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      A review of global terrestrial evapotranspiration: Observation, modeling, climatology, and climatic variability : GLOBAL TERRESTRIAL EVAPOTRANSPIRATION

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      Reviews of Geophysics
      American Geophysical Union (AGU)

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          Natural Evaporation from Open Water, Bare Soil and Grass

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            Increased plant growth in the northern high latitudes from 1981 to 1991

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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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                Author and article information

                Journal
                Reviews of Geophysics
                Rev. Geophys.
                American Geophysical Union (AGU)
                87551209
                June 2012
                June 2012
                : 50
                : 2
                Article
                10.1029/2011RG000373
                8a5f3068-99f8-4e1f-b450-e1dd60a18fe5
                © 2012

                http://doi.wiley.com/10.1002/tdm_license_1.1

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