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Glaciers of the Levaya Sygykta River watershed, Kodar Ridge, southeastern Siberia, Russia: modern morphology, climate conditions and changes over the past decades

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Abstract

Kodar Ridge (57°N, 118°E), southeastern Siberia, is a glaciarized mountain area of inner Asia. Here we have studied areal changes of glaciers and mid-summer snow cover in the Levaya Sygykta River watershed (area ~650 km2, 60 % of total ice cover). We used 1:50,000–1:100,000 topographic maps, Landsat TM (1995), ETM + (2001–2002), high-resolution Cartosat-1 (2009) and WorldView-2 (2013) imagery, two digital elevation models (DEMs) and field survey data to quantify the areal changes of the glaciers since the end of the Little Ice Age (LIA) to 2013. In 2013, the exposed area of 18 small glaciers (from 0.02 to 0.88 km2) in the study area was 3.917 ± 0.064 km2, and volume ~255 × 106 m3. Between the LIA maximum and 2013, the area has been decreased by 61 % with rate of 0.377 % a−1. The data available today suggest the areal shrinkage of Kodar glaciers from the LIA seems to be larger than elsewhere in Siberia. The rate of area decrease in 1995–2001 was five times greater than in 1850–2013, and in 1850–1995, 1.7 times less than in 1850–2013. Using regional climatic data we have found that climate conditions obviously stimulated glacier mass loss over the past at least 60 years. The increased variability of absolute and relative changes in 1995–2013 was due to influence of local factors on the overall climate-driven deglaciation trend. Comparison of two DEMs has showed that between 1970 and 2009, ice surfaces of 12 tested glacier tongues have been lowered, on average, by 29 ± 15 m with a rate of 0.75 m a−1.

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References

  • Adamenko MM, Gutak YM, Solomina ON (2015) Glacial history of the Kuznetsky Alatau mountains (this issue)

  • Arendt A, Echelmeyer K, Harrison W, Lingle C, Valentine V (2002) Rapid wastage of Alaska glaciers and their contribution to rising sea level. Science 297:382–386. doi:10.1126/science.1072497

    Article  Google Scholar 

  • ASTER GDEM Validation Team (2009) ASTER global DEM validation summary report. METI&NASA

  • Beedle M, Menounos B, Wheate R (2015) Glacier change in the Cariboo Mountains, British Columbia, Canada (1952–2005). Cryosphere 9:65–80. doi:10.5194/tc-9-65-2015

    Article  Google Scholar 

  • Bolch T, Buchroithner M, Pieczonka T, Kunert A (2008) Planimetric and volumetric glacier changes in the Khumbu Himal, Nepal, since 1962 using Corona, Landsat TM and ASTER data. J Glaciol 54(187):592–600

    Article  Google Scholar 

  • Chen J, Ohmura A (1990). Estimation of Alpine glacier water resources and their change since the 1870s. In Hydrology in Mountainous Regions, Lausanne, IAHS Publ. No.193:127–135

  • Cía J, Andrés A, Sánchez M, Novau J, Moreno J (2005) Responses to climatic changes since the little ice age on Maladeta Glacier (Central Pyrenees). Geomorphology 68(3–4):167–182. doi:10.1016/j.geomorph.2004.11.012

    Article  Google Scholar 

  • DeBeer C, Sharp M (2009) Topographic influences on recent changes of very small glaciers in the Monashee Mountains, British Columbia, Canada. J Glaciol 55(192):691–700

    Article  Google Scholar 

  • Ganiushkin D, Chistyakov K, Kunaeva E (2015) Fluctuation of glaciers in the South-East Russian Altai and North-West Mongolia Mountains since the Little Ice Age maximum (this issue)

  • Glazyrin GE (1985) Distribution and regime of mountain glaciers. Gidrometeoizdat, Leningrad

    Google Scholar 

  • Granshaw F, Fountain A (2006) Glacier change (1958–1998) in the North Cascades National Park Complex, Washington, USA. J Glaciol 52(177):251–256

    Article  Google Scholar 

  • Gurney S, Popovnin V, Shahgedanova M, Stokes C (2008) A glacier inventory for the Buordakh Massif, Cherskiy Range, northeast Siberia, and evidence for recent glacier recession. Arct Antar Alp Res 40(1):81–88. doi:10.1657/1523-0430(06-042)

    Article  Google Scholar 

  • Haeberli W, Hoelzle M, Paul F, Zemp M (2007) Integrated monitoring of mountain glaciers as key indicators of global climate change: the European Alps. Ann Glaciol 46:150–160

    Article  Google Scholar 

  • Hoffman M, Fountain A, Achuff J (2007) 20th-century variations in area of cirque glaciers and glacierets, Rocky Mountain National Park, Rocky Mountains, Colorado, USA. Ann Glaciol 46:349–354. doi:10.3189/172756407782871233

    Article  Google Scholar 

  • Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Leetmaa A, Reynolds R, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Jenne R, Joseph D (1996) The NCEP/NCAR 40 year reanalysis project. Bull Amer Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Krenke AN (1982) Mass-exchange in glacier systems over the territory of the USSR. Gidrometeoizdat, Leningrad (in Russian)

    Google Scholar 

  • Kutuzov S, 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. Glob Plan Change 69:59–70. doi:10.1016/j.gloplacha.2009.07.001

    Article  Google Scholar 

  • Lehmkuhl F (2012) Holocene glaciers in the Mongolian Altai: an example from the Turgen-Kharkhiraa Mountains. J Asian Earth Sci 52:12–20. doi:10.1016/j.jseaes.2011.11.027

    Article  Google Scholar 

  • Li Ya, Li Yi (2014) Topographic and geometric controls on glacier changes in the central Tien Shan, China, since the Little Ice Age. Ann Glaciol 55(66):177–186. doi:10.3189/2014AoG66A031

    Article  Google Scholar 

  • Li Ya, McNelis J, Li Yi, Lu X (2015) Glacier boundary extraction using high resolution Google Earth satellite imagery: a case study from the Bogeda Range, Eastern Tian Shan, China (this issue)

  • Macheret YY, Kutuzov SS, Matskovsky VV, Lavrentiev II (2013) On the estimation of ice volume of alpine glaciers. Ice Snow 121(1):5–15 (in Russian)

    Article  Google Scholar 

  • Meier M (1984) Contribution of small glaciers to global sea level. Science 226:1418–1420

    Article  Google Scholar 

  • Meier M, Dyurgerov M, McCabe G (2003) The health of glaciers: recent changes in glacier regime. Clim Change 59:123–135

    Article  Google Scholar 

  • Narozhniy Y, Zemtsov V (2011) Current state of the Altai glaciers (Russia) and trends over the period of instrumental observations 1952–2008. Ambio 40:575–588. doi:10.1007/s13280-011-0166-0

    Article  Google Scholar 

  • Novikova ZS, Grinberg AM (1972) Catalogue of glaciers of the USSR: Lena-Indigirka region, basins of Chara and Vitim rivers (Kodar Ridge). Gidrometeoizdat, Leningrad

    Google Scholar 

  • Oerlemans J, Anderson B, Hubbard A, Huybrechts P, Johannesson T, Knap WH, Schmeits M, Stroeven AP, van de Wal RSW, Wallinga J, Zuo Z (1998) Modelling the response of glaciers to climate warming. Clim Dyn 14:267–274

    Article  Google Scholar 

  • Osipov EY, Osipova OP (2014) Mountain glaciers of southeast Siberia: current state and changes since the Little Ice Age. Ann Glaciol 55(66):167–176. doi:10.3189/2014AoG66A135

    Article  Google Scholar 

  • Osipov EY, Osipova OP, Golobokova LP (2012) Assessment of the current state of South Sygyktinsky Glacier—one of the largest glaciers of Kodar Range. Ice Snow 118(2):51–58 (in Russian)

    Google Scholar 

  • Paul F, Andreassen L (2009) A new glacier inventory for the Svartisen region, Norway, from Landsat ETM+ data: challenges and change assessment. J Glaciol 55(192):607–618

    Article  Google Scholar 

  • Paul F, Kääb A, Maisch M, Kellenberger T, Haeberli W (2004) Rapid disintegration of Alpine glaciers observed with satellite data. Geophys Res Lett 31:L21402. doi:10.1029/2004GL020816

    Article  Google Scholar 

  • Paul F, Kääb A, Haeberli W (2007) Recent glacier changes in the Alps observed by satellite: consequences for future monitoring strategies. Glob Plan Change 56:111–122. doi:10.1016/j.gloplacha.2006.07.007

    Article  Google Scholar 

  • Paul F, Barry RG, Cogley JG, Frey H, Haeberli W, Ohmura A, Ommanney CSL, Raup B, Rivera A, Zemp M (2009) Recommendations for the compilation of glacier inventory data from digital sources. Ann Glaciol 50(53):119–126

    Article  Google Scholar 

  • Plastinin LA (1998) Remote mapping study of nival-glacial complexes in mountain regions of Siberia (morphology and dynamics of glaciers, snowfields and icings of Kodar Ridge in Transbaikalia). ISTU, Irkutsk

    Google Scholar 

  • Preobrazhenskiy VS (1960) Kodar glacial area (Transbaykalia). Publishing House of the Academy of Sciences of the USSR, Moscow

    Google Scholar 

  • Shahgedanova M, Popovnin V, Aleynikov A, Stokes CR (2011) Geodetic mass balance of Azarova Glacier, Kodar mountains, eastern Siberia, and its links to observed and projected climatic change. Ann Glaciol 52(58):129–137. doi:10.3189/172756411797252275

    Article  Google Scholar 

  • Solomina ON (1999) Mountain glaciation of Northern Eurasia in the Holocene. Scientific World Press, Moscow

    Google Scholar 

  • Solomina ON (2000) Retreat of mountain glaciers of northern Eurasia since the Little Ice Age maximum. Ann Glaciol 31:26–30. doi:10.3189/172756400781820499

    Article  Google Scholar 

  • Stepanova OG, Trunova VA, Zvereva VV, Melgunov MS, Fedotov AP (2015) Reconstruction of glacier fluctuations in the East Sayan, Baikalsky and Kodar Ridges (East Siberia, Russia) during the last 210 years based on high-resolution geochemical proxies from proglacial lake bottom sediments (this issue)

  • Stokes CR, Shahgedanova M, Evans IS, Popovnin VV (2013) Accelerated loss of alpine glaciers in the Kodar Mountains, south-eastern Siberia. Glob Plan Change 101:82–96. doi:10.1016/j.gloplacha.2012.12.010

    Article  Google Scholar 

  • Tennant C, Menounos B, Wheate R, Clague J (2012) Area change of glaciers in the Canadian Rocky Mountains, 1919–2006. Cryosphere 6:1541–1552. doi:10.5194/tc-6-1541-2012

    Article  Google Scholar 

  • Wang S, Zhang T (2014) Spatial change detection of glacial lakes in the Koshi River Basin, the Central Himalayas Environ. Earth Sci 72:4381–4391. doi:10.1007/s12665-014-3338-y

    Article  Google Scholar 

  • Wang P, Li Z, Li H, Cao M, Wang W, Wang F (2012) Glacier No. 4 of Sigong River over Mt. Bogda of eastern Tianshan, central Asia: thinning and retreat during the period 1962–2009. Environ Earth Sci 66:265–273. doi:10.1007/s12665-011-1236-0

    Article  Google Scholar 

  • Winsvold S, Andreassen L, Kienholz C (2014) Glacier area and length changes in Norway from repeat inventories. Cryosphere Discuss 8(3):3069–3115. doi:10.5194/tcd-8-3069-2014

    Article  Google Scholar 

  • Wu Z, Shiyin L, Shiqiang Z, Honglang X (2013) Internal structure and trend of glacier change assessed by geophysical investigations. Environ Earth Sci 68:1513–1525. doi:10.1007/s12665-012-1845-2

    Article  Google Scholar 

  • Zemp M, Paul F, Hoelzle M, Haeberli W (2008) Glacier fluctuations in the European Alps, 1850–2000: an overview and spatio-temporal analysis of available data. In: Orlove B, Wiegandt E, Luckman B (eds) Darkening Peaks: glacier retreat, science, and society. University of California Press, Berkeley, pp 152–167

    Google Scholar 

  • Zhou J, Li Z, Guo W (2014) Estimation and analysis of the surface velocity field of mountain glaciers in Muztag Ata using satellite SAR data. Environ Earth Sci 71:3581–3592. doi:10.1007/s12665-013-2749-5

    Article  Google Scholar 

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Acknowledgments

We are very grateful to three anonymous reviewers for their valuable comments and suggestions. The present study was carried out within the framework of the Federal Agency of Research Organizations (state job VIII.76.1.6.) and supported by the Russian Foundation for Basic Research (projects #15-05-04525 and #13-05-00022), and by Department of Earth Sciences of RAS (project 12.11). We are grateful to A. Fedotov, K. Vershinin, A. Ashmetiev, V. Ashmetiev and V. Isaev for their help in field investigations.

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The authors declare that they have no conflict of interest.

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  1. Limnological Institute of SB RAS, Ulan-Batorskaya st., 3, 664033, Irkutsk, Russia

    E. Y. Osipov

  2. V.B. Sochava Institute of Geography of SB RAS, Ulan-Batorskaya st., 1, 664033, Irkutsk, Russia

    O. P. Osipova

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  1. E. Y. Osipov
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Osipov, E.Y., Osipova, O.P. Glaciers of the Levaya Sygykta River watershed, Kodar Ridge, southeastern Siberia, Russia: modern morphology, climate conditions and changes over the past decades. Environ Earth Sci 74, 1969–1984 (2015). https://doi.org/10.1007/s12665-015-4352-4

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