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      Climate Change Impacts on Ecosystem Services in High Mountain Areas: A Literature Review

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      Mountain Research and Development
      International Mountain Society (IMS) and United Nations University

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          Potential impacts of a warming climate on water availability in snow-dominated regions.

          All currently available climate models predict a near-surface warming trend under the influence of rising levels of greenhouse gases in the atmosphere. In addition to the direct effects on climate--for example, on the frequency of heatwaves--this increase in surface temperatures has important consequences for the hydrological cycle, particularly in regions where water supply is currently dominated by melting snow or ice. In a warmer world, less winter precipitation falls as snow and the melting of winter snow occurs earlier in spring. Even without any changes in precipitation intensity, both of these effects lead to a shift in peak river runoff to winter and early spring, away from summer and autumn when demand is highest. Where storage capacities are not sufficient, much of the winter runoff will immediately be lost to the oceans. With more than one-sixth of the Earth's population relying on glaciers and seasonal snow packs for their water supply, the consequences of these hydrological changes for future water availability--predicted with high confidence and already diagnosed in some regions--are likely to be severe.
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            Extinction debt of high-mountain plants under twenty-first-century climate change

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              The melting Himalayas: cascading effects of climate change on water, biodiversity, and livelihoods.

              The Greater Himalayas hold the largest mass of ice outside polar regions and are the source of the 10 largest rivers in Asia. Rapid reduction in the volume of Himalayan glaciers due to climate change is occurring. The cascading effects of rising temperatures and loss of ice and snow in the region are affecting, for example, water availability (amounts, seasonality), biodiversity (endemic species, predator-prey relations), ecosystem boundary shifts (tree-line movements, high-elevation ecosystem changes), and global feedbacks (monsoonal shifts, loss of soil carbon). Climate change will also have environmental and social impacts that will likely increase uncertainty in water supplies and agricultural production for human populations across Asia. A common understanding of climate change needs to be developed through regional and local-scale research so that mitigation and adaptation strategies can be identified and implemented. The challenges brought about by climate change in the Greater Himalayas can only be addressed through increased regional collaboration in scientific research and policy making. ©2009 Society for Conservation Biology.
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                Author and article information

                Journal
                Mountain Research and Development
                Mountain Research and Development
                International Mountain Society (IMS) and United Nations University
                0276-4741
                1994-7151
                May 2017
                May 2017
                : 37
                : 2
                : 179-187
                Affiliations
                [1 ]Basque Center for Climate Change, Barrio Sarriena s/n, Leioa, 48940, Spain, and Social-Ecological Systems Laboratory, Department of Ecology, Edificio de Biologíaa, Universidad Autónoma de Madrid, Madrid, 28049, Spain
                Article
                10.1659/MRD-JOURNAL-D-16-00110.1
                090415cf-9668-4361-9720-8fb86fc46210
                © 2017

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