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lmd_Hourdin2014.bib

@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:"Hourdin"  ' -c year=2014 -c $type="ARTICLE" -oc lmd_Hourdin2014.txt -ob lmd_Hourdin2014.bib /home/WWW/LMD/public/Publis_LMDEMC3.link.bib}}
@article{2014GeoRL..41.6493C,
  author = {{Cheruy}, F. and {Dufresne}, J.~L. and {Hourdin}, F. and {Ducharne}, A.
	},
  title = {{Role of clouds and land-atmosphere coupling in midlatitude continental summer warm biases and climate change amplification in CMIP5 simulations}},
  journal = {\grl},
  keywords = {model biases, land-atmosphere coupling, CMIP5, climate change},
  year = 2014,
  month = sep,
  volume = 41,
  pages = {6493-6500},
  abstract = {{Over land, most state-of-the-art climate models contributing to Coupled
Model Intercomparison Project Phase 5 (CMIP5) share a strong summertime
warm bias in midlatitude areas, especially in regions where the coupling
between soil moisture and atmosphere is effective. The most biased
models overestimate solar incoming radiation, because of cloud deficit
and have difficulty to sustain evaporation. These deficiencies are also
involved in the spread of the summer temperature projections among
models in the midlatitude; the models which simulate a
higher-than-average warming overestimate the present climate net
shortwave radiation which increases more-than-average in the future, in
link with a decrease of cloudiness. They also show a higher-than-average
reduction of evaporative fraction in areas with soil moisture-limited
evaporation regimes. Over these areas, the most biased models in the
present climate simulate a larger warming in response to climate change
which is likely to be overestimated.
}},
  doi = {10.1002/2014GL061145},
  adsurl = {http://adsabs.harvard.edu/abs/2014GeoRL..41.6493C},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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