lmd_Grandpeix2011.bib

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@article{2011JGRD..11624118P,
  author = {{Prigent}, C. and {Rochetin}, N. and {Aires}, F. and {Defer}, E. and 
	{Grandpeix}, J.-Y. and {Jimenez}, C. and {Papa}, F.},
  title = {{Impact of the inundation occurrence on the deep convection at continental scale from satellite observations and modeling experiments}},
  journal = {Journal of Geophysical Research (Atmospheres)},
  keywords = {convection, remote sensing, wetland, Atmospheric Processes: Atmospheric electricity, Atmospheric Processes: Convective processes},
  year = 2011,
  month = dec,
  volume = 116,
  number = d15,
  eid = {D24118},
  pages = {24118},
  abstract = {{This study is an attempt to evidence the impact of the inundation
occurrence on the deep convection at continental scale. Three sources of
satellite observations are carefully analyzed over the tropics for 3
years: A multisatellite wetland extent and dynamics data set, a deep
convective activity index derived from passive microwave satellite
measurements at 85 GHz, and precipitation estimates. Although many other
effects contribute to the variability in the convection (e.g.,
large-scale circulation and weather regimes), careful examination of the
seasonal and diurnal variations of the satellite-derived information
makes it possible to observe two distinct regimes. The first regime
corresponds to regions where the inundation is not generated by local
precipitation. There it is shown that stronger convection happens during
the minimum of the inundation, with a marked diurnal cycle of the deep
convective activity. Simulations with a single-column model are in good
agreement with these satellite observations. First, calculations show
that during the season of minimum inundation, hydrometeors are present
higher in altitude, increasing the likelihood of larger ice quantities
aloft. Second, the diurnal cycle of the convective activity related to
the presence of large ice quantities has a larger amplitude. The second
regime corresponds to regions where the inundation is directly generated
by local precipitation. There our observational analysis could not
isolate any effect of the inundation on the convection.
}},
  doi = {10.1029/2011JD016311},
  adsurl = {http://adsabs.harvard.edu/abs/2011JGRD..11624118P},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2011AtScL..12...38T,
  author = {{Taylor}, C.~M. and {Parker}, D.~J. and {Kalthoff}, N. and {Gaertner}, M.~A. and 
	{Philippon}, N. and {Bastin}, S. and {Harris}, P.~P. and {Boone}, A. and 
	{Guichard}, F. and {Agusti-Panareda}, A. and {Baldi}, M. and 
	{Cerlini}, P. and {Descroix}, L. and {Douville}, H. and {Flamant}, C. and 
	{Grandpeix}, J.-Y. and {Polcher}, J.},
  title = {{New perspectives on land-atmosphere feedbacks from the African Monsoon Multidisciplinary Analysis}},
  journal = {Atmospheric Science Letters},
  year = 2011,
  month = jan,
  volume = 12,
  pages = {38-44},
  doi = {10.1002/asl.336},
  adsurl = {http://adsabs.harvard.edu/abs/2011AtScL..12...38T},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}