lmd_Boucher2001.bib

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@article{2001ClDy...18..297B,
  author = {{Boucher}, O. and {Haywood}, J.},
  title = {{On summing the components of radiative forcing of climate change}},
  journal = {Climate Dynamics},
  year = 2001,
  volume = 18,
  pages = {297-302},
  abstract = {{Radiative forcing is a useful concept in determining the potential
influence of a particular mechanism of climate change. However, due to
the increased number of forcing agents identified over the past decade,
the total radiative forcing is difficult to assess. By assigning a range
of probability distribution functions to the individual radiative
forcings and using a Monte-Carlo approach, we estimate the total
radiative forcing since pre-industrial times including all quantitative
radiative forcing estimates to date. The resulting total radiative
forcing has a 75-97\% probability of being positive (or similarly a 3-25\%
probability of being negative), with mean radiative forcing ranging from
+0.68 to +1.34Wm$^{-2}$, and median radiative forcing ranging from
+0.94 to +1.39Wm$^{-2}$.
}},
  doi = {10.1007/s003820100185},
  adsurl = {http://adsabs.harvard.edu/abs/2001ClDy...18..297B},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}