| Literature DB >> 28874558 |
Alexander M Milner1,2, Kieran Khamis3, Tom J Battin4, John E Brittain5, Nicholas E Barrand3, Leopold Füreder6, Sophie Cauvy-Fraunié7,8, Gísli Már Gíslason9, Dean Jacobsen10, David M Hannah3, Andrew J Hodson11, Eran Hood12, Valeria Lencioni13, Jón S Ólafsson14, Christopher T Robinson15, Martyn Tranter16, Lee E Brown17.
Abstract
Glaciers cover ∼10% of the Earth's land surface, but they are shrinking rapidly across most parts of the world, leading to cascading impacts on downstream systems. Glaciers impart unique footprints on river flow at times when other water sources are low. Changes in river hydrology and morphology caused by climate-induced glacier loss are projected to be the greatest of any hydrological system, with major implications for riverine and near-shore marine environments. Here, we synthesize current evidence of how glacier shrinkage will alter hydrological regimes, sediment transport, and biogeochemical and contaminant fluxes from rivers to oceans. This will profoundly influence the natural environment, including many facets of biodiversity, and the ecosystem services that glacier-fed rivers provide to humans, particularly provision of water for agriculture, hydropower, and consumption. We conclude that human society must plan adaptation and mitigation measures for the full breadth of impacts in all affected regions caused by glacier shrinkage.Entities:
Keywords: biodiversity; biogeochemistry; ecosystem services; glacier; runoff
Mesh:
Year: 2017 PMID: 28874558 PMCID: PMC5603989 DOI: 10.1073/pnas.1619807114
Source DB: PubMed Journal: Proc Natl Acad Sci U S A ISSN: 0027-8424 Impact factor: 11.205