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Publications de l'équipe Mermaid
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Claquin T, Schulz M, Balkanski Y and Boucher O (1998), "Uncertainties in assessing radiative forcing by mineral dust", Tellus Series B Chemical and Physical Meteorology B. Vol. 50, pp. 491.

[BibTeX] [DOI] [URL]
BibTeX: 
@article{Claquin_etal_TSBCaPMB_1998a,
  author = {Claquin, T. and Schulz, M. and Balkanski, Y. and Boucher, O.},
  title = {Uncertainties in assessing radiative forcing by mineral dust},
  journal = {Tellus Series B Chemical and Physical Meteorology B},
  year = {1998},
  volume = {50},
  pages = {491},
  url = {http://adsabs.harvard.edu/abs/1998TellB..50..491C},
  doi = {10.1034/j.1600-0889.1998.t01-2-00007.x}
}
Hauglustaine DA, Balkanski Y and Schulz M (2014), "A global model simulation of present and future nitrate aerosols and their direct radiative forcing of climate", Atmospheric Chemistry & Physics. Vol. 14(20), pp. 11031-11063. Copernicus GmbH.

[BibTeX] [DOI] [URL]
BibTeX: 
@article{Hauglustaine_etal_ACP_2014a,
  author = {D. A. Hauglustaine and Y. Balkanski and M. Schulz},
  title = {A global model simulation of present and future nitrate aerosols and their direct radiative forcing of climate},
  journal = {Atmospheric Chemistry & Physics},
  publisher = {Copernicus GmbH},
  year = {2014},
  volume = {14},
  number = {20},
  pages = {11031--11063},
  url = {www.atmos-chem-phys.net/14/11031/2014/},
  doi = {10.5194/acp-14-11031-2014}
}
Lathière J, Hewitt CN and Beerling DJ (2010), "Sensitivity of isoprene emissions from the terrestrial biosphere to 20th century changes in atmospheric CO2 concentration, climate, and land use", Global Biogeochemical Cycles. Vol. 24(1)

[Abstract] [BibTeX] [DOI] [URL]
Abstract: We describe the development and analysis of a global model based on Model of Emissions of Gases and Aerosols from Nature (MEGAN) (Guenther et al., 2006) for estimating isoprene emissions from terrestrial vegetation. The sensitivity of calculated isoprene emissions to descriptors including leaf age, soil moisture, atmospheric CO2 concentration, and regional variability of emission factors is analyzed. The validity of the results is evaluated by comparison with compilations of published field-based canopy-scale observations. Calculated isoprene emissions reproduce above-canopy flux measurements and the site-to-site variability across a wide range of latitudes, with the model explaining 60% of the variance. Although the model underestimates isoprene emissions, especially in northern latitude localities, this disagreement is significantly corrected when regional variability of emission factors for particular plant functional types is considered (r2 = 0.78). At the global scale, we estimate a terrestrial biosphere isoprene flux of 413 TgC yr−1 using the present-day climate, atmospheric CO2 concentration, and vegetation distribution, and this compares with other published estimates from global modeling studies of 402 to 660 TgC yr−1. The validated model was used to calculate changes in isoprene emissions in response to atmospheric CO2 increase, climate change, and land use change during the 20th century (1901–2002). Changes in all of these factors are found to impact significantly on isoprene emissions over the course of the 20th century. Between 1901 and 2002, we estimate that at the global scale, climate change was responsible for a 7% increase in isoprene emissions, and rising atmospheric CO2 caused a 21% reduction. However, by the end of the 20th century (2002), anthropogenic cropland expansion has the largest impact reducing isoprene emissions by 15 Overall, these factors combined to cause a 24% decrease in global isoprene emissions during the 20th century. It remains to be determined whether predicted 21st century warming and increased use of isoprene-emitting crops for biofuels (e.g., oil palm) will more than offset any future CO2 suppression of isoprene emission rates.
BibTeX: 
@article{Lathiere_et_al_GBC_2010,
  author = {Lathière, J. and Hewitt, C. N. and Beerling, D. J.},
  title = {Sensitivity of isoprene emissions from the terrestrial biosphere to 20th century changes in atmospheric CO2 concentration, climate, and land use},
  journal = {Global Biogeochemical Cycles},
  year = {2010},
  volume = {24},
  number = {1},
  url = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2009GB003548},
  doi = {10.1029/2009GB003548}
}
Schulz M, Cozic A and Szopa S (2009), "LMDzT-INCA dust forecast model developments and associated validation efforts", IOP Conference Series: Earth and Environmental Science. Vol. 7, pp. 012014. IOP Publishing.

[BibTeX] [DOI]
BibTeX: 
@article{Schulz_etal_ICSEaES_2009a,
  author = {M Schulz and A Cozic and S Szopa},
  title = {LMDzT-INCA dust forecast model developments and associated validation efforts},
  journal = {IOP Conference Series: Earth and Environmental Science},
  publisher = {IOP Publishing},
  year = {2009},
  volume = {7},
  pages = {012014},
  doi = {10.1088/1755-1307/7/1/012014}
}
Szopa S, Balkanski Y, Schulz M, Bekki S, Cugnet D, Fortems-Cheiney A, Turquety S, Cozic A, Déandreis C, Hauglustaine D, Idelkadi A, Lathière J, Lefevre F, Marchand M, Vuolo R, Yan N and Dufresne J-L (2013), "Aerosol and ozone changes as forcing for climate evolution between 1850 and 2100", Climate Dynamics. Vol. 40, pp. 2223-2250.

[BibTeX] [DOI] [URL]
BibTeX: 
@article{Szopa_etal_CD_2013a,
  author = {Szopa, S. and Balkanski, Y. and Schulz, M. and Bekki, S. and Cugnet, D. and Fortems-Cheiney, A. and Turquety, S. and Cozic, A. and Déandreis, C. and Hauglustaine, D. and Idelkadi, A. and Lathière, J. and Lefevre, F. and Marchand, M. and Vuolo, R. and Yan, N. and Dufresne, J.-L.},
  title = {Aerosol and ozone changes as forcing for climate evolution between 1850 and 2100},
  journal = {Climate Dynamics},
  year = {2013},
  volume = {40},
  pages = {2223-2250},
  url = {http://adsabs.harvard.edu/abs/2013ClDy...40.2223S},
  doi = {10.1007/s00382-012-1408-y}
}
 
#95 - Màj : 11/03/2020

• Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics 

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