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

被引:24
作者
Zhang, Yong [1 ]
Enomoto, Hiroyuki [1 ,2 ]
Ohata, Tetsuo [1 ]
Kitabata, Hideyuki [3 ]
Kadota, Tsutomu [3 ]
Hirabayashi, Yukiko [4 ]
机构
[1] Natl Inst Polar Res, Arct Environm Res Ctr, Tokyo 1908518, Japan
[2] Grad Univ Adv Studies, Tokyo 1908518, Japan
[3] Japan Agcy Marin Earth Sci & Technol, Yokohama, Kanagawa 2370061, Japan
[4] Univ Tokyo, Inst Engn Innovat, Tokyo 1138656, Japan
关键词
Glacier mass balance; Climate change; GCM; Water availability; Altai glaciers; MASS-BALANCE; ICE CAPS; PRECIPITATION; TEMPERATURE; SENSITIVITY; MODEL; INVENTORY; BASINS; RUNOFF; TRENDS;
D O I
10.1007/s00382-016-3006-x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
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 +/- A 10 % for RCP4.5, while it will shrink by 60 +/- A 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 similar to 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.
引用
收藏
页码:2935 / 2953
页数:19
相关论文
共 68 条
  • [1] Arendt AA., 2014, Randolph Glacier Inventory - A Dataset of Global Glacier Outlines: Version 4.0. Global Land Ice measurements from Space
  • [2] A review of volume-area scaling of glaciers
    Bahr, David B.
    Pfeffer, W. Tad
    Kaser, Georg
    [J]. REVIEWS OF GEOPHYSICS, 2015, 53 (01) : 95 - 140
  • [3] Width and length scaling of glaciers
    Bahr, DB
    [J]. JOURNAL OF GLACIOLOGY, 1997, 43 (145) : 557 - 562
  • [4] The physical basis of glacier volume-area scaling
    Bahr, DB
    Meier, MF
    Peckham, SD
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1997, 102 (B9) : 20355 - 20362
  • [5] Response time of glaciers as a function of size and mass balance: 1. Theory
    Bahr, DB
    Pfeffer, WT
    Sassolas, C
    Meier, MF
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1998, 103 (B5) : 9777 - 9782
  • [6] Global response of glacier runoff to twenty-first century climate change
    Bliss, Andrew
    Hock, Regine
    Radic, Valentina
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2014, 119 (04) : 717 - 730
  • [7] Sensitivity of mass balance of five Swiss glaciers to temperature changes assessed by tuning a degree-day model
    Braithwaite, RJ
    Zhang, Y
    [J]. JOURNAL OF GLACIOLOGY, 2000, 46 (152) : 7 - 14
  • [8] Braithwaite RJ., 2003, ZEITSCHAIFT FU R GLE, V38, P35
  • [9] Detection of changes in glacial run-off in alpine basins: examples from North America, the Alps, central Asia and the Andes
    Casassa, Gino
    Lopez, Paulina
    Pouyaud, Bernard
    Escobar, Fernando
    [J]. HYDROLOGICAL PROCESSES, 2009, 23 (01) : 31 - 41
  • [10] Clarke GKC, 2015, NAT GEOSCI, V8, P372, DOI [10.1038/ngeo2407, 10.1038/NGEO2407]