Knowledge of supra-glacial debris cover and its changes remain incomplete in the Greater Caucasus, in spite of recent glacier studies. Here we present data of supra-glacial debris cover for 659 glaciers across the Greater Caucasus based on Landsat and SPOT images from the years 1986, 2000 and 2014. We combined semi-automated methods for mapping the clean ice with manual digitization of debris-covered glacier parts and calculated supra-glacial debris-covered area as the residual between these two maps. The accuracy of the results was assessed by using high-resolution Google Earth imagery and GPS data for selected glaciers. From 1986 to 2014, the total glacier area decreased from 691.5±29.0 to 590.0±25.8 km2 (15.8±4.1 %, or ∼0.52 % yr−1), whi...
Data from the new glacier inventory at two time periods (2000, 2020) covering the entire Greater Cau...
We have generalized observation data on the Fisht Glacier – the most western glacier in the Caucasus...
In this study, we used glacier mass balance and thickness data obtained from geodetic method by Hugo...
Knowledge of supra-glacial debris cover and its changes remain incomplete in the Greater Caucasus, i...
Debris cover on glaciers can significantly alter melt, and hence, glacier mass balance and runoff. D...
This paper reports changes in supraglacial debris cover and supra-/proglacial lake development assoc...
More than 13% of the area of the Caucasus glaciers is covered by debris affecting glacier mass balan...
Glaciers occupy an area of similar to 1600 km(2) in the Caucasus Mountains. There is widespread evid...
The glacier coverage in the Caucasus Mountains underwent considerable changes during the last decade...
An updated glacier inventory is important for understanding glacier behaviour given the accelerating...
Changes in the map area of 498 glaciers located on the Main Caucasus ridge (MCR) and on Mt. Elbrus i...
Glaciers and snow in the Caucasus are major sources of runoff for populated places in many parts of ...
Changes in the area and number of glaciers in the Georgian Caucasus Mountains were examined over the...
Changes in the map area of 498 glaciers located on the Main Caucasus ridge (MCR) and on Mt. Elbrus i...
Glaciers occupy an area of ∼1600 km2 in the Caucasus Mountains. There is widespread evidence of retr...
Data from the new glacier inventory at two time periods (2000, 2020) covering the entire Greater Cau...
We have generalized observation data on the Fisht Glacier – the most western glacier in the Caucasus...
In this study, we used glacier mass balance and thickness data obtained from geodetic method by Hugo...
Knowledge of supra-glacial debris cover and its changes remain incomplete in the Greater Caucasus, i...
Debris cover on glaciers can significantly alter melt, and hence, glacier mass balance and runoff. D...
This paper reports changes in supraglacial debris cover and supra-/proglacial lake development assoc...
More than 13% of the area of the Caucasus glaciers is covered by debris affecting glacier mass balan...
Glaciers occupy an area of similar to 1600 km(2) in the Caucasus Mountains. There is widespread evid...
The glacier coverage in the Caucasus Mountains underwent considerable changes during the last decade...
An updated glacier inventory is important for understanding glacier behaviour given the accelerating...
Changes in the map area of 498 glaciers located on the Main Caucasus ridge (MCR) and on Mt. Elbrus i...
Glaciers and snow in the Caucasus are major sources of runoff for populated places in many parts of ...
Changes in the area and number of glaciers in the Georgian Caucasus Mountains were examined over the...
Changes in the map area of 498 glaciers located on the Main Caucasus ridge (MCR) and on Mt. Elbrus i...
Glaciers occupy an area of ∼1600 km2 in the Caucasus Mountains. There is widespread evidence of retr...
Data from the new glacier inventory at two time periods (2000, 2020) covering the entire Greater Cau...
We have generalized observation data on the Fisht Glacier – the most western glacier in the Caucasus...
In this study, we used glacier mass balance and thickness data obtained from geodetic method by Hugo...