Assessment of permafrost distribution maps in the Hindu Kush Himalayan region using rock glaciers mapped in Google Earth

被引:106
作者
Schmid, M. -O. [1 ]
Baral, P. [1 ]
Gruber, S. [2 ]
Shahi, S. [1 ]
Shrestha, T. [1 ]
Stumm, D. [1 ]
Wester, P. [1 ,3 ]
机构
[1] Int Ctr Integrated Mt Dev, ICIMOD, Kathmandu, Nepal
[2] Carleton Univ, Dept Geog & Environm Studies, Ottawa, ON K1S 5B6, Canada
[3] Wageningen Univ, Water Resources Management Grp, NL-6700 AP Wageningen, Netherlands
关键词
MOUNTAIN PERMAFROST; LOWER LIMIT; CHINA; ACCURACY; PLATEAU; IMAGERY; NEPAL;
D O I
10.5194/tc-9-2089-2015
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The extent and distribution of permafrost in the mountainous parts of the Hindu Kush Himalayan (HKH) region are largely unknown. A long tradition of permafrost research, predominantly on rather gentle relief, exists only on the Tibetan Plateau. Two permafrost maps are available digitally that cover the HKH and provide estimates of permafrost extent, i.e., the areal proportion of permafrost: the manually delineated Circum-Arctic Map of Permafrost and Ground Ice Conditions (Brown et al., 1998) and the Global Permafrost Zonation Index, based on a computer model (Gruber, 2012). This article provides a first-order assessment of these permafrost maps in the HKH region based on the mapping of rock glaciers. Rock glaciers were used as a proxy, because they are visual indicators of permafrost, can occur near the lowermost regional occurrence of permafrost in mountains, and can be delineated based on high-resolution remote sensing imagery freely available on Google Earth. For the mapping, 4000 square samples (similar to 30 km(2)) were randomly distributed over the HKH region. Every sample was investigated and rock glaciers were mapped by two independent researchers following precise mapping instructions. Samples with insufficient image quality were recorded but not mapped. We use the mapping of rock glaciers in Google Earth as first-order evidence for permafrost in mountain areas with severely limited ground truth. The minimum elevation of rock glaciers varies between 3500 and 5500ma.s.l. within the region. The Circum-Arctic Map of Permafrost and Ground Ice Conditions does not reproduce mapped conditions in the HKH region adequately, whereas the Global Permafrost Zonation Index does so with more success. Based on this study, the Permafrost Zonation Index is inferred to be a reasonable first-order prediction of permafrost in the HKH. In the central part of the region a considerable deviation exists that needs further investigations.
引用
收藏
页码:2089 / 2099
页数:11
相关论文
共 41 条
  • [1] Bajracharya SS., 2011, The status of glaciers in the Hindu Kush-Himalayan region
  • [2] Bivand Roger, MAPTOOLS TOOLS READI
  • [3] A statistical approach to modelling permafrost distribution in the European Alps or similar mountain ranges
    Boeckli, L.
    Brenning, A.
    Gruber, S.
    Noetzli, J.
    [J]. CRYOSPHERE, 2012, 6 (01) : 125 - 140
  • [4] The State and Fate of Himalayan Glaciers
    Bolch, T.
    Kulkarni, A.
    Kaab, A.
    Huggel, C.
    Paul, F.
    Cogley, J. G.
    Frey, H.
    Kargel, J. S.
    Fujita, K.
    Scheel, M.
    Bajracharya, S.
    Stoffel, M.
    [J]. SCIENCE, 2012, 336 (6079) : 310 - 314
  • [5] Planimetric and volumetric glacier changes in the Khumbu Himal, Nepal, since 1962 using Corona, Landsat TM and ASTER data
    Bolch, Tobias
    Buchroithner, Manfred
    Pieczonka, Tino
    Kunert, Andre
    [J]. JOURNAL OF GLACIOLOGY, 2008, 54 (187) : 592 - 600
  • [6] Geomorphological, hydrological and climatic significance of rock glaciers in the Andes of Central Chile (33-35°S)
    Brenning, A
    [J]. PERMAFROST AND PERIGLACIAL PROCESSES, 2005, 16 (03) : 231 - 240
  • [7] Benchmarking classifiers to optimally integrate terrain analysis and multispectral remote sensing in automatic rock glacier detection
    Brenning, Alexander
    [J]. REMOTE SENSING OF ENVIRONMENT, 2009, 113 (01) : 239 - 247
  • [8] Brown J., 1998, CIRCUMARCTIC MAP PER
  • [9] Cannone N, 2003, ARCT ANTARCT ALP RES, V35, P384, DOI 10.1657/1523-0430(2003)035[0384:VAAEIO]2.0.CO
  • [10] 2