Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-28T18:49:56.507Z Has data issue: false hasContentIssue false

Glacier change in the Karatal river basin, Zhetysu (Dzhungar) Alatau, Kazakhstan

Published online by Cambridge University Press:  03 March 2016

Azamat Kaldybayev
Affiliation:
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Ürümqi, China University of Chinese Academy of Sciences, Beijing, China
Yaning Chen*
Affiliation:
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Ürümqi, China
Evgeniy Vilesov
Affiliation:
Al-Farabi Kazakh National University, Almaty, Kazakhstan
*
Correspondence: Yaning Chen <[email protected]>
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

We investigated glacier changes in the Karatal river basin, the largest basin in Zhetysu (Dzhungar) Alatau, Kazakhstan, for the periods 1956–89, 1989–2001 and 2001–12, based on Landsat TM/ETM+ data analysis. In 1989, we found 243 glaciers with a total area of 142.8 km2; by 2012 these had shrunk to 214 glaciers with a total area of 109.3 km2, a decrease of 33.5 km2 over 23 years (1.02%a-1). This very high shrinkage rate is likely connected with a general trend of increasing temperatures, and small glaciers being situated at the relatively low altitude of the outer Zhetysu Alatau ranges. We also analyzed the shrinkage rate of glaciers based on their differences in size, altitude and aspect of slopes, as well as other topographic parameters, in four sub-basins where glacier shrinkage varied between 18% and 39%. Weather-station climate data showed a significant temperature increase and stable precipitation trends over the study period. We conclude that glacierized areas of the Karatal river basin are located in the most unfavorable conditions for glaciation, and as a result showed a higher shrinkage rate than other glacierized areas of the Tien Shan from 1956 to 2012.

Type
Paper
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s) 2016

References

Ageta, Y and Kadota, T (1992) Predictions of changes of glacier mass balance in the Nepal Himalaya and Tibetan Plateau: a case study of air temperature increase for three glaciers. Ann. Glaciol, 16, 8994 Google Scholar
Aizen, V, Aizen, E, Melack, J and Martma, T (1997) Isotopic measurements of precipitation on central Asian glaciers (Southeastern Tibet, northern Himalayas, central Tien Shan). J. Geophys. Res., 101(4), 91859198 Google Scholar
Aizen, VB, Kuzmichenok, VA, Surazakov, AB and Aizen, EM (2006) Glacier changes in the central and northern Tien Shan during the last 140 years based on surface and remote-sensing data. Ann. Glaciol., 43, 202213 Google Scholar
Aizen, VB, Kuzmichenok, VA, Surazakov, AB and Aizen, EM (2007) Glacier changes in the Tien Shan as determined from topographic and remotely sensed data. Global Planet Change, 56, 328340 Google Scholar
Albert, TH (2002) Evaluation of remote sensing techniques for ice area classification applied to the tropical Quelccaya ice cap. Peru. Polar Ceogr., 26(3), 210226 Google Scholar
Andreassen, LM, Paul, F, Kääb, A and Hausberg, JE (2008) Landsat-derived glacier inventory for Jotunheimen, Norway, and deduced glacier changes since the 1930s. Cryosphere, 2(2), 131145 CrossRefGoogle Scholar
Armstrong, RL (2010) The glaciers of the Hindu Kush-Himalayan region: a summary of the science regarding glacier melt/retreat in the Himalayan, Hindu Kush, Karakoram, Pamir and Tien Shan mountain ranges. International Centre for Integrated Mountain Development, Kathmandu Google Scholar
Bahr, DB, Pfeffer, WT, Sassolas, C and Meier, MF (1998) Response time of glaciers as a function of size and mass balance. 1. Theory. J. Geophys. Res., 103(B5), 97779782 CrossRefGoogle Scholar
Bolch, T (2007) Climate change and glacier retreat in northern Tien Shan (Kazakhstan/Kyrgyzstan) using remote sensing data. Global Planet. Change, 56, 112 Google Scholar
Bolch, T and Kamp, U (2006) Glacier mapping in high mountains using DEMs, Landsat and ASTER data. Grazer Schr. Geogr. Raumforsch., 41, 1324 Google Scholar
Bolch, T and Marchenko, SS (2009) Significance of glaciers, rock glaciers and ice rich permafrost in the Northern Tien Shan as water towers under climate change conditions. In Braun, L, Hagg, W, Severskiy, I and Young, C eds Assessment of snow, glacier and water resources in Asia, vol. 8. International Hydrological Programme-Hydrology and Water Resources Programme, Koblenz, 132144 Google Scholar
Bolch, T and 7 others (2010) A glacier inventory for the western Nyainqentanglha Range and Nam Co Basin, Tibet, and glacier changes 1976–2009. Cryosphere, 4, 419433 Google Scholar
Braithwaite, RJ and Raper, SCB (2010) Estimating equilibrium-line altitude (ELA) from glacier inventory data. Ann. Glaciol., 50, 127132 CrossRefGoogle Scholar
Chaulagai, N (2003) Impact of climate changes on water resources of Nepal: a case study of Tsho Rolpa glacial lake. (MSc thesis, University of Flensburg)Google Scholar
Cherkasov, PA (2004) Raschet sostavlyauyshih vodno-ledovogo balansa vnutrikontinenta’noi lednikovoi sistemy [Calculation of the components of water-ice balance of inland glacier system]. Google Scholar
Evans, IS (2006) Local aspect asymmetry of mountain glaciation: a global survey of consistency of favoured directions for glacier number and altitudes. Geomorphology, 73(1-2), 166184 Google Scholar
Fujita, K and Ageta, Y (2000) Effect of summer accumulation on glacier mass balance on the Tibetan Plateau revealed by mass-balance model. J. Glaciol., 46(153), 244252 Google Scholar
Cranshaw, FD and Fountain, AC (2006) Glacier change (1958–1998) in the North Cascades National Park Complex, Washington, USA. J. Glaciol., 52(177), 251256 Google Scholar
Hagg, W, Braun, LN, Kuhn, M, Nesgaard, TI (2007) Modelling of hydrological response to climate change in glacierized Central Asian catchments. J. Hydrol., 332, 4053 Google Scholar
Hagg, W, Mayer, C, Lambrecht, A, Kriegel, D and Azizov, E (2012) Glacier changes in the Big Naryn basin, Central Tian Shan. Global Planet. Change, 110, 4050 Google Scholar
Issanova, G, Jilili, A and Semenov, O (2013) Deflation processes and their role in desertification of the southern Pre-Balkhash deserts. Arab. J. Geosci., 7(11), 45134521 Google Scholar
Kaser, G, Großhauser, M and Marzeion, B (2010) Contribution potential of glaciers to water availability in different climate regimes. Proc. Natl Acad. Sci. USA (PNAS), 107, 2022320227 Google Scholar
Katalog Lednikov, SSSR [Glacier Inventory of the USSR] (1980) Centralii i luyzhnii Kazakhstan, ed. II Bassein oz. Balkhash, part 5. Bassein r. Karatala [Central and Southern Kazakhstan, ed. II Balkhash basin, part 5. Karatal river basin]. Hydrometeoizdat, Leningrad Google Scholar
Kokarev, AL and Shesterova, IN (2014) Sovremennye izmeneiya gornyh lednikov na uyzhnom sklone Dzhungarskogo Alatau [Modern change of mountain glaciers on the southern slope of the Dzhungar Alatau]. Led i Sneg, 128, 5462 Google Scholar
Kriegel, D and 6 others (2013) Changes in glacierisation, climate and runoff in the second half of the 20th century in the Naryn basin, Central Asia. Global Planet. Change, 110, 5161 Google Scholar
Kudekov, TK (2002) Sovremennoe ekologicheskoe sostoyanie basseina ozera Balkhash [Modern ecological condition of Balkhash Lake basin]. Kaganat, AlmatyGoogle Scholar
Kutuzov, S and Shahgedanova, M (2009) Glacier retreat and climatic variability in the eastern Terskey-Alatoo, inner Tien Shan between the middle of the 19th century and beginning of the 21st century. Global Planet. Change, 69, 5970 Google Scholar
Li, B, A, Zhu, Zhang, Y, Pei, T, Qin, C and Zhou, C (2007) Glacier change over the past four decades in the middle Chinese Tien Shan. J. Glaciol, 52, 425432 Google Scholar
Li, Z, Zhao, Z, Edwards, R, Wang, W and Zhou, P (2011) Characteristics of individual aerosol particles over Ürümqi Glacier No. 1 in eastern Tianshan, central Asia, China. Atmos. Res., 99, 5766 Google Scholar
Narama, C, Shimamura, Y, Nakayama, D and Abdrakhmatov, K (2006) Recent changes of glacier coverage in the western Terskey-Alatoo range, Kyrgyz Republic, using Corona and Landsat. Ann. Glaciol., 43, 223229 Google Scholar
Narama, C, Kääb, A, Duishonakunov, M and Abdrakhmatov, K (2010) Spatial variability of recent glacier area changes in the Tien Shan Mountains, Central Asia, using Corona (1970), Landsat (2000), and ALOS (2007) satellite data. Global Planet. Change, 71, 4254 Google Scholar
Niederer, P, Bilenko, V, Ershove, N, Hurni, H, Yerokhin, S and Maselli, D (2008) Tracing glacier wastage in the Northern Tien Shan (Kyrgyzstan/Central Asia) over the last 40 years. Climatic Change, 86, 227234 Google Scholar
Paul, F and Andreassen, LM (2009) A new glacier inventory for the Svartisen region, Norway, from Landsat ETM+ data: challenges and change assessment. J. Glaciol., 55(192), 607618 (doi: 10.3189/002214309789471003)Google Scholar
Paul, F and Kääb, A (2005) Perspectives on the production of a glacier inventory from multispectral satellite data in Arctic Canada: Cumberland Peninsula, Baffin Island. Ann. Glaciol., 42, 5966 Google Scholar
Paul, F, Huggel, C, Kääb, A, Kellenberger, T and Maisch, M (2003) Comparison of TM-derived glacier areas with higher resolution data sets. EARSeL eProc, 2(1), 1521 Google Scholar
Paul, F and 19 others (2013) On the accuracy of glacier outlines derived from remote-sensing data. Ann. Glaciol., 54(63 Pt 1), 171182 (doi: 10.31 89/201 3AoG63A296)Google Scholar
Pieczonka, T and Bolch, T (2015) Region-wide glacier mass budgets and area changes for the Central Tien Shan between ~1975 and 1999 using Hexagon KH-9 imagery. Global Planet. Change, 128, 113 Google Scholar
Severskiy, IV and 6 others (2012) Lednikovye sistemy Balkash-Alakolskogo basseina: sostoyanie, sovremennye, izmeneniya [Glaciological system of Balkhash-Alakol basin: state and current changes]. Probl. Geogr. Geoecol, 2, 3140 Google Scholar
Shahgedanova, M, Nosenko, G, Khromova, T and Muraveyev, A (2010) Glacier shrinkage and climatic change in the Russian Altai from the mid-20th century: an assessment using remote sensing and PRECIS regional climate model. J. Geophys. Res., 115(D16), D16107 (doi: 10.1029/2009JD012976)Google Scholar
Sorg, A, Bolch, T, Stoffel, M, Solomina, O and Beniston, M (2012) Climate change impacts on glaciers and runoff in Tien Shan (Central Asia). Nature Climate Change, 2, 725731 Google Scholar
Stocker, TF and 9 others eds (2013) Climate change 2013: the physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge and New York Google Scholar
Unger-Shayesteh, K and 6 others (2013) What do we know about past changes in the water cycle of Central Asian headwaters? A review. Global Planet. Change, 110, 425 Google Scholar
Vandenberghe, J and 7 others (2006) Penetration of Atlantic westerly winds into Central and East Asia. Quat. Sci. Rev., 25, 23802389 Google Scholar
Vilesov, EN, Morozova, VI and Severskiy, IV (2013) Oledenenle Dzhungarskogo (Zhetysu) Alatau: proshloe, nastoyashee, budushee [Claciation of Dzhungar (Zhetysu) Alatau: past, present, future]. Volkova, AlmatyGoogle Scholar
Viviroli, D, Weingartner, R and Messerli, B (2003) Assessing the hydrological significance of the world's mountains. Mt. Res. Dev., 23, 3240 Google Scholar
Wang, L, Li, Z, Wang, F and Edwards, R (2014) Glacier shrinkage in the Ebinur lake basin, Tien Shan, China, during the past 40 years. J. Glaciol., 60(220), 245254 (doi: 10.3189/2014JoC13J023)Google Scholar
Ye, B, Ding, Y and Liu, C (2001) Response of valley glaciers in various sizes and their runoff to climate change. J. Glaciol. Geocryol., 23(2), 103110 Google Scholar