Antarctic Ice Cloud Identification and Properties Using Downwelling Spectral Radiance From 100 to 1,400 cm −1
Author:
Affiliation:
1. DIFA, Department of Physics and AstronomyUniversity of Bologna Bologna Italy
2. IUP—Institute of Environmental PhysicsUniversity of Bremen Bremen Germany
3. National Institute of OpticsINO at National Research Council Sesto Fiorentino Italy
Funder
Agenzia Spaziale Italiana
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JD029205
Reference44 articles.
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2. Spectrally resolved observations of atmospheric emitted radiance in the H2O rotation band
3. Bianchini G. Di Natale G. Del Guasta M. &Palchetti L.(2016).Two years of spectrally‐resolved measurements of the Antarctic downwelling atmospheric radiance within the COMPASS project. Fourier Transform Spectroscopy pp. FTu3C–3 Optical Society of America.
4. Bianchini G. Palchetti L. &Carli B.(2006).A wide‐band nadir‐sounding spectroradiometer for the characterization of the Earth's outgoing long‐wave radiation. Remote Sensing p. 63610A International Society for Optics and Photonics.
5. Bianchini G. Palchetti L. Guasta M. D. &Natale G. D.(2013).The PRANA experiment: Characterization of atmospheric downwelling long‐wavelength radiance over the Antarctic plateau. InEGU General Assembly Conference Abstracts EGU General Assembly Conference Abstracts(Vol.15 pp.14033).
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