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      Larger Drought and Flood Hazards and Adverse Impacts on Population and Economic Productivity Under 2.0 than 1.5°C Warming

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          Decomposition of the mean squared error and NSE performance criteria: Implications for improving hydrological modelling

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            The physical basis for increases in precipitation extremes in simulations of 21st-century climate change.

            Global warming is expected to lead to a large increase in atmospheric water vapor content and to changes in the hydrological cycle, which include an intensification of precipitation extremes. The intensity of precipitation extremes is widely held to increase proportionately to the increase in atmospheric water vapor content. Here, we show that this is not the case in 21st-century climate change scenarios simulated with climate models. In the tropics, precipitation extremes are not simulated reliably and do not change consistently among climate models; in the extratropics, they consistently increase more slowly than atmospheric water vapor content. We give a physical basis for how precipitation extremes change with climate and show that their changes depend on changes in the moist-adiabatic temperature lapse rate, in the upward velocity, and in the temperature when precipitation extremes occur. For the tropics, the theory suggests that improving the simulation of upward velocities in climate models is essential for improving predictions of precipitation extremes; for the extratropics, agreement with theory and the consistency among climate models increase confidence in the robustness of predictions of precipitation extremes under climate change.
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              Improvements in ecosystem services from investments in natural capital.

              In response to ecosystem degradation from rapid economic development, China began investing heavily in protecting and restoring natural capital starting in 2000. We report on China's first national ecosystem assessment (2000-2010), designed to quantify and help manage change in ecosystem services, including food production, carbon sequestration, soil retention, sandstorm prevention, water retention, flood mitigation, and provision of habitat for biodiversity. Overall, ecosystem services improved from 2000 to 2010, apart from habitat provision. China's national conservation policies contributed significantly to the increases in those ecosystem services.
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                Author and article information

                Contributors
                Journal
                Earth's Future
                Earth's Future
                American Geophysical Union (AGU)
                2328-4277
                2328-4277
                July 2020
                July 11 2020
                July 2020
                : 8
                : 7
                Affiliations
                [1 ]Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources ResearchChinese Academy of Sciences Beijing China
                [2 ]College of Resources and EnvironmentUniversity of Chinese Academy of Sciences Beijing China
                [3 ]Natural Resources Institute Finland (Luke) Helsinki Finland
                [4 ]Columbia Water CenterColumbia University New York New York USA
                [5 ]Department of Earth and Environmental EngineeringColumbia University New York New York USA
                [6 ]State Key Laboratory of Urban and Regional Ecology, Research Center for Eco‐Environmental SciencesChinese Academy of Sciences Beijing China
                [7 ]Department of Computer ScienceUniversity of Chicago Chicago Illinois USA
                [8 ]NASA Goddard Institute for Space Studies New York New York USA
                Article
                10.1029/2019EF001398
                8e9e0d16-8b87-475e-9b1d-7340b426e67e
                © 2020

                http://creativecommons.org/licenses/by/4.0/

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

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