GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS

SummaryPaper presents the results of interpretation of space images (from Landsat and World View-2), which made possible to estimate the areal extent of glaciers ofMeynypilgynskyRange, North-East of Koryak Upland, in the early 2000's. Assessments of glaciers were analyzed in comparison with the...

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Published in:Ice and Snow
Main Authors: M. Ananicheva D., G. Kapustin A., A. Mikhailov Yu., М. Ананичева Д., Г. Капустин А., А. Михайлов Ю.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2015
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/225
id ftjias:oai:oai.ice.elpub.ru:article/225
record_format openpolar
institution Open Polar
collection Ice and Snow (E-Journal)
op_collection_id ftjias
language Russian
topic Climatic scenario
equilibrium line altitude
glacier area
glacier system
image interpretation
space image
Высота границы питания
дешифрирование снимков
климатический сценарий
космический снимок
ледниковая система
площадь ледника
spellingShingle Climatic scenario
equilibrium line altitude
glacier area
glacier system
image interpretation
space image
Высота границы питания
дешифрирование снимков
климатический сценарий
космический снимок
ледниковая система
площадь ледника
M. Ananicheva D.
G. Kapustin A.
A. Mikhailov Yu.
М. Ананичева Д.
Г. Капустин А.
А. Михайлов Ю.
GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS
topic_facet Climatic scenario
equilibrium line altitude
glacier area
glacier system
image interpretation
space image
Высота границы питания
дешифрирование снимков
климатический сценарий
космический снимок
ледниковая система
площадь ледника
description SummaryPaper presents the results of interpretation of space images (from Landsat and World View-2), which made possible to estimate the areal extent of glaciers ofMeynypilgynskyRange, North-East of Koryak Upland, in the early 2000's. Assessments of glaciers were analyzed in comparison with the Glacier Inventory of the region, compiled by R.V. Sedov (2001), as a whole and for groups of glaciers belonging to the selected six glacial systems. After dozens of years since the compilation of the Inventory (1985) and from some glacier data referred to 1967, the glaciers ofMeynypilgynskyRangelost about 30% of the area, mainly due to drying that accompanies climate warming. The analysis of glaciers, which had retreated, was conducted for the groups by the same morphological type, and the same aspect. The largest retreat and area reduction is relevant to valley-corrie and hanging glaciers of eastern aspect. Glaciers facing north less suffered. As a result of application of the developed methodology for assessing the evolution of glacier systems under given climate scenario, the parameters for the state of the glacier systems ofMeynypilgynskyRangeup to the time span 2049–2060 were obtained. The AOGCM–ECHAM 5 (B1) was used as a scenario; it is the optimal for theNorthern Eurasia. It turned out that the glaciers reduction would be catastrophic (about 90%), but nevertheless they would not completely disappeared. Дешифрирование космических снимков спутников Landsat и WorldView-2 позволило оценить площадное распространение оледенения в пределах Мейныпильгынского хребта (северо-восток Корякского нагорья) в начале 2000-х годов. Полученные результаты сравнивались с данными Каталога этого региона, составленного Р.В. Седовым [16], как в целом по региону, так и по группам ледников, относящихся к шести выделенным нами ледниковым системам. За несколько десятков лет, прошедших со времени составления Каталога (1980-е годы), ледники Мейныпильгынского хребта потеряли около 30% площади, в основном за счёт уменьшения количества твёрдых ...
format Article in Journal/Newspaper
author M. Ananicheva D.
G. Kapustin A.
A. Mikhailov Yu.
М. Ананичева Д.
Г. Капустин А.
А. Михайлов Ю.
author_facet M. Ananicheva D.
G. Kapustin A.
A. Mikhailov Yu.
М. Ананичева Д.
Г. Капустин А.
А. Михайлов Ю.
author_sort M. Ananicheva D.
title GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS
title_short GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS
title_full GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS
title_fullStr GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS
title_full_unstemmed GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS
title_sort glaciers in the meynypilgynsky range: current state and development forecast of glacier systems
publisher IGRAS
publishDate 2015
url https://ice-snow.igras.ru/jour/article/view/225
long_lat ENVELOPE(14.083,14.083,-69.367,-69.367)
geographic Sedov
geographic_facet Sedov
genre Arctic
Arctic and Alpine Research
Koryak
The Cryosphere
genre_facet Arctic
Arctic and Alpine Research
Koryak
The Cryosphere
op_source Ice and Snow; Том 52, № 2 (2012); 40-50
Лёд и Снег; Том 52, № 2 (2012); 40-50
2412-3765
2076-6734
10.15356/2076-6734-2012-2
op_relation Alekseev G.V., Pnyushkov A.V., Ivanov N.E., Ashik I.M., Sokolov V.T., Golovin P.N., Bogorodsky P.V. Complex evaluation of climatic changes in maritime Arctic using the data of IPY2007/08. Problemy Arktiki. Problems of Arctic. 2009, 1 (81): 7–14. [In Russian].
Ananicheva M.D. Fields of glaciological characteristics for scenario ECHAM 4: north-east Siberia and Kamchatka. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2009, 107: 81–87. [In Russian].
Ananicheva M.D. Present-day glaciers of the Koryak Highland and assessment of their evolution in the nearest future. Led i Sneg. Ice and Snow. 2011, 4 (112): 47–56. [In Russian].
Ananicheva M.D., Kapustin G.A., Koreisha M.M. Changes of glaciers in the Suntar-Khayata Mountains and Chersky Range according to the data of the USSR Glacier Inventory and space images of 2001–2003. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2006, 101: 163–169. [In Russian].
Ananicheva M.D., Kapustin G.A. Assessment glacier changes in the Byrranga mountains according to the space images and data of the USSR Glacier Inventory. Led i Sneg. Ice and Snow. 2010, 3 (111): 19–27. [In Russian].
Ananicheva M.D., Krenke A.N. Flaciological prediction. Mountain glaciation (North-East of Russia and Kamchatka as examples). Oledenenie Severnoy Evrazii v nedavnem proshlom i blizhayshem budushchem. Glaciation in North Eurasia in the recent past and immediate future. Moscow: Nauka, 2007: 277–293. [In Russian].
Zhiltsova E.L., Anisimov O.A. On precision of reproduction of temperature and precipitation on the territory of Russia by global climatic archives. Meteorologiya i Gidrologiya. Meteorology and Hydrology. 2009, 10: 79–89. [In Russian].
Kononova N.K. Klassifikatsiya tsirkulyatsionnykh mekhanizmov Severnogo polushariya po B.L.Dzerdzeevskomy. Classification of circulation mechanisms in the Northern Hemisphere according to B.L. Dzerdzeevsky. Ed. A.B. Shmakin. Moscow: 2009: 372 p. [In Russian].
Kotlyakov V.M., Khromova T.E., Zverkova N.M., Chernova L.P., Nosenko G.A. Two new glacier systems at the north-east of Eurasia. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2011, 437 (1): 108–113. [In Russian].
Krenke A.N. Massoobmen v lednikovykh sistemakh na territorii SSSR. Mass-exchange in glacier systems at the territory of the USSR. Leningrad: Hydrometeoizdat, 1982: 488 p. [In Russian].
Krenke A.N., Chernova L.P. Glacier Systems in the North-East of the USSR. Izvestya Ross. Akad. Nauk, Seriya Geogr. Proc. of the RAS, Geographical Series. 1980, 1: 17–33. [In Russian].
Krenke A.N., Kitaev L.M., Turkov D.V. Climatic role of the snow cover changes in the period of warming. Izvestya Ross. Akad. Nauk, Seriya Geogr. Proc. of the RAS, Geographical Series. 2001, 4: 44–50. [In Russian].
Magidovich I.P., Magidovich V.I. Ocherki po istorii geograficheskikh otkrytiy. Essays on history of geographical discoveries. V. 5. Moscow, 1986: 223 p. [In Russian].
Mikhailov A.Yu. Role of orographic vertical movement in the formation of climatic field of summer precipitation. Izvestya Ross. Akad. Nauk, Seriya Geogr. Proc. of the RAS, Geographical Series. 1985, 5: 96–103. [In Russian].
Mikhailov A.Yu. Calculation of the influence of relief to the value of vertical wind velocity. Izvestya Ross. Akad. Nauk. Fizika atmosfery i okeana. Proc. of the USSR Academy of Sciences. Physics of atmosphere and ocean. 1986, 5: 543–546. [In Russian].
Sedov R.V. Glacier inventory of the north-east part of Koryak Highland. V. 19. North-East. Pt. 1. Meynypilgynsky Range. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2001, 91: 195–224. [In Russian].
Ananicheva M.D., Krenke A.N., Barry R.G. The Northeast Asia mountain glaciers in the near future by AOGCM scenarios. The Cryosphere. 2010, 4: 435–445.
Bacher A., Oberhuber J.M., Roeckner E. ENSO dynamics and seasonal cycle in the tropical Pacific as simulated by the ECHAM4/OPYC3 coupled general circulation model. Climate Dynamics. 1998, 14: 431–450.
GLIMS RC 18 procedures and guidelines for glacier analysis Frank Rau, Steffen Vogt, Fabian Mauz & Florian König Institut für Physische Geographie, Freiburg (Germany) (Version 2.0). 2004–12–15.
Davidovich N.V., Ananicheva M.D. Prediction of possible changes in glacio-hydrological characteristics under global warming: south-eastern Alaska, USA. Journ. of Glaciology. 1996, 42 (142): 407–412.
Johannesson T., Raymond C.F., Waddington E.D. Timescale for adjustments of glaciers to changes in mass balance. Journ. of Glaciology. 1989, 35 (121): 355–369.
Wendler G., Ishikawa N., Streten N. The climate of the McCall Glacier, Brooks Range, Alaska, in relation to its geographical setting. Arctic and Alpine Research. 1974, 6: 307–318.
https://ice-snow.igras.ru/jour/article/view/225
op_rights Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).
Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access).
op_rightsnorm CC-BY
op_doi https://doi.org/10.15356/2076-6734-2012-2
container_title Ice and Snow
container_volume 52
container_issue 2
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spelling ftjias:oai:oai.ice.elpub.ru:article/225 2023-05-15T14:28:15+02:00 GLACIERS IN THE MEYNYPILGYNSKY RANGE: CURRENT STATE AND DEVELOPMENT FORECAST OF GLACIER SYSTEMS ЛЕДНИКИ МЕЙНЫПИЛЬГЫНСКОГО ХРЕБТА: СОВРЕМЕННОЕ СОСТОЯНИЕ И ПРОГНОЗ ЭВОЛЮЦИИ ЛЕДНИКОВЫХ СИСТЕМ M. Ananicheva D. G. Kapustin A. A. Mikhailov Yu. М. Ананичева Д. Г. Капустин А. А. Михайлов Ю. 2015-11-15 https://ice-snow.igras.ru/jour/article/view/225 ru rus IGRAS Alekseev G.V., Pnyushkov A.V., Ivanov N.E., Ashik I.M., Sokolov V.T., Golovin P.N., Bogorodsky P.V. Complex evaluation of climatic changes in maritime Arctic using the data of IPY2007/08. Problemy Arktiki. Problems of Arctic. 2009, 1 (81): 7–14. [In Russian]. Ananicheva M.D. Fields of glaciological characteristics for scenario ECHAM 4: north-east Siberia and Kamchatka. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2009, 107: 81–87. [In Russian]. Ananicheva M.D. Present-day glaciers of the Koryak Highland and assessment of their evolution in the nearest future. Led i Sneg. Ice and Snow. 2011, 4 (112): 47–56. [In Russian]. Ananicheva M.D., Kapustin G.A., Koreisha M.M. Changes of glaciers in the Suntar-Khayata Mountains and Chersky Range according to the data of the USSR Glacier Inventory and space images of 2001–2003. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2006, 101: 163–169. [In Russian]. Ananicheva M.D., Kapustin G.A. Assessment glacier changes in the Byrranga mountains according to the space images and data of the USSR Glacier Inventory. Led i Sneg. Ice and Snow. 2010, 3 (111): 19–27. [In Russian]. Ananicheva M.D., Krenke A.N. Flaciological prediction. Mountain glaciation (North-East of Russia and Kamchatka as examples). Oledenenie Severnoy Evrazii v nedavnem proshlom i blizhayshem budushchem. Glaciation in North Eurasia in the recent past and immediate future. Moscow: Nauka, 2007: 277–293. [In Russian]. Zhiltsova E.L., Anisimov O.A. On precision of reproduction of temperature and precipitation on the territory of Russia by global climatic archives. Meteorologiya i Gidrologiya. Meteorology and Hydrology. 2009, 10: 79–89. [In Russian]. Kononova N.K. Klassifikatsiya tsirkulyatsionnykh mekhanizmov Severnogo polushariya po B.L.Dzerdzeevskomy. Classification of circulation mechanisms in the Northern Hemisphere according to B.L. Dzerdzeevsky. Ed. A.B. Shmakin. Moscow: 2009: 372 p. [In Russian]. Kotlyakov V.M., Khromova T.E., Zverkova N.M., Chernova L.P., Nosenko G.A. Two new glacier systems at the north-east of Eurasia. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2011, 437 (1): 108–113. [In Russian]. Krenke A.N. Massoobmen v lednikovykh sistemakh na territorii SSSR. Mass-exchange in glacier systems at the territory of the USSR. Leningrad: Hydrometeoizdat, 1982: 488 p. [In Russian]. Krenke A.N., Chernova L.P. Glacier Systems in the North-East of the USSR. Izvestya Ross. Akad. Nauk, Seriya Geogr. Proc. of the RAS, Geographical Series. 1980, 1: 17–33. [In Russian]. Krenke A.N., Kitaev L.M., Turkov D.V. Climatic role of the snow cover changes in the period of warming. Izvestya Ross. Akad. Nauk, Seriya Geogr. Proc. of the RAS, Geographical Series. 2001, 4: 44–50. [In Russian]. Magidovich I.P., Magidovich V.I. Ocherki po istorii geograficheskikh otkrytiy. Essays on history of geographical discoveries. V. 5. Moscow, 1986: 223 p. [In Russian]. Mikhailov A.Yu. Role of orographic vertical movement in the formation of climatic field of summer precipitation. Izvestya Ross. Akad. Nauk, Seriya Geogr. Proc. of the RAS, Geographical Series. 1985, 5: 96–103. [In Russian]. Mikhailov A.Yu. Calculation of the influence of relief to the value of vertical wind velocity. Izvestya Ross. Akad. Nauk. Fizika atmosfery i okeana. Proc. of the USSR Academy of Sciences. Physics of atmosphere and ocean. 1986, 5: 543–546. [In Russian]. Sedov R.V. Glacier inventory of the north-east part of Koryak Highland. V. 19. North-East. Pt. 1. Meynypilgynsky Range. Materialy Glyatsiologicheskikh Issledovaniy. Data of Glaciological Studies. 2001, 91: 195–224. [In Russian]. Ananicheva M.D., Krenke A.N., Barry R.G. The Northeast Asia mountain glaciers in the near future by AOGCM scenarios. The Cryosphere. 2010, 4: 435–445. Bacher A., Oberhuber J.M., Roeckner E. ENSO dynamics and seasonal cycle in the tropical Pacific as simulated by the ECHAM4/OPYC3 coupled general circulation model. Climate Dynamics. 1998, 14: 431–450. GLIMS RC 18 procedures and guidelines for glacier analysis Frank Rau, Steffen Vogt, Fabian Mauz & Florian König Institut für Physische Geographie, Freiburg (Germany) (Version 2.0). 2004–12–15. Davidovich N.V., Ananicheva M.D. Prediction of possible changes in glacio-hydrological characteristics under global warming: south-eastern Alaska, USA. Journ. of Glaciology. 1996, 42 (142): 407–412. Johannesson T., Raymond C.F., Waddington E.D. Timescale for adjustments of glaciers to changes in mass balance. Journ. of Glaciology. 1989, 35 (121): 355–369. Wendler G., Ishikawa N., Streten N. The climate of the McCall Glacier, Brooks Range, Alaska, in relation to its geographical setting. Arctic and Alpine Research. 1974, 6: 307–318. https://ice-snow.igras.ru/jour/article/view/225 Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access). Авторы, публикующие статьи в данном журнале, соглашаются на следующее:Авторы сохраняют за собой авторские права и предоставляют журналу право первой публикации работы, которая по истечении 6 месяцев после публикации автоматически лицензируется на условиях Creative Commons Attribution License , что позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Редакция журнала будет размещать принятую для публикации статью на сайте журнала до выхода её в свет (после утверждения к печати редколлегией журнала). Авторы также имеют право размещать их работу в сети Интернет (например в институтском хранилище или персональном сайте) до и во время процесса рассмотрения ее данным журналом, так как это может привести к продуктивному обсуждению и большему количеству ссылок на данную работу (См. The Effect of Open Access). CC-BY Ice and Snow; Том 52, № 2 (2012); 40-50 Лёд и Снег; Том 52, № 2 (2012); 40-50 2412-3765 2076-6734 10.15356/2076-6734-2012-2 Climatic scenario equilibrium line altitude glacier area glacier system image interpretation space image Высота границы питания дешифрирование снимков климатический сценарий космический снимок ледниковая система площадь ледника info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2012-2 2022-12-20T13:29:52Z SummaryPaper presents the results of interpretation of space images (from Landsat and World View-2), which made possible to estimate the areal extent of glaciers ofMeynypilgynskyRange, North-East of Koryak Upland, in the early 2000's. Assessments of glaciers were analyzed in comparison with the Glacier Inventory of the region, compiled by R.V. Sedov (2001), as a whole and for groups of glaciers belonging to the selected six glacial systems. After dozens of years since the compilation of the Inventory (1985) and from some glacier data referred to 1967, the glaciers ofMeynypilgynskyRangelost about 30% of the area, mainly due to drying that accompanies climate warming. The analysis of glaciers, which had retreated, was conducted for the groups by the same morphological type, and the same aspect. The largest retreat and area reduction is relevant to valley-corrie and hanging glaciers of eastern aspect. Glaciers facing north less suffered. As a result of application of the developed methodology for assessing the evolution of glacier systems under given climate scenario, the parameters for the state of the glacier systems ofMeynypilgynskyRangeup to the time span 2049–2060 were obtained. The AOGCM–ECHAM 5 (B1) was used as a scenario; it is the optimal for theNorthern Eurasia. It turned out that the glaciers reduction would be catastrophic (about 90%), but nevertheless they would not completely disappeared. Дешифрирование космических снимков спутников Landsat и WorldView-2 позволило оценить площадное распространение оледенения в пределах Мейныпильгынского хребта (северо-восток Корякского нагорья) в начале 2000-х годов. Полученные результаты сравнивались с данными Каталога этого региона, составленного Р.В. Седовым [16], как в целом по региону, так и по группам ледников, относящихся к шести выделенным нами ледниковым системам. За несколько десятков лет, прошедших со времени составления Каталога (1980-е годы), ледники Мейныпильгынского хребта потеряли около 30% площади, в основном за счёт уменьшения количества твёрдых ... Article in Journal/Newspaper Arctic Arctic and Alpine Research Koryak The Cryosphere Ice and Snow (E-Journal) Sedov ENVELOPE(14.083,14.083,-69.367,-69.367) Ice and Snow 52 2