A Midlatitude Cirrus Cloud Climatology from the Facility for Atmospheric Remote Sensing. Part III: Radiative Properties
By Kenneth Sassen, J. Comstock. 2001
198 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/5202c00b7bd20fad7757da96fa8ce366cb5828c2
How researchers see this paper
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In Atmospheric Science
- Mark A. Vaughan
- D. Winker
- Kathleen Powell
- Ali H. Omar
- Zhaoyan Liu
- W. Hunt
- Stuart A. Young
- Yongxiang Hu
In Global and Planetary Change
- Mark A. Vaughan
- D. Winker
- Kathleen Powell
- Zhaoyan Liu
- Ali H. Omar
- W. Hunt
- Stuart A. Young
- Yongxiang Hu
Citations in the corpus
- A review of the light scattering properties of cirrus (2009, background): “Cirrus usually appears at altitudes greater than about 6 km and as satellite observations show can permanently cover 30% of the Earth’s surface, with 60–70% coverage in the tropics [2–7] and it is not confined to a particular latitude or season.”
- Arctic Mixed-Phase Cloud Properties from AERI Lidar Observations: Algorithm and Results from SHEBA (2005, background): “However, Sassen and Comstock (2001) have shown that nearly half of the cirrus at a midlatitude site have optical depths less than 0.3, and so research is continuing to determine the source of this bias.”
- Overview of the CALIPSO Mission and CALIOP Data Processing Algorithms (2009, methodology): “In version 2 processing, a constant value of 25 sr is used for ice clouds, which is the mean value measured by ground-based lidar (Sassen and Comstock 2001), and a constant value of 18 sr is used for water clouds.”