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    POSITION DETERMINATION METHODS USED TO TRACK SUPERPRESSURE BALLOONS 

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 010:;page 756
    Author(s): BLAMONT, J. E.; HEINSHEIMER, T. F.; POMMEREAU, J.-P.
    Publisher: American Meteorological Society
    Abstract: The method that has been used in the past to determine the position of superpressure balloons employed in long-term meteorological and technological experiments?projects GHOST (Global Horizontal Sounding Technique), EOLE ...
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    Noctilucent Clouds in Daytime: Circumpolar Particulate Layers Near the Summer Mesopause 

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 006:;page 1205
    Author(s): Donahue, T. M.; Guenther, B.; Blamont, J. E.
    Publisher: American Meteorological Society
    Abstract: Observations with a horizon scanning airglow photometer on OGO-6 have revealed the presence of a dense scattering layer near 80 km over the geographic pole during the local summer. The layer is detected on all satellite ...
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    An Experimental Demonstration of the Isentropic Nature of the Motion of Stratospheric Air Masses 

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 006:;page 1015
    Author(s): Blamont, J. E.; Heinsheimer, T. F.; Pommereau, J. P.; Doury, A.
    Publisher: American Meteorological Society
    Abstract: A superpressure balloon flying at a constant density level fortuitously encountered (on two consecutive days) an artificial cloud generated by a French nuclear test over the South Pacific. The measurements of temperature ...
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