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    Ground-Based Infrared Remote Sensing of Cloud Properties over the Antarctic Plateau. Part II: Cloud Optical Depths and Particle Sizes 

    Source: Journal of Applied Meteorology:;2001:;volume( 040 ):;issue: 007:;page 1279
    Author(s): Mahesh, Ashwin; Walden, Von P.; Warren, Stephen G.
    Publisher: American Meteorological Society
    Abstract: One full year of twice-daily longwave atmospheric emission spectra measured from the surface at 1-cm?1 resolution are used to infer optical thicknesses and ice crystal sizes in tropospheric clouds over the Antarctic Plateau. ...
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    Ground-Based Infrared Remote Sensing of Cloud Properties over the Antarctic Plateau. Part I: Cloud-Base Heights 

    Source: Journal of Applied Meteorology:;2001:;volume( 040 ):;issue: 007:;page 1265
    Author(s): Mahesh, Ashwin; Walden, Von P.; Warren, Stephen G.
    Publisher: American Meteorological Society
    Abstract: A Fourier-transform interferometer, operated throughout 1992 at South Pole Station, measured downward spectral longwave radiance from 550 to 1500 cm?1 (7?18 ?m) at a resolution of 1 cm?1. Radiance measurements were usually ...
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    Radiosonde Temperature Measurements in Strong Inversions: Correction for Thermal Lag Based on an Experiment at the South Pole 

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 001:;page 45
    Author(s): Mahesh, Ashwin; Walden, Von P.; Warren, Stephen G.
    Publisher: American Meteorological Society
    Abstract: Very steep shallow temperature inversions occur during most of the year in the near-surface layer on the Antarctic Plateau. A radiosonde carried by a balloon rising at a few meters per second does not measure such inversions ...
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