Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century

As it is known from recent investigations 448 glaciers are situated on the Kamchatka Peninsula, their total area are about 905 km2 [8]. More than 80% of them are glaciers of the Sredinny Range and the Klyuchevskaya group that is explained by large altitudes of them. Glaciers of the Kronotsky Penisul...

Full description

Bibliographic Details
Published in:Ice and Snow
Main Authors: A. Muravjev Ya., А. Муравьёв Я.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2015
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/38
https://doi.org/10.15356/2076-6734-2014-2-22-28
id ftjias:oai:oai.ice.elpub.ru:article/38
record_format openpolar
institution Open Polar
collection Ice and Snow (E-Journal)
op_collection_id ftjias
language Russian
topic Glacier recession;glaciers;Kamchatka;space survey;USSR Glacier Inventory
Камчатка;Каталог ледников СССР;космическая съёмка;ледники;сокращение ледников
spellingShingle Glacier recession;glaciers;Kamchatka;space survey;USSR Glacier Inventory
Камчатка;Каталог ледников СССР;космическая съёмка;ледники;сокращение ледников
A. Muravjev Ya.
А. Муравьёв Я.
Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century
topic_facet Glacier recession;glaciers;Kamchatka;space survey;USSR Glacier Inventory
Камчатка;Каталог ледников СССР;космическая съёмка;ледники;сокращение ледников
description As it is known from recent investigations 448 glaciers are situated on the Kamchatka Peninsula, their total area are about 905 km2 [8]. More than 80% of them are glaciers of the Sredinny Range and the Klyuchevskaya group that is explained by large altitudes of them. Glaciers of the Kronotsky Penisula are less studied since this territory is practically not influenced by present-day volcanic processes. This paper presents results of investigation of changes in glaciations of the Kronotsky Peninsula and the mountain mass Alney-Chashakondzha (Fig. 1).The following materials are used: 1) the Landsat satellite picture of September 2nd, 2013; 2) pictures from satellite WorldView-2 of July 20th, 2010, and of August 1st, 2012 with spatial resolution of about 1 m; 3) aerial photographs made in August of 1950; 4) topographic maps of the 1:100 000 scale; 5) data from the USSR Glacier Inventory; 6) results of observations at hydrometeorological stations (HMS) Klyuchi and Kronoki (1950–2006) (www.meteo.ru).According to data from the USSR Glacier Inventory 32 glaciers were situated on the Kronotsky Peninsula, their total area 91.9 km2. By 2013, six glaciers disintegrated. Deciphering of the Landsat pictures did show 50 glaciers. Among them 23 glaciers are presented in the Inventory and they still hold their wholeness; 13 glaciers are segments of six disintegrated ones; 14 glaciers found in the pictures are not presented in the Inventory. Changes in areas of the Kronotsky Peninsula glaciers for period 1950–2013 in dependence on their sizes and expositions are shown in Tables 1 and 2.According to the Inventory 26 glaciers were situated in region of the Alney-Chashakondzha massif, their total area 61.4 km2. By 2010, four of them disintegrated. Deciphering of the World-View-2 picture of July 2010 did show 45 glaciers: 20 glaciers are consistent with the Inventory, and they hold their wholeness; 9 glaciers are segments of four disintegrated ones; 16 glaciers found in the pictures are not presented in the Inventory. Changes in ...
format Article in Journal/Newspaper
author A. Muravjev Ya.
А. Муравьёв Я.
author_facet A. Muravjev Ya.
А. Муравьёв Я.
author_sort A. Muravjev Ya.
title Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century
title_short Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century
title_full Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century
title_fullStr Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century
title_full_unstemmed Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century
title_sort glacier size changes in kronotsky peninsula and alney-chashakondzha massif, kamchatka peninsula in the second half of xx century and the beginning of xxi century
publisher IGRAS
publishDate 2015
url https://ice-snow.igras.ru/jour/article/view/38
https://doi.org/10.15356/2076-6734-2014-2-22-28
long_lat ENVELOPE(160.000,160.000,56.000,56.000)
ENVELOPE(160.805,160.805,56.310,56.310)
ENVELOPE(161.148,161.148,54.592,54.592)
geographic Kamchatka Peninsula
Klyuchi
Kronoki
geographic_facet Kamchatka Peninsula
Klyuchi
Kronoki
genre Kamchatka
Kamchatka Peninsula
КАМЧАТК*
genre_facet Kamchatka
Kamchatka Peninsula
КАМЧАТК*
op_source Ice and Snow; Том 54, № 2 (2014); 22-28
Лёд и Снег; Том 54, № 2 (2014); 22-28
2412-3765
2076-6734
10.15356/2076-6734-2014-2
op_relation https://ice-snow.igras.ru/jour/article/view/38/24
Атлас снежно-ледовых ресурсов мира. М: изд. РАН, 1997. 392 с.
Виноградов В.Н., Ходаков В.Г. Баланс льда ледника Корыто в Кроноцком массиве Камчатки // Гляциол. исследования. 1976. № 25. С. 18–26.
Глазырин Г.Е., Муравьев Я.Д., Виноградов В.Н. О климатическом фоне оледенения Камчатки // Гляциол. исследования. 1985. № 27. С. 51–66.
Каталог ледников СССР: Т. 20. Камчатка. Ч. 2–4 / Под ред. В.Н. Виноградова. Л.: Гидрометеоиздат, 1968. 76 с.
Кондратюк В.И. Климат Камчатки. М.: Гидрометеоиздат. 1974. 201 с.
Кутузов С.С. Изменение площади и объёма ледников хр. Терскей Ала-Тоо во второй половине ХХ в. // Лёд и Снег. 2012. № 1 (117) С. 5–15.
Муравьев А.Я., Носенко Г.А. Изменения оледенения северной части Срединного хребта на Камчатке во второй половине XX в. // Лёд и Снег. 2013. № 2 (122). С. 5–11.
Оледенение Северной и Центральной Евразии в современную эпоху / Под ред. В.М. Котлякова. М.: Наука, 2006. С. 204–210.
Shahgedanova M., Nosenko G., Khromova T., Muraveyev A. Glacier shrinkage and climatic change in the Russian Altai from the mid-20th century: An assessment using remote sensing and PRECIS regional climate model // Journ. of Geophys. Research. 2010. V. 115. D16107. doi:10.1029/2009JD012976
https://ice-snow.igras.ru/jour/article/view/38
doi:10.15356/2076-6734-2014-2-22-28
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/10.15356/2076-6734-2014-2-22-28
https://doi.org/10.15356/2076-6734-2014-2
https://doi.org/10.1029/2009JD012976
container_title Ice and Snow
container_volume 126
container_issue 2
container_start_page 22
_version_ 1766051146270507008
spelling ftjias:oai:oai.ice.elpub.ru:article/38 2023-05-15T16:59:00+02:00 Glacier size changes in Kronotsky Peninsula and Alney-Chashakondzha Massif, Kamchatka Peninsula in the second half of XX century and the beginning of XXI century Изменение размеров ледников Кроноцкого полуострова и массива Алней-Чашаконджа на Камчатке во второй половине XX – начале XXI вв. A. Muravjev Ya. А. Муравьёв Я. 2015-03-26 application/pdf https://ice-snow.igras.ru/jour/article/view/38 https://doi.org/10.15356/2076-6734-2014-2-22-28 rus rus IGRAS https://ice-snow.igras.ru/jour/article/view/38/24 Атлас снежно-ледовых ресурсов мира. М: изд. РАН, 1997. 392 с. Виноградов В.Н., Ходаков В.Г. Баланс льда ледника Корыто в Кроноцком массиве Камчатки // Гляциол. исследования. 1976. № 25. С. 18–26. Глазырин Г.Е., Муравьев Я.Д., Виноградов В.Н. О климатическом фоне оледенения Камчатки // Гляциол. исследования. 1985. № 27. С. 51–66. Каталог ледников СССР: Т. 20. Камчатка. Ч. 2–4 / Под ред. В.Н. Виноградова. Л.: Гидрометеоиздат, 1968. 76 с. Кондратюк В.И. Климат Камчатки. М.: Гидрометеоиздат. 1974. 201 с. Кутузов С.С. Изменение площади и объёма ледников хр. Терскей Ала-Тоо во второй половине ХХ в. // Лёд и Снег. 2012. № 1 (117) С. 5–15. Муравьев А.Я., Носенко Г.А. Изменения оледенения северной части Срединного хребта на Камчатке во второй половине XX в. // Лёд и Снег. 2013. № 2 (122). С. 5–11. Оледенение Северной и Центральной Евразии в современную эпоху / Под ред. В.М. Котлякова. М.: Наука, 2006. С. 204–210. Shahgedanova M., Nosenko G., Khromova T., Muraveyev A. Glacier shrinkage and climatic change in the Russian Altai from the mid-20th century: An assessment using remote sensing and PRECIS regional climate model // Journ. of Geophys. Research. 2010. V. 115. D16107. doi:10.1029/2009JD012976 https://ice-snow.igras.ru/jour/article/view/38 doi:10.15356/2076-6734-2014-2-22-28 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 54, № 2 (2014); 22-28 Лёд и Снег; Том 54, № 2 (2014); 22-28 2412-3765 2076-6734 10.15356/2076-6734-2014-2 Glacier recession;glaciers;Kamchatka;space survey;USSR Glacier Inventory Камчатка;Каталог ледников СССР;космическая съёмка;ледники;сокращение ледников info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2014-2-22-28 https://doi.org/10.15356/2076-6734-2014-2 https://doi.org/10.1029/2009JD012976 2022-12-20T13:29:44Z As it is known from recent investigations 448 glaciers are situated on the Kamchatka Peninsula, their total area are about 905 km2 [8]. More than 80% of them are glaciers of the Sredinny Range and the Klyuchevskaya group that is explained by large altitudes of them. Glaciers of the Kronotsky Penisula are less studied since this territory is practically not influenced by present-day volcanic processes. This paper presents results of investigation of changes in glaciations of the Kronotsky Peninsula and the mountain mass Alney-Chashakondzha (Fig. 1).The following materials are used: 1) the Landsat satellite picture of September 2nd, 2013; 2) pictures from satellite WorldView-2 of July 20th, 2010, and of August 1st, 2012 with spatial resolution of about 1 m; 3) aerial photographs made in August of 1950; 4) topographic maps of the 1:100 000 scale; 5) data from the USSR Glacier Inventory; 6) results of observations at hydrometeorological stations (HMS) Klyuchi and Kronoki (1950–2006) (www.meteo.ru).According to data from the USSR Glacier Inventory 32 glaciers were situated on the Kronotsky Peninsula, their total area 91.9 km2. By 2013, six glaciers disintegrated. Deciphering of the Landsat pictures did show 50 glaciers. Among them 23 glaciers are presented in the Inventory and they still hold their wholeness; 13 glaciers are segments of six disintegrated ones; 14 glaciers found in the pictures are not presented in the Inventory. Changes in areas of the Kronotsky Peninsula glaciers for period 1950–2013 in dependence on their sizes and expositions are shown in Tables 1 and 2.According to the Inventory 26 glaciers were situated in region of the Alney-Chashakondzha massif, their total area 61.4 km2. By 2010, four of them disintegrated. Deciphering of the World-View-2 picture of July 2010 did show 45 glaciers: 20 glaciers are consistent with the Inventory, and they hold their wholeness; 9 glaciers are segments of four disintegrated ones; 16 glaciers found in the pictures are not presented in the Inventory. Changes in ... Article in Journal/Newspaper Kamchatka Kamchatka Peninsula КАМЧАТК* Ice and Snow (E-Journal) Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Klyuchi ENVELOPE(160.805,160.805,56.310,56.310) Kronoki ENVELOPE(161.148,161.148,54.592,54.592) Ice and Snow 126 2 22