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2Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
limiting the...
GJ Marseille, A Stoffelen | Year: 2012
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The impact of varying ice sheets and greenhouse gases on the intensity and timing of boreal summer monsoons
Climate models, forced only with insolation, indicate that boreal summer monsoons respond to orbi...
SL Weber, E Tuenter | Status: published | Journal: Quatern. Science Rev. | Volume: 30 | Year: 2011 | First page: 469 | Last page: 479 | doi: 10.1016/j.quascirev.2010.12.009
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Atmospheric properties and the ENSO cycle: models versus observations
Two important atmospheric features affecting the ENSO cycle are weather noise and a nonlinear atm...
SY Philip, GJ van Oldenborgh | Status: published | Journal: Clim. Dyn. | Year: 2009 | doi: 10.1007/s00382-009-0579-7
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Stratospheric age of air computed with trajectories based on various 3-D-Var and 4-D-Var data sets
Stratospheric age of air computed with trajectories based on various 3D-Var and 4D-Var data sets...
MP Scheele, PC Siegmund, PFJ van Velthoven | Status: published | Journal: Atm. Chem. Phys. | Volume: 5 | Year: 2005 | First page: 1 | Last page: 7 | doi: 1680-7324/acp/2005-5-1
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Precipitation change: models and paleoreconstructions
Zonal-scale patterns of precipitation change, as reconstructed for the Mid-Pliocene and the two P...
MV Shabalova, GP Können, II Borzenkova | Status: published | Journal: Climatic Change | Volume: 42/4 | Year: 1999 | First page: 693 | Last page: 712
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