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      Response of the Zonal Mean Atmospheric Circulation to El Niño versus Global Warming

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      Journal of Climate
      American Meteorological Society

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          Constraints on future changes in climate and the hydrologic cycle.

          What can we say about changes in the hydrologic cycle on 50-year timescales when we cannot predict rainfall next week? Eventually, perhaps, a great deal: the overall climate response to increasing atmospheric concentrations of greenhouse gases may prove much simpler and more predictable than the chaos of short-term weather. Quantifying the diversity of possible responses is essential for any objective, probability-based climate forecast, and this task will require a new generation of climate modelling experiments, systematically exploring the range of model behaviour that is consistent with observations. It will be substantially harder to quantify the range of possible changes in the hydrologic cycle than in global-mean temperature, both because the observations are less complete and because the physical constraints are weaker.
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            Global Warming and the Weakening of the Tropical Circulation

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              Thermal Equilibrium of the Atmosphere with a Given Distribution of Relative Humidity

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                Author and article information

                Journal
                Journal of Climate
                J. Climate
                American Meteorological Society
                0894-8755
                1520-0442
                November 2008
                November 2008
                : 21
                : 22
                : 5835-5851
                Article
                10.1175/2008JCLI2200.1
                0ecf13f6-9227-4e70-ab4c-9c06f7c02b26
                © 2008
                History

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