Explaining darker deep convective clouds over the western Pacific than over tropical continental convective regions release_652k3c2h7fdvpjqwb6yc63un5m

by B.-J. Sohn, M.-J. Choi, J. Ryu

Published in Atmospheric Measurement Techniques by Copernicus GmbH.

Issue 11 p4573-4585 (2015)


<strong>Abstract.</strong> This study attempted to explain why deep convective clouds (DCCs) over the western Pacific are generally darker than those found over tropical African and South American land regions. The western Pacific domain was further divided into its land and ocean regions to deduce the general differences in DCC characteristics between convectively active tropical land and ocean regions. DCC in this study is defined as a single-layer cloud whose thickness is greater than 15 km, and it is determined from CloudSat-measured reflectivity profiles. Corresponding MODIS-measured reflectivities at 0.645 μm were examined, along with the analysis of cloud products from Cloud Aerosol Lidar Infrared Pathfinder Satellite Observation (CALIPSO) measurements. <br><br> From an analysis of the four January months of 2007–2010, a distinct difference in ice water path (IWP) between the ocean region of the western Pacific and the three tropical land regions was revealed. Distinct differences in the effective radius between land and ocean were also found. The findings lead to a conclusion that smaller IWP over the western Pacific ocean region than over the tropical land regions, which should be caused by different cloud microphysics between land and ocean, is the main cause of smaller reflectivity there.
In application/xml+jats format

Archived Files and Locations

application/pdf  16.7 MB
web.archive.org (webarchive)
www.atmos-meas-tech.net (web)
web.archive.org (webarchive)
Read Archived PDF
Type  article-journal
Stage   published
Date   2015-11-02
Language   en ?
Container Metadata
Open Access Publication
In Keepers Registery
ISSN-L:  1867-1381
Work Entity
access all versions, variants, and formats of this works (eg, pre-prints)
Catalog Record
Revision: 560ea1c3-be06-491f-913b-e4ec99129008