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    Strato-Mesospheric Measurements of Density, Temperature, and Other Meteorological Variables in the Central Tropical Pacific

    Source: Journal of Applied Meteorology:;1966:;volume( 005 ):;issue: 002::page 182
    Author:
    Masterson, J. E.
    ,
    Hoehne, W. E.
    ,
    Lea, D. A.
    ,
    Carr, T. R.
    DOI: 10.1175/1520-0450(1966)005<0182:SMMODT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The structure and state of the stratosphere and the mesosphere have been measured in the central tropical Pacific under a composite program of meteorological measurements. Density and temperature profiles between the altitudes of 30 and 120 km have been obtained, and wind velocities between the altitudes of 30 and 60 km have been derived from the radar track of an inflated sphere ejected from a rocket. The wind data have been supplemented by profiles from conventional meteorological rockets. Water vapor measurements by balloon-borne frost-point hygrometers have provided accurate humidity measurements in the upper troposphere and lower stratosphere.
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      Strato-Mesospheric Measurements of Density, Temperature, and Other Meteorological Variables in the Central Tropical Pacific

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4215245
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    contributor authorMasterson, J. E.
    contributor authorHoehne, W. E.
    contributor authorLea, D. A.
    contributor authorCarr, T. R.
    date accessioned2017-06-09T16:43:59Z
    date available2017-06-09T16:43:59Z
    date copyright1966/04/01
    date issued1966
    identifier issn0021-8952
    identifier otherams-7316.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215245
    description abstractThe structure and state of the stratosphere and the mesosphere have been measured in the central tropical Pacific under a composite program of meteorological measurements. Density and temperature profiles between the altitudes of 30 and 120 km have been obtained, and wind velocities between the altitudes of 30 and 60 km have been derived from the radar track of an inflated sphere ejected from a rocket. The wind data have been supplemented by profiles from conventional meteorological rockets. Water vapor measurements by balloon-borne frost-point hygrometers have provided accurate humidity measurements in the upper troposphere and lower stratosphere.
    publisherAmerican Meteorological Society
    titleStrato-Mesospheric Measurements of Density, Temperature, and Other Meteorological Variables in the Central Tropical Pacific
    typeJournal Paper
    journal volume5
    journal issue2
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1966)005<0182:SMMODT>2.0.CO;2
    journal fristpage182
    journal lastpage188
    treeJournal of Applied Meteorology:;1966:;volume( 005 ):;issue: 002
    contenttypeFulltext
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