lmd_Hourdin2010.bib

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@article{2010ClDy...34....1M,
  author = {{Marti}, O. and {Braconnot}, P. and {Dufresne}, J.-L. and {Bellier}, J. and 
	{Benshila}, R. and {Bony}, S. and {Brockmann}, P. and {Cadule}, P. and 
	{Caubel}, A. and {Codron}, F. and {de Noblet}, N. and {Denvil}, S. and 
	{Fairhead}, L. and {Fichefet}, T. and {Foujols}, M.-A. and {Friedlingstein}, P. and 
	{Goosse}, H. and {Grandpeix}, J.-Y. and {Guilyardi}, E. and 
	{Hourdin}, F. and {Idelkadi}, A. and {Kageyama}, M. and {Krinner}, G. and 
	{Lévy}, C. and {Madec}, G. and {Mignot}, J. and {Musat}, I. and 
	{Swingedouw}, D. and {Talandier}, C.},
  title = {{Key features of the IPSL ocean atmosphere model and its sensitivity to atmospheric resolution}},
  journal = {Climate Dynamics},
  keywords = {Climate, Simulations, Ocean, Atmosphere, Coupling, Circulation, El Ni{\~n}o/Southern oscillation, North-Atlantic oscillation, Storm-tracks, Resolution},
  year = 2010,
  month = jan,
  volume = 34,
  pages = {1-26},
  abstract = {{This paper presents the major characteristics of the Institut Pierre
Simon Laplace (IPSL) coupled ocean-atmosphere general circulation model.
The model components and the coupling methodology are described, as well
as the main characteristics of the climatology and interannual
variability. The model results of the standard version used for IPCC
climate projections, and for intercomparison projects like the
Paleoclimate Modeling Intercomparison Project (PMIP 2) are compared to
those with a higher resolution in the atmosphere. A focus on the North
Atlantic and on the tropics is used to address the impact of the
atmosphere resolution on processes and feedbacks. In the North Atlantic,
the resolution change leads to an improved representation of the
storm-tracks and the North Atlantic oscillation. The better
representation of the wind structure increases the northward salt
transports, the deep-water formation and the Atlantic meridional
overturning circulation. In the tropics, the ocean-atmosphere dynamical
coupling, or Bjerknes feedback, improves with the resolution. The
amplitude of ENSO (El Ni{\~n}o-Southern oscillation) consequently
increases, as the damping processes are left unchanged.
}},
  doi = {10.1007/s00382-009-0640-6},
  adsurl = {http://adsabs.harvard.edu/abs/2010ClDy...34....1M},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010BoLMe.135..469R,
  author = {{Rio}, C. and {Hourdin}, F. and {Couvreux}, F. and {Jam}, A.
	},
  title = {{Resolved Versus Parametrized Boundary-Layer Plumes. Part II: Continuous Formulations of Mixing Rates for Mass-Flux Schemes}},
  journal = {Boundary-Layer Meteorology},
  keywords = {Boundary-layer thermals, Entrainment and detrainment, Large-eddy simulations, Mass-flux parametrization},
  year = 2010,
  month = jun,
  volume = 135,
  pages = {469-483},
  abstract = {{The conditional sampling of coherent structures in large-eddy
simulations of the convective boundary layer (Couvreux et al.
Boundary-layer Meteorol 134:441-458, 2010) is used to propose and
evaluate formulations of fractional entrainment and detrainment rates
for mass-flux schemes. The proposed formulations are physically-based
and continuous from the surface to the top of clouds. Entrainment is
related to the updraft vertical velocity divergence, while detrainment
depends on the thermal vertical velocity, on buoyancy and on the
moisture contrast between the mean plume and its environment. The
proposed formulations are first directly evaluated in simulations of
shallow clouds. They are then tested in single-column simulations with
the thermal plume model, a mass-flux representation of boundary-layer
thermals.
}},
  doi = {10.1007/s10546-010-9478-z},
  adsurl = {http://adsabs.harvard.edu/abs/2010BoLMe.135..469R},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010ACP....10.3463R,
  author = {{Rio}, C. and {Hourdin}, F. and {Chédin}, A.},
  title = {{Numerical simulation of tropospheric injection of biomass burning products by pyro-thermal plumes}},
  journal = {Atmospheric Chemistry \& Physics},
  year = 2010,
  month = apr,
  volume = 10,
  pages = {3463-3478},
  abstract = {{The thermal plume model, a mass-flux scheme originally developed to
represent the vertical transport by convective structures within the
boundary layer, is adapted to the representation of plumes generated by
fires, with the aim of estimating the height at which fire emissions are
actually injected in the atmosphere. The parameterization, which takes
into account the excess of near surface temperature induced by fires and
the mixing between convective plumes and environmental air, is first
evaluated on two well-documented fires. Simulations over Southern Africa
performed with the general circulation model LMDZ over one month show
that the CO$_{2}$ can be injected far above the boundary layer
height, leading to a daily excess of CO$_{2}$ in the
mid-troposphere of an order of 2 ppmv. These results agree with
satellite retrievals of a diurnal cycle of CO$_{2}$ in the free
troposphere over regions affected by biomass burning in the Tropics.
}},
  adsurl = {http://adsabs.harvard.edu/abs/2010ACP....10.3463R},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010BoLMe.134..441C,
  author = {{Couvreux}, F. and {Hourdin}, F. and {Rio}, C.},
  title = {{Resolved Versus Parametrized Boundary-Layer Plumes. Part I: A Parametrization-Oriented Conditional Sampling in Large-Eddy Simulations}},
  journal = {Boundary-Layer Meteorology},
  keywords = {Coherent structures, Conditional sampling, Convective boundary layer, Large-eddy simulations, Mass-flux parametrization},
  year = 2010,
  month = mar,
  volume = 134,
  pages = {441-458},
  abstract = {{A conditional sampling based on the combination of a passive tracer
emitted at the surface and thermodynamic variables is proposed to
characterise organized structures in large-eddy simulations of
cloud-free and cloudy boundary layers. The sampling is evaluated against
more traditional sampling of dry thermals or clouds. It enables the
characterization of convective updrafts from the surface to the top of
the boundary layer (or the top of cumulus clouds), describing in
particular the transition from the sub-cloud to the cloud layer, and
retrieves plume characteristics, entrainment and detrainment rates,
variances and fluxes. This sampling is used to analyze the contribution
of boundary-layer thermals to vertical fluxes and variances.
}},
  doi = {10.1007/s10546-009-9456-5},
  adsurl = {http://adsabs.harvard.edu/abs/2010BoLMe.134..441C},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010BAMS...91...95H,
  author = {{Hourdin}, F. and {Musat}, I. and {Guichard}, F. and {Ruti}, P.~M. and 
	{Favot}, F. and {Filiberti*}, M.-A. and {Pham}, M. and {Grandpeix}, J.-Y. and 
	{Polcher}, J. and {Marquet}, P. and {Boone}, A. and {Lafore}, J.-P. and 
	{Redelsperger}, J.-L. and {Dell'Aquila}, A. and {Doval}, T.~L. and 
	{Traore}, A.~K. and {Gallée}, H.},
  title = {{AMMA-Model Intercomparison Project}},
  journal = {Bulletin of the American Meteorological Society},
  year = 2010,
  volume = 91,
  pages = {95},
  doi = {10.1175/2009BAMS2791.1},
  adsurl = {http://adsabs.harvard.edu/abs/2010BAMS...91...95H},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010JGRE..115.6006L,
  author = {{Lebonnois}, S. and {Hourdin}, F. and {Eymet}, V. and {Crespin}, A. and 
	{Fournier}, R. and {Forget}, F.},
  title = {{Superrotation of Venus' atmosphere analyzed with a full general circulation model}},
  journal = {Journal of Geophysical Research (Planets)},
  keywords = {Planetary Sciences: Solid Surface Planets: Meteorology (3346), Atmospheric Processes: Planetary meteorology (5445, 5739), Atmospheric Composition and Structure: Planetary atmospheres (5210, 5405, 5704), Atmospheric Processes: General circulation (1223)},
  year = 2010,
  month = jun,
  volume = 115,
  eid = {E06006},
  pages = {6006},
  abstract = {{A general circulation model (GCM) has been developed for the Venus
atmosphere, from the surface up to 100 km altitude, based on the GCM
developed for Earth at our laboratory. Key features of this new GCM
include topography, diurnal cycle, dependence of the specific heat on
temperature, and a consistent radiative transfer module based on net
exchange rate matrices. This allows a consistent computation of the
temperature field, in contrast to previous GCMs of Venus atmosphere that
used simplified temperature forcing. The circulation is analyzed after
350 Venus days (111 Earth years). Superrotation is obtained above
roughly 40 km altitude. Below, the zonal wind remains very small
compared to observed values, which is a major pending question. The
meridional circulation consists of equator-to-pole cells, the dominant
one being located within the cloud layers. The modeled temperature
structure is globally consistent with observations, though discrepancies
persist in the stability of the lowest layers and equator-pole
temperature contrast within the clouds (10 K in the model compared to
the observed 40 K). In agreement with observational data, a convective
layer is found between the base of the clouds (around 47 km) and the
middle of the clouds (55-60 km altitude). The transport of angular
momentum is analyzed, and comparison between the reference simulation
and a simulation without diurnal cycle illustrates the role played by
thermal tides in the equatorial region. Without diurnal cycle, the
Gierasch-Rossow-Williams mechanism controls angular momentum transport.
The diurnal tides add a significant downward transport of momentum in
the equatorial region, causing low latitude momentum accumulation.
}},
  doi = {10.1029/2009JE003458},
  adsurl = {http://adsabs.harvard.edu/abs/2010JGRE..115.6006L},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010MWRv..138.1767D,
  author = {{Diatta}, S. and {Hourdin}, F. and {Gaye}, A.~T. and {Viltard}, N.
	},
  title = {{Comparison of Rainfall Profiles in the West African Monsoon as Depicted by TRMM PR and the LMDZ Climate Model}},
  journal = {Monthly Weather Review},
  year = 2010,
  month = may,
  volume = 138,
  pages = {1767-1777},
  doi = {10.1175/2009MWR3092.1},
  adsurl = {http://adsabs.harvard.edu/abs/2010MWRv..138.1767D},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

@article{2010BAMS...91..611W,
  author = {{Williams}, J.~E. and {Scheele}, R. and {van Velthoven}, P. and 
	{Bouarar}, I. and {Law}, K. and {Josse}, B. and {Peuch}, V.-H. and 
	{Yang}, X. and {Pyle}, J. and {Thouret}, V. and {Barret}, B. and 
	{Liousse}, C. and {Hourdin}, F. and {Szopa}, S. and {Cozic}, A.
	},
  title = {{Global Chemistry Simulations in the AMMA Multimodel Intercomparison Project}},
  journal = {Bulletin of the American Meteorological Society},
  year = 2010,
  month = may,
  volume = 91,
  pages = {611-624},
  doi = {10.1175/2009BAMS2818.1},
  adsurl = {http://adsabs.harvard.edu/abs/2010BAMS...91..611W},
  adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}