Balmaseda MA, Mogensen K, Weaver AT. 2013. Evaluation of the ECMWF ocean reanalysis system ORAS4. Q. J. R. Meteorol. Soc. DOI:10.1002/ qj.2063
Bellucci, A., S. Gualdi, S. Masina, A. Storto and E. Scoccimarro, C. Cagnazzo, P. Fogli, E. Manzini, A. Navarra (2012), Decadal climate predictions with a coupled OAGCM initialized with oceanic reanalyses, Clim. Dyn., DOI 10.1007/s00382-012-1468-z
Cagnazzo, C., E. Manzini, P.G. Fogli, M. Vichi, P. Davini (2013) Role of stratospheric dynamics in the ozone–carbon connection in the Southern Hemisphere. Clim Dyn. doi:10.1007/s00382-013-1745-5
Corti, S., A. Weisheimer, T. Palmer, F. Doblas-Reyes, and L. Magnusson (2012), Reliability of decadal predictions, Geophys. Res. Lett., doi:10.1029/2012GL053354
Eade, R., E. Hamilton, D. M. Smith, R. J. Graham and A. A. Scaife, Forecasting the number of extreme daily events out to a decade ahead (2012), J. Geophys. Res., 117, D21110, doi:10.1029/2012JD018015
Guemas, V., Corti S., Garcìa-Serrano J., Doblas-Reyes F., Balmaseda M., Magnusson L. (2012), The Indian Ocean: the region of highest skill worldwide in decadal climate prediction, J. Clim., DOI:10.1175/JCLI-D-12-00049.1
Hardiman, Steven C., Neal Butchart, Tim J. Hinton, Scott M. Osprey, and Lesley J. Gray (2012), The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model, J. Climate, 25, 7083-7099. doi: dx.doi.org/10.1175/JCLI-D-11-00579.1
Jieshun Zhu, B. Huang, and M. A. Balmaseda (2011), An ensemble estimation of the variability of upper-ocean heat content over the tropical Atlantic Ocean with multi-ocean reanalysis products. Climate Dynamics, Published online. 10.1007/s00382-011-1189-8
Jieshun Zhu, B. Huang, L. Marx, J. L. Kinter III, M.A. Balmaseda, R.-H. Zhang,a nd Z-Z Hu (2012), Ensemble ENSO hindcasts initialized from multiple ocean analyses.GEOPHYSICAL RESEARCH LETTERS, VOL. 39, L09602, 7 PP.,doi:10.1029/2012GL051503
Karpechko, A.Y. and E. Manzini, 2012: Stratospheric influence on tropospheric climate change in the Northern Hemisphere. J. Geophys. Res., 117, D05133, doi:10.1029/ 2011JD017036
Koenigk, T., C. König Beatty, M. Caian, R. Döscher and K. Wyser (2011), Potential decadal predictability and its sensitivity to sea ice albedo parameterization in a global coupled model. Clim. Dyn., DOI 10.1007/s00382-011-1132-z
Kröger, J., W. Müller, and J.-S. von Storch (2012), Impact of Different Ocean Reanalyses on Decadal Climate Prediction, Clim. Dyn., doi: 10.1007/s00382-012-1310-7
Lecomte, O., T. Fichefet, M. Vancoppenolle, and M. Nicolaus (2011), A new snow thermodynamic scheme for large-scale sea ice models. Annals of Glaciology, 52(57), 337-346.
Magnusson, L., M. Alonso-Balmaseda, S. Corti, F. Molteni, T. Stockdale (2012), Evaluation of forecast strategies for seasonal and decadal forecasts in presence of systematic model errors. Climate Dynamics. link.springer.com/article/10.1007/s00382-012-1599-2
Magnusson, L., M. Alonso-Balmaseda and F. Molteni (2012), On the dependence of ENSO simulation on the coupled model mean state Climate Dynamics, doi: 10.1007/s00382-012-1574-y
Massonnet, F. T. Fichefet, H. Goosse, C. M. Bitz, G. Philippon-Berthier, M. M. Holland, and P.-Y. Barriat (2012), Constraining projections of summer Arctic sea ice, The Cryosphere, 6, 1383–1394, www.the-cryosphere.net/6/1383/2012/doi:10.5194/tc-6-1383-2012
Mathiot, P., C. Koenig Beatty, T. Fichefet, H. Goosse, F. Massonnet, and M. Vancoppenolle (2012), Better constraints on the sea-ice state using global sea-ice data assimilation, Geosci. Model Dev., 5, 1501–1515, www.geosci-model-dev.net/5/1501/2012/ doi:10.5194/gmd-5-1501-2012
Mitchell, D. M., S. M. Osprey, L. J. Gray, N. Butchart, S. C. Hardiman, A. J. Charlton-Perez, P. Watson (2012) The Effect of Climate Change on the Variability of the Northern Hemisphere Stratospheric Polar Vortex. J. Atmos. Sci., 69, 2608–2618. doi: http://dx.doi.org/10.1175/JAS-D-12-021.1
Osprey, Scott M., Lesley J. Gray, Steven C. Hardiman, Neal Butchart, and Tim J. Hinton (2012), Stratospheric variability in 20th Century CMIP5 simulations of the Met Office climate model: High-top versus low-top, J. Climate, accepted. doi: dx.doi.org/10.1175/JCLI-D-12-00147.1
Räisänen, P and H Järvinen (2010), Impact of cloud and radiation scheme modifications on climate simulated by the ECHAM5 atmospheric GCM. Q. J. R. Meteorol. Soc., 136, 1733-1752. doi:10.1002/qj.674
Tomassini, L., O. Geoffroy, J.-L. Dufresne, A. Idelkadi, C. Cagnazzo, K. Block, T. Mauritsen, M. Giorgetta, J. Quaas (2013), The respective roles of surface temperature driven feedbacks and tropospheric adjustment to CO2 in CMIP5 transient climate simulations, Clim Dyn DOI 10.1007/s00382-013-1682-3
Tomassini, L., E. P. Gerber, M. P. Baldwin, F. Bunzel, and M. Giorgetta (2012), The role of stratosphere-troposphere coupling in the occurrence of extreme winter cold spells over northern Europe, J. Adv. Model. Earth Syst. 4, M00A03. doi:10.1029/2012MS000177
Tjiputra, F. and O. H. Otterå (2011), Role of volcanic forcing on future global carbon cycle Earth Syst. Dynam. Discuss., 2, 133–159
Wanninkhof, R., G.-H. Park, T. Takahashi, C. Sweeney, R. Feely, Y. Nojiri, N. Gruber, S. C. Doney, G. A. McKinley, A. Lenton, C. Le Quere, C. Heinze1, J. Schwinger, H. Graven, and S. Khatiwala (2013), Global ocean carbon uptake: magnitude, variability and trends, Biogeosciences, 10, 1983–2000, 2013 www.biogeosciences.net/10/1983/2013/ doi:10.5194/bg-10-1983-2013