<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Zekollari, Harry</dc:creator>
  <dc:creator>Huss, Matthias</dc:creator>
  <dc:creator>Farinotti, Daniel</dc:creator>
  <dc:date>2019-04-09</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Glaciers in the European Alps play an important role in the hydrological cycle, act as a  source for hydroelectricity and have a large touristic importance. The future evolution  of these glaciers is driven by surface mass balance and ice flow processes, of which  the latter is to date not included explicitly in regional glacier projections for the Alps.  Here, we model the future evolution of glaciers in the European Alps with  GloGEMflow, an extended version of the Global Glacier Evolution Model (GloGEM), in  which both surface mass balance and ice flow are explicitly accounted for. The mass  balance model is calibrated with glacier-specific geodetic mass balances and forced  with high-resolution regional climate model (RCM) simulations from the EURO- CORDEX ensemble. The evolution of the total glacier volume in the coming decades  is relatively similar under the various representative concentrations pathways  (RCP2.6, 4.5 and 8.5), with volume losses of about 47 %–52 % in 2050 with respect to  2017. We find that under RCP2.6, the ice loss in the second part of the 21st century is  relatively limited and that about one-third (36.8 % ± 11.1 %, multi-model mean ±1σ) of  the present-day (2017) ice volume will still be present in 2100. Under a strong  warming (RCP8.5) the future evolution of the glaciers is dictated by a substantial  increase in surface melt, and glaciers are projected to largely disappear by 2100  (94.4±4.4 % volume loss vs. 2017). For a given RCP, differences in future changes are  mainly determined by the driving global climate model (GCM), rather than by the  RCM, and these differences are larger than those arising from various model  parameters (e.g. flow parameters and cross-section parameterisation). We find that  under a limited warming, the inclusion of ice dynamics reduces the projected mass  loss and that this effect increases with the glacier elevation range, implying that the  inclusion of ice dynamics is likely to be important for global glacier evolution  projections.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307763</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307763/files/hus_mfe.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-13-1125-2019</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>The Cryosphere. - 2019, vol. 13, no. 4, p. 1125–1146</dc:source>
  <dc:subject>info:eu-repo/classification/udc/556</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Modelling the future evolution of glaciers in the European Alps under the EURO-CORDEX RCM ensemble</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
