Works matching IS 09307575 AND DT 2010 AND VI 35 AND IP 2/3
Results: 19
A method for climate and vegetation reconstruction through the inversion of a dynamic vegetation model.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 371, doi. 10.1007/s00382-009-0629-1
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Storm track sensitivity to sea surface temperature resolution in a regional atmosphere model.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 341, doi. 10.1007/s00382-009-0554-3
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Three centuries of Slovakian drought dynamics.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 315, doi. 10.1007/s00382-009-0563-2
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Weighting of model results for improving best estimates of climate change.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 407, doi. 10.1007/s00382-009-0659-8
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Contrasting the termination of moderate and extreme El Niño events in coupled general circulation models.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 299, doi. 10.1007/s00382-009-0562-3
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Mechanisms and reliability of future projected changes in daily precipitation.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 489, doi. 10.1007/s00382-009-0639-z
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- Article
Arctic oscillation and the interannual variability of dust emissions from the Tarim Basin: a TOMS AI based study.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 511, doi. 10.1007/s00382-009-0687-4
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Fast versus slow response in climate change: implications for the global hydrological cycle.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 423, doi. 10.1007/s00382-009-0583-y
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The Madden–Julian oscillation wind-convection coupling and the role of moisture processes in the MM5 model.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 435, doi. 10.1007/s00382-009-0626-4
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A role for icebergs in the 8.2 ka climate event.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 535, doi. 10.1007/s00382-009-0645-1
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New approach for optimal perturbation method in ensemble climate prediction with empirical singular vector.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 331, doi. 10.1007/s00382-009-0664-y
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Downscaling large-scale NCEP CFS to resolve fine-scale seasonal precipitation and extremes for the crop growing seasons over the southeastern United States.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 449, doi. 10.1007/s00382-009-0671-z
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Winter synoptic-scale variability over the Mediterranean Basin under future climate conditions as simulated by the ECHAM5.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 473, doi. 10.1007/s00382-009-0678-5
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A method for regional climate change detection using smooth temporal patterns.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 391, doi. 10.1007/s00382-009-0670-0
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A summer teleconnection pattern over the extratropical Northern Hemisphere and associated mechanisms.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 523, doi. 10.1007/s00382-009-0699-0
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Moisture transport from the Atlantic to the Pacific basin and its response to North Atlantic cooling and global warming.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 551, doi. 10.1007/s00382-009-0708-3
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Toward the snowball earth deglaciation...
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 285, doi. 10.1007/s00382-010-0748-8
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How are seasonal prediction skills related to models’ performance on mean state and annual cycle?
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 267, doi. 10.1007/s00382-010-0857-4
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- Article
Role of the upper ocean structure in the response of ENSO-like SST variability to global warming.
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- Climate Dynamics, 2010, v. 35, n. 2/3, p. 355, doi. 10.1007/s00382-010-0849-4
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- Article