Strong acceleration of glacier area loss in the Greater Caucasus between 2000 and 2020
-
Published:2022-02-10
Issue:2
Volume:16
Page:489-504
-
ISSN:1994-0424
-
Container-title:The Cryosphere
-
language:en
-
Short-container-title:The Cryosphere
Author:
Tielidze Levan G.ORCID, Nosenko Gennady A., Khromova Tatiana E., Paul Frank
Abstract
Abstract. An updated glacier inventory is important for understanding glacier behaviour given the accelerating glacier retreat observed around the world. Here,
we present data from a new glacier inventory for two points in time (2000, 2020) covering the entire Greater Caucasus (Georgia, Russia, and
Azerbaijan). Satellite imagery (Landsat, Sentinel, SPOT) was used to conduct a remote-sensing survey of glacier change. The 30 m resolution
Advanced Spaceborne Thermal Emission and Reflection Radiometer Global Digital Elevation Model (ASTER GDEM; 17 November 2011) was used to determine
aspect, slope, and elevations, for all glaciers. Glacier margins were mapped manually and reveal that in 2000 the mountain range contained 2186
glaciers with a total glacier area of 1381.5 ± 58.2 km2. By 2020, the area had decreased to 1060.9 ± 33.6 km2 a
reduction of 23.2 ± 3.8 % (320.6 ± 45.9 km2) or −1.16 % yr−1 over the last 20 years in the Greater
Caucasus. Of the 2223 glaciers, 14 have an area > 10 km2, resulting in the 221.9 km2 or 20.9 % of total glacier area
in 2020. The Bezengi Glacier with an area of 39.4 ± 0.9 km2 was the largest glacier mapped in the 2020 database. Glaciers between
1.0 and 5.0 km2 accounted for 478.1 km2 or 34.6 % in total area in 2000, while they accounted for
354.0 km2 or 33.4 % in total area in 2020. The rates of area shrinkage and mean elevation vary between the northern and southern and
between the western, central, and eastern Greater Caucasus. Area shrinkage is significantly stronger in the eastern Greater Caucasus
(−1.82 % yr−1), where most glaciers are very small. The observed increased summer temperatures and decreased winter precipitation
along with increased Saharan dust deposition might be responsible for the predominantly negative mass balances of Djankuat and Garabashi glaciers
with long-term measurements. Both glacier inventories are available from the Global Land Ice Measurements from Space (GLIMS) database and can be
used for future studies.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
Reference53 articles.
1. Catalog of Glaciers of the USSR:
Katalog Lednitov USSR, vol. 8–9, Gidrometeoizdat, Leningrad, 1967–1978. 2. Chernomorets, S. S., Petrakov, D. A., Aleynikov, A. A., Bekkiev, M. Y., Viskhadzhieva, K. S., Dokukin, M. D., Kalov, R. K., Kidyaeva, V. M., Krylenko, V. V., Krylenko, I. V., Krylenko, I. N., Rets, E. P., and Savernyuk, E. A., and Smirnov A. M.:
The outburst of Bashkara glacier lake (Central Caucasus, Russia) on September 1, 2017,
Earth's Cryosphere,
XXII, 70–80, https://doi.org/10.21782/KZ1560-7496-2018-2(70-80), 2018. 3. Cogley, J. G.:
A more complete version of the World Glacier Inventory,
Ann. Glaciol.,
50, 32–38, https://doi.org/10.3189/172756410790595859, 2009. 4. Dumont, M., Tuzet, F., Gascoin, S., Picard, G., Kutuzov, S., Lafaysse, M., Cluzet, B., Nheili, R., and Painter, T. H.:
Accelerated snow melt in the Russian Caucasus mountains after the Saharan dust outbreak in March 2018,
J. Geophys. Res.-Earth,
125, e2020JF005641, https://doi.org/10.1029/2020JF005641, 2020. 5. Evans, S. G, Tutubalina, O. V., Drobyshev, V. N., Chernomorets, S. S., McDougall, S., Petrakov, D. A., and Hungr, O.:
Catastrophic detachment and high-velocity long-runout flow of Kolka Glacier, Caucasus Mountains, Russia in 2002,
Geomorphology,
105, 314–321, https://doi.org/10.1016/j.geomorph.2008.10.008, 2009.
Cited by
21 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|