Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century

The paper compares remotely sensed glacier inventories of the Byrranga, Suntar-Khayata, and Chersky ranges (2003), Koryak Highland and Chukotka mountains (2008) with data from the Inventory of Glaciers of the USSR (1945–1985). We studied changes in glacier area since the Inventory, which was primari...

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Main Author: M. D. Ananicheva
Format: Article
Language:Russian
Published: Nauka 2015-03-01
Series:Lëd i Sneg
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/22
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spelling doaj-c02c863b5ff243009032d76d6a25888a2021-08-02T08:42:06ZrusNaukaLëd i Sneg2076-67342412-37652015-03-01541354710.15356/2076-6734-2014-1-35-4716Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI centuryM. D. Ananicheva0Institute of Geography, Russian Academy of Sciences, MoscowThe paper compares remotely sensed glacier inventories of the Byrranga, Suntar-Khayata, and Chersky ranges (2003), Koryak Highland and Chukotka mountains (2008) with data from the Inventory of Glaciers of the USSR (1945–1985). We studied changes in glacier area since the Inventory, which was primarily based on aerial photos and field research. The glaciers have been classified by orientation (aspect) and morphological type. Overall the glacierization of the Chersky Range (1970–2003), Suntar-Khayata (1945–2003), Byrranga (1967–2003), Koryak Highland (1950–2003) and Meynypilginsky Range (1984–2008) reduced by about 30, 20, 15, 60 (debatable value) and 25% respectively due to summer temperature rise. Calculation of glacier volumes for the dates indicated in the USSR Glacier Inventory and satellite imagery: during this period in sum for 5 studied glacier regions the area, covered by ice, has decreased by 225.2 km², and ice volume – by 8.7 Gtg. Construction of spatial patterns (maps) of current ELA for 3 different by climate mountain regions – the Suntar-Khayata Mountains– Chersky Range, and Meynypilgynsky Range ( North Far East), showed that despite of retreat of the glaciers, the mean ELA change for the first studied region is not large compared with the data from the Glacier Inventory (100 m ), and significant for the second (100–150 m).https://ice-snow.igras.ru/jour/article/view/22aspect of glacierequilibrium line altitudeglacier areamorphological typespace imagethe ussr glacier inventory
collection DOAJ
language Russian
format Article
sources DOAJ
author M. D. Ananicheva
spellingShingle M. D. Ananicheva
Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century
Lëd i Sneg
aspect of glacier
equilibrium line altitude
glacier area
morphological type
space image
the ussr glacier inventory
author_facet M. D. Ananicheva
author_sort M. D. Ananicheva
title Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century
title_short Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century
title_full Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century
title_fullStr Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century
title_full_unstemmed Assessment of area, volume and ELA of glacial systems in Northeast Russia from satellite images in the beginning of XXI century
title_sort assessment of area, volume and ela of glacial systems in northeast russia from satellite images in the beginning of xxi century
publisher Nauka
series Lëd i Sneg
issn 2076-6734
2412-3765
publishDate 2015-03-01
description The paper compares remotely sensed glacier inventories of the Byrranga, Suntar-Khayata, and Chersky ranges (2003), Koryak Highland and Chukotka mountains (2008) with data from the Inventory of Glaciers of the USSR (1945–1985). We studied changes in glacier area since the Inventory, which was primarily based on aerial photos and field research. The glaciers have been classified by orientation (aspect) and morphological type. Overall the glacierization of the Chersky Range (1970–2003), Suntar-Khayata (1945–2003), Byrranga (1967–2003), Koryak Highland (1950–2003) and Meynypilginsky Range (1984–2008) reduced by about 30, 20, 15, 60 (debatable value) and 25% respectively due to summer temperature rise. Calculation of glacier volumes for the dates indicated in the USSR Glacier Inventory and satellite imagery: during this period in sum for 5 studied glacier regions the area, covered by ice, has decreased by 225.2 km², and ice volume – by 8.7 Gtg. Construction of spatial patterns (maps) of current ELA for 3 different by climate mountain regions – the Suntar-Khayata Mountains– Chersky Range, and Meynypilgynsky Range ( North Far East), showed that despite of retreat of the glaciers, the mean ELA change for the first studied region is not large compared with the data from the Glacier Inventory (100 m ), and significant for the second (100–150 m).
topic aspect of glacier
equilibrium line altitude
glacier area
morphological type
space image
the ussr glacier inventory
url https://ice-snow.igras.ru/jour/article/view/22
work_keys_str_mv AT mdananicheva assessmentofareavolumeandelaofglacialsystemsinnortheastrussiafromsatelliteimagesinthebeginningofxxicentury
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