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      Tree-ring hydrological research in the Himalaya: State of the art and future directions

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          Abstract

          Recent developments in tree-ring research offer great potential for reconstructing past climate changes; determining the frequencies of natural hazards; and assessing the availability of freshwater resources over timescales that extend well into the pre-instrumental period. Here, we review the state of dendrochronological research in the Himalaya and outline future directions for tree-ring-based hydrological reconstructions in a region that has a pressing societal need to understand the causes and consequences of past, present and future changes in the hydrological cycle. We used ‘tree ring’ and ‘Himalaya’ as keywords to identify scholarly articles from the Web of Science that were published between 1994 and 2022. The resulting 173 publications were separated by their spatial coverage into the western, central and eastern Himalaya, as well as their scientific purpose (e.g. reconstructing growth-climate relationships, temperature, precipitation, streamflow, floods, droughts, etc.). Our analysis shows that dendrochronological research in the Himalaya primarily focused on understanding growth-climate relationships using annual tree-ring widths measurements obtained for coniferous species, and their application in climate reconstructions. Reconstructions of hydrological processes such as streamflows, and extremes such as glacial and landslide lake outburst floods, have received less attention. Recent advances in dendrochronology, including blue intensity (BI), quantitative wood anatomy (QWA), and tree-ring stable isotopes (TRSI) should be combined to improve the resolution and accuracy of hydrological reconstructions in all parts of the Himalaya. Such studies may allow us to better understand the effects of climate change and the Himalayan water resources for its lowland surroundings. They may also facilitate decision-making processes for mitigating the impacts of climate change on natural hazards, and for better managing water resources in the region.

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          Climate change will affect the Asian water towers.

          More than 1.4 billion people depend on water from the Indus, Ganges, Brahmaputra, Yangtze, and Yellow rivers. Upstream snow and ice reserves of these basins, important in sustaining seasonal water availability, are likely to be affected substantially by climate change, but to what extent is yet unclear. Here, we show that meltwater is extremely important in the Indus basin and important for the Brahmaputra basin, but plays only a modest role for the Ganges, Yangtze, and Yellow rivers. A huge difference also exists between basins in the extent to which climate change is predicted to affect water availability and food security. The Brahmaputra and Indus basins are most susceptible to reductions of flow, threatening the food security of an estimated 60 million people.
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            Importance and vulnerability of the world’s water towers

            Mountains are the water towers of the world, supplying a substantial part of both natural and anthropogenic water demands1,2. They are highly sensitive and prone to climate change3,4, yet their importance and vulnerability have not been quantified at the global scale. Here we present a global water tower index (WTI), which ranks all water towers in terms of their water-supplying role and the downstream dependence of ecosystems and society. For each water tower, we assess its vulnerability related to water stress, governance, hydropolitical tension and future climatic and socio-economic changes. We conclude that the most important (highest WTI) water towers are also among the most vulnerable, and that climatic and socio-economic changes will affect them profoundly. This could negatively impact 1.9 billion people living in (0.3 billion) or directly downstream of (1.6 billion) mountainous areas. Immediate action is required to safeguard the future of the world's most important and vulnerable water towers.
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              The Changing Character of Precipitation

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                Author and article information

                Contributors
                (View ORCID Profile)
                Journal
                Progress in Physical Geography: Earth and Environment
                Progress in Physical Geography: Earth and Environment
                SAGE Publications
                0309-1333
                1477-0296
                February 16 2024
                Affiliations
                [1 ]Institute of Earth Surface Dynamics (IDYST), University of Lausanne, Lausanne, Switzerland
                [2 ]Department of Geography, University of Cambridge, Cambridge, UK
                [3 ]Global Change Research Institute CzechGlobe, Czech Academy of Sciences, Brno, Czech Republic
                [4 ]Department of Geography, Faculty of Science, Masaryk University, Brno, Czech Republic
                [5 ]Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
                [6 ]Faculty of Forestry, University of British Columbia, Vancouver, Canada
                Article
                10.1177/03091333241229919
                669bd83d-ceb5-49d2-8721-6df19f45ec86
                © 2024

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

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