Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016
In 1967‑2015, Institute of Geography of the USSR/Russian Academy of Sciences together with other organizations carried out field expeditions in different areas of mountain and polar glaciations in many regions: the Polar Urals, Caucasus, Pamir, Zailiysky and Jungar Alatau, Tien‑Shan, Pamir‑Alai, the...
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2016
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Online Access: | https://ice-snow.igras.ru/jour/article/view/344 https://doi.org/10.15356/2076-6734-2016-4-561-574 |
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gravimetry mountain glaciers polar glaciers radio‑echo sounding горные ледники;гравиметрия;полярные ледники;радиозондирование |
spellingShingle |
gravimetry mountain glaciers polar glaciers radio‑echo sounding горные ледники;гравиметрия;полярные ледники;радиозондирование V. Kotlyakov M. Yu. Macheret Ya. В. Котляков М. Ю. Мачерет Я. Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 |
topic_facet |
gravimetry mountain glaciers polar glaciers radio‑echo sounding горные ледники;гравиметрия;полярные ледники;радиозондирование |
description |
In 1967‑2015, Institute of Geography of the USSR/Russian Academy of Sciences together with other organizations carried out field expeditions in different areas of mountain and polar glaciations in many regions: the Polar Urals, Caucasus, Pamir, Zailiysky and Jungar Alatau, Tien‑Shan, Pamir‑Alai, the Kamchatka Peninsula, the Pyrenees, the Arctic – Spitsbergen, Novaya Zemlya, Franz Josef and Severnaya Zemlya, and Antarctica – on the ice flow B, and in the sub‑Antarctic – Islands King George, Galindez, and Livingston. The gravimetric and ground and aerial radar observations were made in these expeditions. About 300 glaciers of different morphological types and sizes with cold, subpolar and temperate thermal regime were studied. Basic results of these studies are the following: (1) the new data on the ice thicknesses, ice volumes, subglacial relief, internal structure, and thermal state of the glaciers were obtained; (2) the two‑layered (polythermal) glaciers consisting of the upper layer of cold ice and the lower layer of temperate water‑filled ice had been revealed in Svalbard for the first time; spatial distribution of cold, polythermal and temperate glaciers had been determined; (3) the evidences were obtained that measured changes in thickness of the upper cold ice layer in polythermal glaciers can be used to estimate the long‑period variations of regional climates and serve as regional paleothermometers; (4) methods for estimating the water content in temperate and polythermal glaciers from the RES data were developed; and its space‑time variations in temperate ices of the Svaldbald glaciers were estimated since even small water content inside of them can noticeably change their dynamic behavior; (5) methods for estimating the ice volume within glaciers in large regions of mountain and polar glaciations had been created; the ice storages were estimated in Svalbard, Franz Josef Land, Dzhungrsky Alatau, the Great Caucasus, and Mt. Elbrus; (6) detailed data on the ice thicknesses and the subglacial relief had ... |
format |
Article in Journal/Newspaper |
author |
V. Kotlyakov M. Yu. Macheret Ya. В. Котляков М. Ю. Мачерет Я. |
author_facet |
V. Kotlyakov M. Yu. Macheret Ya. В. Котляков М. Ю. Мачерет Я. |
author_sort |
V. Kotlyakov M. |
title |
Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 |
title_short |
Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 |
title_full |
Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 |
title_fullStr |
Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 |
title_full_unstemmed |
Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 |
title_sort |
fifty years of geophysical researches of glaciers in institute of geography, the russian academy of sciences, 1966–2016 |
publisher |
IGRAS |
publishDate |
2016 |
url |
https://ice-snow.igras.ru/jour/article/view/344 https://doi.org/10.15356/2076-6734-2016-4-561-574 |
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ENVELOPE(160.000,160.000,56.000,56.000) ENVELOPE(55.000,55.000,81.000,81.000) ENVELOPE(98.000,98.000,79.500,79.500) ENVELOPE(-64.248,-64.248,-65.250,-65.250) |
geographic |
Arctic Antarctic Svalbard Kamchatka Peninsula Franz Josef Land Severnaya Zemlya Galindez |
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Arctic Antarctic Svalbard Kamchatka Peninsula Franz Josef Land Severnaya Zemlya Galindez |
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Antarc* Antarctic Antarctica Arctic Franz Josef Land Kamchatka Kamchatka Peninsula Novaya Zemlya Severnaya Zemlya Svalbard Spitsbergen |
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Antarc* Antarctic Antarctica Arctic Franz Josef Land Kamchatka Kamchatka Peninsula Novaya Zemlya Severnaya Zemlya Svalbard Spitsbergen |
op_source |
Ice and Snow; Том 56, № 4 (2016); 561-574 Лёд и Снег; Том 56, № 4 (2016); 561-574 2412-3765 2076-6734 10.15356/2076-6734-2016-4 |
op_relation |
https://ice-snow.igras.ru/jour/article/view/344/196 Глазовский А.Ф., Мачерет Ю.Я. Вода в ледниках. Методы и результаты геофизических и дистанционных исследований. М.: ГЕОС. 2014. 528 с. Котляков В.М. (ред.) Гляциология Шпицбергена. М.: Наука, 1985. 200 с. Котляков В.М. (ред.) Режим и эволюция полярных ледниковых покровов. СПб.: Гидрометеоиздат, 1992. 232 с. Котляков В.М (ред.) Оледенение Северной и Центральной Евразии в современную эпоху. М.: Наука, 2006. 482 с. Котляков В.М. (ред.) Оледенение Северной Евразии в недавнем прошлом и ближайшем будущем. М.: Наука, 2007. 368 с. Мачерет Ю.Я. Радиозондирование ледников / Ред. В.М. Котляков. М.: Научный мир, 2006. 392 с. Мачерет Ю.Я. Метки на экране. М.: Медиа‑Пресс, 2006. 216 с. Мачерет Ю.Я. Гляциологи на ледниках. М.-СПб.: Нестор‑История, 2015. 144 с. https://ice-snow.igras.ru/jour/article/view/344 doi:10.15356/2076-6734-2016-4-561-574 |
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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). |
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ftjias:oai:oai.ice.elpub.ru:article/344 2023-05-15T13:44:15+02:00 Fifty years of geophysical researches of glaciers in Institute of Geography, the Russian Academy of Sciences, 1966–2016 50 лет геофизических исследований ледников в Институте географии V. Kotlyakov M. Yu. Macheret Ya. В. Котляков М. Ю. Мачерет Я. 2016-12-21 application/pdf https://ice-snow.igras.ru/jour/article/view/344 https://doi.org/10.15356/2076-6734-2016-4-561-574 rus rus IGRAS https://ice-snow.igras.ru/jour/article/view/344/196 Глазовский А.Ф., Мачерет Ю.Я. Вода в ледниках. Методы и результаты геофизических и дистанционных исследований. М.: ГЕОС. 2014. 528 с. Котляков В.М. (ред.) Гляциология Шпицбергена. М.: Наука, 1985. 200 с. Котляков В.М. (ред.) Режим и эволюция полярных ледниковых покровов. СПб.: Гидрометеоиздат, 1992. 232 с. Котляков В.М (ред.) Оледенение Северной и Центральной Евразии в современную эпоху. М.: Наука, 2006. 482 с. Котляков В.М. (ред.) Оледенение Северной Евразии в недавнем прошлом и ближайшем будущем. М.: Наука, 2007. 368 с. Мачерет Ю.Я. Радиозондирование ледников / Ред. В.М. Котляков. М.: Научный мир, 2006. 392 с. Мачерет Ю.Я. Метки на экране. М.: Медиа‑Пресс, 2006. 216 с. Мачерет Ю.Я. Гляциологи на ледниках. М.-СПб.: Нестор‑История, 2015. 144 с. https://ice-snow.igras.ru/jour/article/view/344 doi:10.15356/2076-6734-2016-4-561-574 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 56, № 4 (2016); 561-574 Лёд и Снег; Том 56, № 4 (2016); 561-574 2412-3765 2076-6734 10.15356/2076-6734-2016-4 gravimetry mountain glaciers polar glaciers radio‑echo sounding горные ледники;гравиметрия;полярные ледники;радиозондирование info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftjias https://doi.org/10.15356/2076-6734-2016-4-561-574 https://doi.org/10.15356/2076-6734-2016-4 2022-12-20T13:30:01Z In 1967‑2015, Institute of Geography of the USSR/Russian Academy of Sciences together with other organizations carried out field expeditions in different areas of mountain and polar glaciations in many regions: the Polar Urals, Caucasus, Pamir, Zailiysky and Jungar Alatau, Tien‑Shan, Pamir‑Alai, the Kamchatka Peninsula, the Pyrenees, the Arctic – Spitsbergen, Novaya Zemlya, Franz Josef and Severnaya Zemlya, and Antarctica – on the ice flow B, and in the sub‑Antarctic – Islands King George, Galindez, and Livingston. The gravimetric and ground and aerial radar observations were made in these expeditions. About 300 glaciers of different morphological types and sizes with cold, subpolar and temperate thermal regime were studied. Basic results of these studies are the following: (1) the new data on the ice thicknesses, ice volumes, subglacial relief, internal structure, and thermal state of the glaciers were obtained; (2) the two‑layered (polythermal) glaciers consisting of the upper layer of cold ice and the lower layer of temperate water‑filled ice had been revealed in Svalbard for the first time; spatial distribution of cold, polythermal and temperate glaciers had been determined; (3) the evidences were obtained that measured changes in thickness of the upper cold ice layer in polythermal glaciers can be used to estimate the long‑period variations of regional climates and serve as regional paleothermometers; (4) methods for estimating the water content in temperate and polythermal glaciers from the RES data were developed; and its space‑time variations in temperate ices of the Svaldbald glaciers were estimated since even small water content inside of them can noticeably change their dynamic behavior; (5) methods for estimating the ice volume within glaciers in large regions of mountain and polar glaciations had been created; the ice storages were estimated in Svalbard, Franz Josef Land, Dzhungrsky Alatau, the Great Caucasus, and Mt. Elbrus; (6) detailed data on the ice thicknesses and the subglacial relief had ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Arctic Franz Josef Land Kamchatka Kamchatka Peninsula Novaya Zemlya Severnaya Zemlya Svalbard Spitsbergen Ice and Snow (E-Journal) Arctic Antarctic Svalbard Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) Galindez ENVELOPE(-64.248,-64.248,-65.250,-65.250) Ice and Snow 56 4 561 574 |