Comparison of Hydrothermal Structure of Two Glaciers in Spitsbergen and Tian Shan Based on Radio-Echo Sounding Data
This article considers the features of the thickness distribution of cold and temperate ice and water in polythermal glaciers on Spitsbergen (Nordenskiöld Land) and Tian Shan (Zailiiskii Alatau) according to the data of ground-based radar measurements at a frequency of 20 MHz, which were performed,...
Gespeichert in:
| Veröffentlicht in: | Water resources 2022-12, Vol.49 (Suppl 1), p.S69-S79 |
|---|---|
| Hauptverfasser: | , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | S79 |
|---|---|
| container_issue | Suppl 1 |
| container_start_page | S69 |
| container_title | Water resources |
| container_volume | 49 |
| creator | Macheret, Yu. Ya Glazovsky, A. F. Vasilenko, E. V. Lavrentiev, I. I. Matskovsky, V. V. |
| description | This article considers the features of the thickness distribution of cold and temperate ice and water in polythermal glaciers on Spitsbergen (Nordenskiöld Land) and Tian Shan (Zailiiskii Alatau) according to the data of ground-based radar measurements at a frequency of 20 MHz, which were performed, respectively, in spring 2010 and 2019, and in summer 2013. According to the delay time and intensity of reflections from the cold-temperate ice interface from the temperate ice layer and from the bed, the thickness and volume of cold and temperate ice are determined, the water content in temperate ice is estimated, and the relationship of these characteristics with the structural features and regime of the glaciers in spring and summer before and after the beginning of melting is shown. |
| doi_str_mv | 10.1134/S0097807822070107 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2770321832</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2770321832</sourcerecordid><originalsourceid>FETCH-LOGICAL-c198t-f74752058c77844ee7debe1e3075a29d191423a10f6e4bcd4d5f7ba0c2aef4743</originalsourceid><addsrcrecordid>eNp1kEFLAzEQhYMoWKs_wFvA82qSTZvsUWttBUFwK3hbsslsm9Ima7KL9N-bpYIH8TID8773Bh5C15TcUprzu5KQQkgiJGNEEErECRrRKZFZzvnHKRoNcjbo5-gixi1JCJHFCMWZ37cq2Ogd9g1eHkzw3QbCXu1w2YVed32AQVl9ebzYKW0hRGwdLlvbxRrCGhxWzuCVVem4SeNBRTA45b0pY3021xuPS987Y90aP6pOXaKzRu0iXP3sMXp_mq9my-zldfE8u3_JNC1klzWCiwkjE6mFkJwDCAM1UMiJmChWGFpQznJFSTMFXmvDzaQRtSKaKWi44PkY3Rxz2-A_e4hdtfV9cOllxYQgOaMyZ4miR0oHH2OApmqD3atwqCiphm6rP90mDzt6YmLdGsJv8v-mb_uPezk</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2770321832</pqid></control><display><type>article</type><title>Comparison of Hydrothermal Structure of Two Glaciers in Spitsbergen and Tian Shan Based on Radio-Echo Sounding Data</title><source>SpringerLink Journals - AutoHoldings</source><creator>Macheret, Yu. Ya ; Glazovsky, A. F. ; Vasilenko, E. V. ; Lavrentiev, I. I. ; Matskovsky, V. V.</creator><creatorcontrib>Macheret, Yu. Ya ; Glazovsky, A. F. ; Vasilenko, E. V. ; Lavrentiev, I. I. ; Matskovsky, V. V.</creatorcontrib><description>This article considers the features of the thickness distribution of cold and temperate ice and water in polythermal glaciers on Spitsbergen (Nordenskiöld Land) and Tian Shan (Zailiiskii Alatau) according to the data of ground-based radar measurements at a frequency of 20 MHz, which were performed, respectively, in spring 2010 and 2019, and in summer 2013. According to the delay time and intensity of reflections from the cold-temperate ice interface from the temperate ice layer and from the bed, the thickness and volume of cold and temperate ice are determined, the water content in temperate ice is estimated, and the relationship of these characteristics with the structural features and regime of the glaciers in spring and summer before and after the beginning of melting is shown.</description><identifier>ISSN: 0097-8078</identifier><identifier>EISSN: 1608-344X</identifier><identifier>DOI: 10.1134/S0097807822070107</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Aquatic Pollution ; Delay time ; Earth and Environmental Science ; Earth Sciences ; Echo sounding ; Echoes ; Glaciers ; Glaсiers and Ice Sheets ; Hydrogeology ; Hydrology/Water Resources ; Ice ; Moisture content ; Radar ; Radar data ; Radar measurement ; Spring ; Summer ; Thickness ; Waste Water Technology ; Water content ; Water Management ; Water Pollution Control</subject><ispartof>Water resources, 2022-12, Vol.49 (Suppl 1), p.S69-S79</ispartof><rights>Pleiades Publishing, Ltd. 2022. ISSN 0097-8078, Water Resources, 2022, Vol. 49, Suppl. 1, pp. S69–S79. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2021, published in Led i Sneg, 2021, Vol. 61, No. 2, pp. 165–178.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c198t-f74752058c77844ee7debe1e3075a29d191423a10f6e4bcd4d5f7ba0c2aef4743</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0097807822070107$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0097807822070107$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Macheret, Yu. Ya</creatorcontrib><creatorcontrib>Glazovsky, A. F.</creatorcontrib><creatorcontrib>Vasilenko, E. V.</creatorcontrib><creatorcontrib>Lavrentiev, I. I.</creatorcontrib><creatorcontrib>Matskovsky, V. V.</creatorcontrib><title>Comparison of Hydrothermal Structure of Two Glaciers in Spitsbergen and Tian Shan Based on Radio-Echo Sounding Data</title><title>Water resources</title><addtitle>Water Resour</addtitle><description>This article considers the features of the thickness distribution of cold and temperate ice and water in polythermal glaciers on Spitsbergen (Nordenskiöld Land) and Tian Shan (Zailiiskii Alatau) according to the data of ground-based radar measurements at a frequency of 20 MHz, which were performed, respectively, in spring 2010 and 2019, and in summer 2013. According to the delay time and intensity of reflections from the cold-temperate ice interface from the temperate ice layer and from the bed, the thickness and volume of cold and temperate ice are determined, the water content in temperate ice is estimated, and the relationship of these characteristics with the structural features and regime of the glaciers in spring and summer before and after the beginning of melting is shown.</description><subject>Aquatic Pollution</subject><subject>Delay time</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Echo sounding</subject><subject>Echoes</subject><subject>Glaciers</subject><subject>Glaсiers and Ice Sheets</subject><subject>Hydrogeology</subject><subject>Hydrology/Water Resources</subject><subject>Ice</subject><subject>Moisture content</subject><subject>Radar</subject><subject>Radar data</subject><subject>Radar measurement</subject><subject>Spring</subject><subject>Summer</subject><subject>Thickness</subject><subject>Waste Water Technology</subject><subject>Water content</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><issn>0097-8078</issn><issn>1608-344X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kEFLAzEQhYMoWKs_wFvA82qSTZvsUWttBUFwK3hbsslsm9Ima7KL9N-bpYIH8TID8773Bh5C15TcUprzu5KQQkgiJGNEEErECRrRKZFZzvnHKRoNcjbo5-gixi1JCJHFCMWZ37cq2Ogd9g1eHkzw3QbCXu1w2YVed32AQVl9ebzYKW0hRGwdLlvbxRrCGhxWzuCVVem4SeNBRTA45b0pY3021xuPS987Y90aP6pOXaKzRu0iXP3sMXp_mq9my-zldfE8u3_JNC1klzWCiwkjE6mFkJwDCAM1UMiJmChWGFpQznJFSTMFXmvDzaQRtSKaKWi44PkY3Rxz2-A_e4hdtfV9cOllxYQgOaMyZ4miR0oHH2OApmqD3atwqCiphm6rP90mDzt6YmLdGsJv8v-mb_uPezk</recordid><startdate>20221201</startdate><enddate>20221201</enddate><creator>Macheret, Yu. Ya</creator><creator>Glazovsky, A. F.</creator><creator>Vasilenko, E. V.</creator><creator>Lavrentiev, I. I.</creator><creator>Matskovsky, V. V.</creator><general>Pleiades Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20221201</creationdate><title>Comparison of Hydrothermal Structure of Two Glaciers in Spitsbergen and Tian Shan Based on Radio-Echo Sounding Data</title><author>Macheret, Yu. Ya ; Glazovsky, A. F. ; Vasilenko, E. V. ; Lavrentiev, I. I. ; Matskovsky, V. V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c198t-f74752058c77844ee7debe1e3075a29d191423a10f6e4bcd4d5f7ba0c2aef4743</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Aquatic Pollution</topic><topic>Delay time</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Echo sounding</topic><topic>Echoes</topic><topic>Glaciers</topic><topic>Glaсiers and Ice Sheets</topic><topic>Hydrogeology</topic><topic>Hydrology/Water Resources</topic><topic>Ice</topic><topic>Moisture content</topic><topic>Radar</topic><topic>Radar data</topic><topic>Radar measurement</topic><topic>Spring</topic><topic>Summer</topic><topic>Thickness</topic><topic>Waste Water Technology</topic><topic>Water content</topic><topic>Water Management</topic><topic>Water Pollution Control</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Macheret, Yu. Ya</creatorcontrib><creatorcontrib>Glazovsky, A. F.</creatorcontrib><creatorcontrib>Vasilenko, E. V.</creatorcontrib><creatorcontrib>Lavrentiev, I. I.</creatorcontrib><creatorcontrib>Matskovsky, V. V.</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Water resources</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Macheret, Yu. Ya</au><au>Glazovsky, A. F.</au><au>Vasilenko, E. V.</au><au>Lavrentiev, I. I.</au><au>Matskovsky, V. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Comparison of Hydrothermal Structure of Two Glaciers in Spitsbergen and Tian Shan Based on Radio-Echo Sounding Data</atitle><jtitle>Water resources</jtitle><stitle>Water Resour</stitle><date>2022-12-01</date><risdate>2022</risdate><volume>49</volume><issue>Suppl 1</issue><spage>S69</spage><epage>S79</epage><pages>S69-S79</pages><issn>0097-8078</issn><eissn>1608-344X</eissn><abstract>This article considers the features of the thickness distribution of cold and temperate ice and water in polythermal glaciers on Spitsbergen (Nordenskiöld Land) and Tian Shan (Zailiiskii Alatau) according to the data of ground-based radar measurements at a frequency of 20 MHz, which were performed, respectively, in spring 2010 and 2019, and in summer 2013. According to the delay time and intensity of reflections from the cold-temperate ice interface from the temperate ice layer and from the bed, the thickness and volume of cold and temperate ice are determined, the water content in temperate ice is estimated, and the relationship of these characteristics with the structural features and regime of the glaciers in spring and summer before and after the beginning of melting is shown.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0097807822070107</doi></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0097-8078 |
| ispartof | Water resources, 2022-12, Vol.49 (Suppl 1), p.S69-S79 |
| issn | 0097-8078 1608-344X |
| language | eng |
| recordid | cdi_proquest_journals_2770321832 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Aquatic Pollution Delay time Earth and Environmental Science Earth Sciences Echo sounding Echoes Glaciers Glaсiers and Ice Sheets Hydrogeology Hydrology/Water Resources Ice Moisture content Radar Radar data Radar measurement Spring Summer Thickness Waste Water Technology Water content Water Management Water Pollution Control |
| title | Comparison of Hydrothermal Structure of Two Glaciers in Spitsbergen and Tian Shan Based on Radio-Echo Sounding Data |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-08T09%3A49%3A38IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Comparison%20of%20Hydrothermal%20Structure%20of%20Two%20Glaciers%20in%20Spitsbergen%20and%20Tian%20Shan%20Based%20on%20Radio-Echo%20Sounding%20Data&rft.jtitle=Water%20resources&rft.au=Macheret,%20Yu.%20Ya&rft.date=2022-12-01&rft.volume=49&rft.issue=Suppl%201&rft.spage=S69&rft.epage=S79&rft.pages=S69-S79&rft.issn=0097-8078&rft.eissn=1608-344X&rft_id=info:doi/10.1134/S0097807822070107&rft_dat=%3Cproquest_cross%3E2770321832%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2770321832&rft_id=info:pmid/&rfr_iscdi=true |