. The wind directions were found to be easterly in summer and westerly in autumn and winter. The wind speeds were a maximum at about 55 km, the largest measured speed having been 104 meters per second.
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      MEASUREMENT OF WINDS AT ELEVATIONS OF 30 TO 80 KILOMETERS BY THE ROCKET-GRENADE EXPERIMENT

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4149761
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    contributor authorWeisner, Allan G.
    date accessioned2017-06-09T14:11:21Z
    date available2017-06-09T14:11:21Z
    date copyright1956/02/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14223.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149761
    description abstractThirty-two values of wind velocity between 30 and 80 kilometers have been obtained from six Aerobee rocket flights made at night at White Sands Proving Ground, New Mexico (32°N), between July 1950 and November 1951. The average wind velocity in a horizontal layer at a particular altitude was determined from the effect of the wind on a sound wave traveling downward through the layer. The sources of the sound waves were grenades, ejected and exploded along the upward path of the rocket. The positions of the grenades, the travel times of the sound waves to a point of the ground almost directly underneath the grenades, and the angles of arrival of the waves at the ground are the data required for the calculations. The wind directions were found to be easterly in summer and westerly in autumn and winter. The wind speeds were a maximum at about 55 km, the largest measured speed having been 104 meters per second.
    publisherAmerican Meteorological Society
    titleMEASUREMENT OF WINDS AT ELEVATIONS OF 30 TO 80 KILOMETERS BY THE ROCKET-GRENADE EXPERIMENT
    typeJournal Paper
    journal volume13
    journal issue1
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0030:MOWAEO>2.0.CO;2
    journal fristpage30
    journal lastpage39
    treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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