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@ARTICLE{AR-CMGC-20-58, author = {Roberts, M.J. and Bellucci, A. and Vannière, B. and Camp, J. and Roberts, C.D. and Putrashan, D. and Mecking, J. and Hodges, K. and Terray, L. and Caron, L.P. and Vidale, P.L. and Haarsma, R. and Senan, R. and Seddon, J. and Moine, M.-P. and Kodama, C. and Yamada, Y. and Zarzycki, C. and Ullrich, P. and Mizuta, R. and Fu, D. and Danabasoglu, G. and Wu, L. and Rosenbloom, N.A. and Zhang, Q. and Scoccimarro, E. and Chauvin, F. and Valcke, S. and Wang, H. }, title = {Projected Future Changes in Tropical Cyclones using the CMIP6 HighResMIP Multi-model Ensemble}, year = {2020}, number = {14}, volume = {47}, pages = {e2020GL088662}, doi = {10.1029/2020GL088662}, journal = {Geophysical Research Letters}, pdf = {https://cerfacs.fr/wp-content/uploads/2020/05/GlobC-Article-Valcke-essoar.10503125.1.2020.pdf}}

@ARTICLE{AR-CMGC-20-60, author = {Bador, M. and Boé, J. and Terray, L. and Alexander, L.V. and Baker, A. and Bellucci, A. and Haarsma, R. and Koenigk, T. and Moine, M.-P. and Lohmann, K. and Putrasahan, D. and Roberts, C. and Roberts, M. and Scoccimarro, E. and Schiemann, R. and Seddon, J. and Senan, R. and Valcke, S. and Vannière, B. }, title = {Impact of higher spatial atmospheric resolution on precipitation extremes over land in global climate models}, year = {2020}, number = {13}, volume = {125}, pages = {e2019JD032184}, doi = {10.1029/2019JD032184}, journal = {Journal of Geophysical Research}, supplementaryMaterial = {https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019JD032184}}

@ARTICLE{AR-CMGC-20-52, author = {Boé, J. and Terray, L. and Moine, M.-P. and Valcke, S. and Bellucci, A. and Drijfhout, S. and Haarsma, R. and Lohmann, K. and Putrasahan, D. and Roberts, C.D. and Roberts, M.J. and Scoccimarro, E. and Senan, R. and Wyser, K. }, title = {Past long-term summer warming over western Europe in new generation climate models: role of large-scale atmospheric circulation}, year = {2020}, doi = {10.1088/1748-9326/ab8a89}, journal = {Environmental Research Letters}, pdf = {https://iopscience.iop.org/article/10.1088/1748-9326/ab8a89}}

@ARTICLE{AR-CFD-20-76, author = {Dupuy, F. and Gatti, M. and Mirat, C. and Gicquel, L.Y.M. and Nicoud, F. }, title = {Combining analytical models and LES data to determine the transfer function from swirled premixed flames}, year = {2020}, number = {July}, volume = {217}, pages = {222-236}, doi = {10.1016/j.combustflame.2020.03.026}, journal = {Combustion and Flame}, abstract = {A methodology is developed where the acoustic response of a swirl stabilized flame is obtained from a reduced set of simulations. Building upon previous analytical Flame Transfer Functions, a parametrization of the flame response is first proposed, based on six independent physical parameters: a Strouhal number, the mean flame angle with respect to the main flow direction, the vortical structures convection speed, a swirl intensity parameter, a time delay between acoustic and vortical perturbations, as well as a phase shift between bulk and local velocity signals. It is then shown how these parameters can be deduced from steady and unsteady simulations. The methodology is applied to a laboratory scale premixed swirl stabilized flame exhibiting features representative of real aero-engines. In this matter, cold and reactive flow Large Eddy Simulations are first validated by comparing results with reference data from experiments. The high fidelity simulations are seen to be able to capture the flame structure and velocity profiles at different locations while forced flame dynamics for the frequency range of interest also match the experimental data. From the same analytical transfer function model, three methodologies of increasing complexity are presented for the determination of the model parameters, depending on the available data or computational resources. A first estimation of the flame acoustic response is obtained by evaluating parameters from a single stationary flame simulation in conjunction with analytical estimations for the acoustic-convective time delay. Flame dynamics and swirl related parameters can then be determined from a series of robust treatments on pulsed simulations data to improve the model accuracy. It is shown that good qualitative agreement for the flame transfer function can be obtained from a single non-forced simulation while quantitative agreement over the frequency range of interest can be obtained using additional reactive or non-reactive pulsed simulations at one single forcing frequency corresponding to a local gain minimum. The method also naturally handles different perturbation levels.}, keywords = {Flame transfer Function, Swirling flame, Large Eddy Simulation, Analytical model}}

@ARTICLE{AR-CMGC-20-78, author = {Menary, M.B. and Robson, J. and Allan, R.P. and Booth, B.B.B. and Cassou, C. and Gastineau, G. and Gregory, J. and Hodson, D. and Jones, C. and Mignot, J. and Ringer, M. and Sutton, R. and Wilcox, L. and Zhang, R. }, title = {Aerosol‐Forced AMOC Changes in CMIP6 Historical Simulations}, year = {2020}, number = {14}, volume = {47}, doi = {10.1029/2020GL088166}, journal = {Geophysical Research Letters}, pdf = {https://cerfacs.fr/wp-content/uploads/2020/07/GlobC-Article-Aerosol‐Forced-AMOC-Changes-in-CMIP6-2020-GRL.pdf}}