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contributor authorWinker, David M.
contributor authorVaughan, Mark A.
contributor authorOmar, Ali
contributor authorHu, Yongxiang
contributor authorPowell, Kathleen A.
contributor authorLiu, Zhaoyan
contributor authorHunt, William H.
contributor authorYoung, Stuart A.
date accessioned2017-06-09T16:31:18Z
date available2017-06-09T16:31:18Z
date copyright2009/11/01
date issued2009
identifier issn0739-0572
identifier otherams-69337.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210995
description abstractThe Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) is a two-wavelength polarization lidar that performs global profiling of aerosols and clouds in the troposphere and lower stratosphere. CALIOP is the primary instrument on the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite, which has flown in formation with the NASA A-train constellation of satellites since May 2006. The global, multiyear dataset obtained from CALIOP provides a new view of the earth?s atmosphere and will lead to an improved understanding of the role of aerosols and clouds in the climate system. A suite of algorithms has been developed to identify aerosol and cloud layers and to retrieve a variety of optical and microphysical properties. CALIOP represents a significant advance over previous space lidars, and the algorithms that have been developed have many innovative aspects to take advantage of its capabilities. This paper provides a brief overview of the CALIPSO mission, the CALIOP instrument and data products, and an overview of the algorithms used to produce these data products.
publisherAmerican Meteorological Society
titleOverview of the CALIPSO Mission and CALIOP Data Processing Algorithms
typeJournal Paper
journal volume26
journal issue11
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/2009JTECHA1281.1
journal fristpage2310
journal lastpage2323
treeJournal of Atmospheric and Oceanic Technology:;2009:;volume( 026 ):;issue: 011
contenttypeFulltext


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