Projections of glacier change in the Altai Mountains under twenty-first century climate scenarios

We project glacier surface mass balances of the Altai Mountains over the period 2006–2100 for the representative concentration pathway (RCP) 4.5 and RCP8.5 scenarios using daily near-surface air temperature and precipitation from 12 global climate models in combination with a surface mass balance mo...

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Veröffentlicht in:Climate dynamics 2016-11, Vol.47 (9-10), p.2935-2953
Hauptverfasser: Zhang, Yong, Enomoto, Hiroyuki, Ohata, Tetsuo, Kitabata, Hideyuki, Kadota, Tsutomu, Hirabayashi, Yukiko
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container_end_page 2953
container_issue 9-10
container_start_page 2935
container_title Climate dynamics
container_volume 47
creator Zhang, Yong
Enomoto, Hiroyuki
Ohata, Tetsuo
Kitabata, Hideyuki
Kadota, Tsutomu
Hirabayashi, Yukiko
description We project glacier surface mass balances of the Altai Mountains over the period 2006–2100 for the representative concentration pathway (RCP) 4.5 and RCP8.5 scenarios using daily near-surface air temperature and precipitation from 12 global climate models in combination with a surface mass balance model. The results indicate that the Altai glaciers will undergo sustained mass loss throughout the 21st for both RCPs and reveal the future fate of glaciers of different sizes. By 2100, glacier area in the region will shrink by 26 ± 10 % for RCP4.5, while it will shrink by 60 ± 15 % for RCP8.5. According to our simulations, most disappearing glaciers are located in the western part of the Altai Mountains. For RCP4.5, all glaciers disappearing in the twenty-first century have a present-day size smaller than 5.0 km 2 , while for RCP8.5, an additional ~7 % of glaciers in the initial size class of 5.0–10.0 km 2 also vanish. We project different trends in the total meltwater discharge of the region for the two RCPs, which does not peak before 2100, with important consequences for regional water availability, particular for the semi-arid and arid regions. This further highlights the potential implications of change in the Altai glaciers on regional hydrology and environment.
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The results indicate that the Altai glaciers will undergo sustained mass loss throughout the 21st for both RCPs and reveal the future fate of glaciers of different sizes. By 2100, glacier area in the region will shrink by 26 ± 10 % for RCP4.5, while it will shrink by 60 ± 15 % for RCP8.5. According to our simulations, most disappearing glaciers are located in the western part of the Altai Mountains. For RCP4.5, all glaciers disappearing in the twenty-first century have a present-day size smaller than 5.0 km 2 , while for RCP8.5, an additional ~7 % of glaciers in the initial size class of 5.0–10.0 km 2 also vanish. We project different trends in the total meltwater discharge of the region for the two RCPs, which does not peak before 2100, with important consequences for regional water availability, particular for the semi-arid and arid regions. 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This further highlights the potential implications of change in the Altai glaciers on regional hydrology and environment.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00382-016-3006-x</doi><tpages>19</tpages></addata></record>
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subjects Air temperature
Analysis
Arid zones
Climate change
Climate models
Climatology
Earth and Environmental Science
Earth Sciences
Freshwater
Geophysics/Geodesy
Glaciers
Global climate
Hydrology
Meltwater
Mountains
Oceanography
Precipitation (Meteorology)
Surface temperature
Water
Water availability
title Projections of glacier change in the Altai Mountains under twenty-first century climate scenarios
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