The Cumulus And Stratocumulus CloudSat-CALIPSO Dataset (CASCCAD)
نویسندگان
چکیده
منابع مشابه
AIRS, CloudSat, and CALIPSO clouds
B. H. Kahn, M. T. Chahine, G. L. Stephens, G. G. Mace, R. T. Marchand, Z. Wang, C. D. Barnet, A. Eldering, R. E. Holz, R. E. Kuehn, and D. G. Vane Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA Department of Meteorology, University of Utah, Salt Lake City, UT, USA Joint Institut...
متن کاملCumulus penetration of stratocumulus clouds
On the importance of cumulus penetration on the microphysical and optical properties of stratocumulus clouds S. Ghosh, S. Osborne, and M. H. Smith Institute for Atmospheric Science, School of the Environment, University of Leeds, Leeds, LS2 9JT, UK The Meteorological Office, Exeter, Devon, EX1 3PB, UK Received: 10 June 2004 – Accepted: 27 June 2004 – Published: 20 August 2004 Correspondence to:...
متن کاملArctic cloud macrophysical characteristics from CloudSat and CALIPSO
a r t i c l e i n f o The lidar and radar profiling capabilities of the CloudSat and Cloud-Aerosol Lidar and Infrared Pathfinder (CALIPSO) satellites provide opportunities to improve the characterization of cloud properties. An Arctic cloud climatology based on their observations may be fundamentally different from earlier Arctic cloud climatologies based on passive satellite observations, whic...
متن کاملTerminal versus transient cumulus congestus: A CloudSat perspective
[1] While cumulus congestus as an important mode of tropical convection has been established, many of the previous studies that rely on radar observations usually capture them as snapshots. A logical question to consider is: are the statistics gathered from snapshot observations of cumulus congestus really reflective of this mode of convection that ceases its growth at these intermediate levels...
متن کاملLarge-eddy Simulations of Stratocumulus to Cumulus Transition
The vast fields of subtropical marine stratocumulus off the western coasts of continents are known for their persistent existence. In these regions, the large-scale subsidence associated with Hadley circulation provides favorable conditions for the formation of strong inversion, which separates moist and cool stratocumulustopped boundary layer (STBL) from dry and warm free atmosphere above. A q...
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ژورنال
عنوان ژورنال: Earth System Science Data
سال: 2019
ISSN: 1866-3516
DOI: 10.5194/essd-11-1745-2019