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Improving IR cloud phase determination with 20 microns spectral observations
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Improving IR cloud phase determination with 20 microns spectral observations

Author: Carsten Rathke Affiliation: Institut für Weltraumwissenschaften, Freie Universität Berlin, , Germany; Jürgen Fischer Affiliation: Institut für Weltraumwissenschaften, Freie Universität Berlin, , Germany; Steven Neshyba Affiliation: Chemistry Department, University of Puget Sound, TacomaWashington, USA; Matthew Shupe Affiliation: Science and Technology Corporation, NOAA-Environmental Technology Laboratory, BoulderColorado, USA; et al
Edition/Format: Article Article : English
Publication:Geophysical Research Letters, v29 n8 (April 2002): 50-1-50-4
Summary:
Adding 20 μm spectral observations to observations in the 8-12 μm region can significantly improve infrared cloud phase determination from both space and the surface. We demonstrate this with 7-20 μm radiance spectra of Arctic stratus clouds measured by a ship-based FTIR spectrometer during the SHEBA experiment. Our results are compared with phase classifications obtained from lidar, microwave radiometer, and radar  Read more...
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Document Type: Article
All Authors / Contributors: Carsten Rathke Affiliation: Institut für Weltraumwissenschaften, Freie Universität Berlin, , Germany; Jürgen Fischer Affiliation: Institut für Weltraumwissenschaften, Freie Universität Berlin, , Germany; Steven Neshyba Affiliation: Chemistry Department, University of Puget Sound, TacomaWashington, USA; Matthew Shupe Affiliation: Science and Technology Corporation, NOAA-Environmental Technology Laboratory, BoulderColorado, USA; et al
ISSN:0094-8276
Language Note: English
Unique Identifier: 5153963786
Notes: Number of Figures: 4
Number of Tables: 1
Awards:
Other Titles: CLOUD PHASE FROM 20 MICRONS OBSERVATIONS
Responsibility: Rathke et al.

Abstract:

Adding 20 μm spectral observations to observations in the 8-12 μm region can significantly improve infrared cloud phase determination from both space and the surface. We demonstrate this with 7-20 μm radiance spectra of Arctic stratus clouds measured by a ship-based FTIR spectrometer during the SHEBA experiment. Our results are compared with phase classifications obtained from lidar, microwave radiometer, and radar data.

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