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    DESIRABILITY OF USING A FAST SAMPLING RATE FOR COMPUTING WIND VELOCITY FROM PILOT-BALLOON DATA 

    Source: Monthly Weather Review:;1967:;volume( 095 ):;issue: 004:;page 198
    Author(s): RACHELE, HENRY; DUNCAN, LOUIS D.
    Publisher: American Meteorological Society
    Abstract: Advantages of using a fast sampling rate for providing raw data for computing wind velocities from pilot-balloon observations are discussed. Two independent approaches show that (for a given sampling rate) the errors in ...
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    Real-Time Meteorological System for Firing of Unguided Rockets 

    Source: Journal of Applied Meteorology:;1967:;volume( 006 ):;issue: 002:;page 396
    Author(s): Duncan, Louis D.; Rachele, Henry
    Publisher: American Meteorological Society
    Abstract: A real-time meteorological system which has been developed by the U.S. Army Electronics Command, Atmospheric Sciences Laboratory at White Sands Missile Range, is described. The system was designed for computation and ...
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    Direct Determination of Wind Shears from the Gradients of Satellite Radiance Observations 

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 011:;page 1336
    Author(s): Ohring, George; Neeman, Binyamin; Duncan, Louis D.
    Publisher: American Meteorological Society
    Abstract: To the extent that the stratosphere wind field is close to geostrophic, the thermal wind is a good approximation to the vertical wind shear (vertical variation of the horizontal wind). And since the thermal wind is ...
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    Experimental Study of the Relationship Between Radiosonde Temperatures and Satellite-Derived Temperatures 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 004:;page 493
    Author(s): Bruce, Rufus E.; Duncan, Louis D.; Pierluissi, Joseph H.
    Publisher: American Meteorological Society
    Abstract: A large sample of temperature observations was statistically analyzed to estimate horizontal temperature variability as a function of distance. These estimates were determined at several altitudes from the surface to 15 ...
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