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@comment{{This file has been generated by bib2bib 1.95}}
@comment{{Command line: /usr/bin/bib2bib --quiet -c 'not journal:"Discussions"' -c 'not journal:"Polymer Science"' -c '  author:"Bony"  ' -c year=2000 -c $type="ARTICLE" -oc lmd_Bony2000.txt -ob lmd_Bony2000.bib /home/WWW/LMD/public/}}
  author = {{Bony}, S. and {Collins}, W.~D. and {Fillmore}, D.~W.},
  title = {{Indian Ocean Low Clouds during the Winter Monsoon.}},
  journal = {Journal of Climate},
  year = 2000,
  month = jun,
  volume = 13,
  pages = {2028-2043},
  abstract = {{While low-level clouds over the Pacific and Atlantic Oceans have been
investigated extensively, low clouds over the Indian Ocean are not as
well characterized. This study examines the occurrence of nonoverlapped
low clouds over the Indian Ocean during the northeast monsoon using
several sources of data. Climatologies derived from surface observations
and from the International Satellite Cloud Climatology Project are
reviewed. Another cloud climatology is developed using infrared and
visible imagery from the Indian geostationary satellite. The new
climatology has better spatial and temporal resolution than in situ
observations. The three datasets are generally consistent and show
several persistent features in the cloud distribution. During
January-April, maxima in the occurrence of low clouds occur at
subtropical latitudes over the Arabian Sea, the Bay of Bengal, the China
Sea, and the southern Indian Ocean. The predominant types of low clouds
differ in the northern and southern areas of the Indian Ocean region and
China Sea. The Arabian Sea and the Bay of Bengal are covered mostly by
cumulus clouds, while the southern Indian Ocean and the China Sea are
covered mostly by large-scale stratiform clouds such as stratocumulus.
These observations are consistent with atmospheric analyses of
temperature, humidity, and stability over the Indian Ocean.
  doi = {10.1175/1520-0442(2000)013<2028:IOLCDT>2.0.CO;2},
  adsurl = {},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
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