Javascript must be enabled to continue!
The Greater Caucasus Glacier Inventory (Russia/Georgia/Azerbaijan)
View through CrossRef
Abstract. While there are a large number of glaciers in the Greater Caucasus, the region is not fully represented in modern glacier databases with previous incomplete inventories. Here, we present an expanded glacier inventory for this region over the 1960–1986–2014 period. Large scale topographic maps and satellite imagery (Landsat 5, Landsat 8 and ASTER) were used to conduct a remote sensing survey of glacier change in the Greater Caucasus mountains. Glacier margins were mapped manually and reveal that, in 1960, the mountains contained 2349 glaciers, with a total glacier surface area of 1674.9 ± 35.2 km2. By 1986, glacier surface area had decreased to 1482.1 ± 32.2 km2 (2209 glaciers), and by 2014, to 1193.2 ± 27.0 km2 (2020 glaciers). This represents a 28.8 ± 2.2 % (481 ± 10.6 km2) reduction in total glacier surface area between 1960 and 2014 and a marked acceleration in the rate of area loss since 1986. Analysis of possible controls suggest that the general decreases in both glacier area and number for the period 1960–2014 are directly due to general increase in temperature, especially in summer (June–July–August), although the response of individual glaciers was modulated by other factors, including glacier size, elevation, rock structure, exposition, morphological type and debris cover. This new glacier inventory can be used as a basis dataset for future studies including glacier change assessment.
Title: The Greater Caucasus Glacier Inventory (Russia/Georgia/Azerbaijan)
Description:
Abstract.
While there are a large number of glaciers in the Greater Caucasus, the region is not fully represented in modern glacier databases with previous incomplete inventories.
Here, we present an expanded glacier inventory for this region over the 1960–1986–2014 period.
Large scale topographic maps and satellite imagery (Landsat 5, Landsat 8 and ASTER) were used to conduct a remote sensing survey of glacier change in the Greater Caucasus mountains.
Glacier margins were mapped manually and reveal that, in 1960, the mountains contained 2349 glaciers, with a total glacier surface area of 1674.
9 ± 35.
2 km2.
By 1986, glacier surface area had decreased to 1482.
1 ± 32.
2 km2 (2209 glaciers), and by 2014, to 1193.
2 ± 27.
0 km2 (2020 glaciers).
This represents a 28.
8 ± 2.
2 % (481 ± 10.
6 km2) reduction in total glacier surface area between 1960 and 2014 and a marked acceleration in the rate of area loss since 1986.
Analysis of possible controls suggest that the general decreases in both glacier area and number for the period 1960–2014 are directly due to general increase in temperature, especially in summer (June–July–August), although the response of individual glaciers was modulated by other factors, including glacier size, elevation, rock structure, exposition, morphological type and debris cover.
This new glacier inventory can be used as a basis dataset for future studies including glacier change assessment.
Related Results
Glacier Mass Loss Simulation Based on Remote Sensing Data: A Case Study of the Yala Glacier and the Qiyi Glacier in the Third Pole
Glacier Mass Loss Simulation Based on Remote Sensing Data: A Case Study of the Yala Glacier and the Qiyi Glacier in the Third Pole
The climate warming over the Third Pole is twice as large as that in other regions and glacier mass loss is considered to be more intensive in the region. However, due to the vast ...
A new global dataset of mountain glacier centerline and length
A new global dataset of mountain glacier centerline and length
Abstract. Length is one of the key determinants of glacier geometry and is an important parameter of glacier inventory and modeling; glacier centerlines are crucial inputs for many...
Azerbaijan – Georgian Relations in the Early 20th Century
Azerbaijan – Georgian Relations in the Early 20th Century
This article examines the relations between Georgia and Azerbaijan in the early 20th century. The article utilizes secondary research methods and applies historical and comparative...
Holocene thinning history of David Glacier, Antarctica
Holocene thinning history of David Glacier, Antarctica
<p>The Antarctic Ice Sheet is a significant component of the Earth System, modulating Earth‘s sea level and climate. Present day and projected ice mass losses from Antarctica...
Studies on the Basal-Ice Zone of Findelen Glacier, Switzerland
Studies on the Basal-Ice Zone of Findelen Glacier, Switzerland
Basal and englacial debris layers have been observed to coincide distinctly with the location of glacier thrust planes or shear zones, e.g. at Shoestring Glacier (Brugman and Meier...
Glaciers Variation at ‘Shocking’ Pace in the Northeastern Margin of Tibetan Plateau from 1957 to 21st Century: A Case Study of Qiyi Glacier
Glaciers Variation at ‘Shocking’ Pace in the Northeastern Margin of Tibetan Plateau from 1957 to 21st Century: A Case Study of Qiyi Glacier
Accelerating glacier shrinkage is one of the most consequential of global warming. Yet, projections for the region remain ambiguous because of the tremendous spatial heterogeneity,...
Glacier Speed-Up Events and Subglacial Hydrology on the Lower Franz Josef Glacier, New Zealand
Glacier Speed-Up Events and Subglacial Hydrology on the Lower Franz Josef Glacier, New Zealand
<p>The contribution of glacier mass loss to future sea level rise is still poorly constrained (Lemke and others, 2007). One of the remaining unknowns is how water inputs infl...
Monitoring glacier fade out in Austrian Eastern Alps
Monitoring glacier fade out in Austrian Eastern Alps
<p>In the Austrian Alps, recent rapid glacier melt affected the glaciers up to the summits. Glacier disintegration, debris flows, rock falls and increased melt rates ...

