Ice ridges in landfast ice of Shokal'skogo Strait

Three first-year ice ridges have been examined with respect to geometry and morphology in landfast ice of Shokal'skogo Strait (Severnaya Zemlya Archipelago) in May 2018. Two of the studied ice ridges were located on the edge of the ridged field and were part of it, because their keels extended...

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Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Author: Victor Kharitonov V.
Format: Article in Journal/Newspaper
Language:English
Published: Russian Geographical Society 2019
Subjects:
ice ridge;water thermal drilling;cross-sectional profile;consolidated layer;porosity
Severnaya Zemlya
Arctic
Polar Research
Online Access:https://ges.rgo.ru/jour/article/view/819
https://doi.org/10.24057/2071-9388-2019-43
id ftjges:oai:oai.gesj.elpub.ru:article/819
record_format openpolar
institution Open Polar
collection Geography, Environment, Sustainability (E-Journal)
op_collection_id ftjges
language English
topic ice ridge;water thermal drilling;cross-sectional profile;consolidated layer;porosity
spellingShingle ice ridge;water thermal drilling;cross-sectional profile;consolidated layer;porosity
Victor Kharitonov V.
Ice ridges in landfast ice of Shokal'skogo Strait
topic_facet ice ridge;water thermal drilling;cross-sectional profile;consolidated layer;porosity
description Three first-year ice ridges have been examined with respect to geometry and morphology in landfast ice of Shokal'skogo Strait (Severnaya Zemlya Archipelago) in May 2018. Two of the studied ice ridges were located on the edge of the ridged field and were part of it, because their keels extended for a long distance deep into this field. Ice ridges characteristics are discussed in the paper. These studies were conducted using hot water thermal drilling with computer recording of the penetration rate. Boreholes were drilled along the cross-section of the ridge crest at 0.25 m intervals. Cross-sectional profiles of ice ridges are illustrated. The maximal sail height varied from 2.9 up to 3.2 m, the maximal keel depth varied from 8.5 up to 9.6 m. The average keel depth to sail height ratio varied from 2.8 to 3.3, and the thickness of the consolidated layer was 2.5-3.5 m. The porosity of the non-consolidated part of the keel was about 23-27%. The distributions of porosity versus depth for all ice ridges are presented.
format Article in Journal/Newspaper
author Victor Kharitonov V.
author_facet Victor Kharitonov V.
author_sort Victor Kharitonov V.
title Ice ridges in landfast ice of Shokal'skogo Strait
title_short Ice ridges in landfast ice of Shokal'skogo Strait
title_full Ice ridges in landfast ice of Shokal'skogo Strait
title_fullStr Ice ridges in landfast ice of Shokal'skogo Strait
title_full_unstemmed Ice ridges in landfast ice of Shokal'skogo Strait
title_sort ice ridges in landfast ice of shokal'skogo strait
publisher Russian Geographical Society
publishDate 2019
url https://ges.rgo.ru/jour/article/view/819
https://doi.org/10.24057/2071-9388-2019-43
long_lat ENVELOPE(98.000,98.000,79.500,79.500)
geographic Severnaya Zemlya
geographic_facet Severnaya Zemlya
genre Arctic
Polar Research
Severnaya Zemlya
genre_facet Arctic
Polar Research
Severnaya Zemlya
op_source GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 12, No 3 (2019); 16-26
2542-1565
2071-9388
op_relation https://ges.rgo.ru/jour/article/view/819/390
Beketsky S.P. & Truskov P.A. (1995). Internal Structure of Ice pressure ridges in the sea of Okhotsk. Proc. of the 13th Int. Conference on Port and Ocean Engineering under Arctic Conditions. August 15-18, 1995. Murmansk, Russia, V. 1, pp. 109-111.
Bonath V., Petrich C., Sand B., Fransson L., Cwirzen A. (2018). Morphology, internal structure and formation of ice ridges in the sea around Svalbard. Cold Regions Science and Technology V. 155, pp. 263-279.
Bonnemaire B., Høyland K.V., Liferov P. & Moslet P.O. (2003). An ice ridge in the Barents Sea, part I: morphology and physical parameters in-situ. Proc. of the 17th Int. Conf. on Port and Ocean Engineering under Arctic Conditions. June 16-19 2003, Trondheim, Norway.
Borodkin V.A, Paramzin A.S., Khotchenkov S.V. (2018). Joint application of a multirotor unmanned aerial vehicle and a scanning sonar to create a three-dimensional digital model of the ice feature relief. Rossiiskie poliarnye issledovaniia. Russian polar research. 2018, 4: 31-35 [In Russian]. http://www.aari.ru/misc/publicat/sources/34/RPR-34el_l_30-34.pdf
Ervik Å., Høyland K.V., Shestov A., Nord T.S. (2018). On the decay of first-year ice ridges: Measurements and evolution of rubble macroporosity, ridge drilling resistance and consolidated layer strength. Cold Regions Science and Technology, V. 151, July 2018, pp. 196-207.
Grishchenko V.D. (1988). Morphometric characteristics of ice ridges at Arctic basin. Proc. of AARI. V. 401, pp. 46-55 (in Russian with English summary).
Høyland Knut V. (2007). Consolidation of first-year sea ice ridges. Journal of Geophysical Research. 107 (C6, 10.1029/2000JC000526). 15,1-15,15. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2000JC000526
Høyland K.V. (2007). Morphology and small-scale strength of ridges in the North-western Barents Sea. Cold Regions Science and Technology, 48, pp. 169-187.
Knut V. Høyland & Sveinung Løset. (1999). Experiments and preliminary simulations of the consolidation of a first-year sea ice Ridge. Proc. of the 15th Int. Conf. on Port and Ocean Engineering under Arctic Condition, POAC`99, 1999. Vol. 1, p.49-59.
ISO19906 (2010). Petroleum and Natural Gas Industries — Arctic Offshore Structures (2010).
Kharitonov V.V. & Morev V.A. (2011). Method of investigation of internal structure of ice hummocks and stamukhas using the thermal drilling technique. Russian Meteorology and Hydrology. V. 36. No. 7: 460-466. http://mig-journal.ru/archive?id=574.
Mironov Y.U., Morev V.А., Porubayev V.S. & Kharitonov V.V. (2003). Study of geometry and internal structure of ice ridges and stamukhas using thermal water drilling. Proc. of the 17th Int. Conf. on Port and Ocean Engineering under Arctic Conditions POAC'03. Trondheim, Norway, June 16-19 2003, V. 2, pp. 623-632.
Mironov Ye.U. & Porubaev V.S. (2012). Formation of ice ridges in the coastal part of the Kara sea and their morphometric characteristics. Sovremennye problemy nauki i obrazovaniia. Modern problems of science and education. No. 4. URL: http://science-education.ru/ru/article/view?id=6707 (accessed: 05.07.2018).
Mironov Ye.U. & Porubaev V.S. (2005). Structural peculiarities of ice features of the offshore of the Caspian Sea, the Sea of Okhotsk and the Pechora Sea. Proc. of the 18th Int. Conf. on Port and Ocean Eng. under Arctic Conditions (POAC). Potsdam, New York, 26-30 June 2005, Vol. 2, pp. 483-492.
Morev V.A., Morev A.V. & Kharitonov V.V. (2000). Method of determination of ice ridge and stamukha structure, ice features and boundaries of ice and ground. License of Russia № 2153070, Bulletin of inventions № 20 (in Russian).
Pavlov V.A., Kornishin K.A., Efimov Ya.O., Mironov Ye.U. et al. (2016). Peculiarities of consolidated layer growth of the Kara and Laptev Sea ice ridges. Neftyanoe khozyaystvo (Oil industry), No. 11, pp. 49-54 (in Russian with English summary).
Strub-Klein L. & Sudom D. (2012). A comprehensive analysis of the morphology of first-year sea ice ridges. Cold Regions Science and Technology. V. 82, pp. 94–109.
Sudom D. & Timco G. (2013). Knowledge gaps in sea ice ridge properties. Proc. of the 22nd Int. Conf. on Port and Ocean Engineering under Arctic Conditions (POAC). June 9-13, 2013. Espoo, Finland.
Surkov G.A. (2001). Internal structure of first-year hummocks. Proc. of ISOPE, Stavanger, Norway, June 17-22, 2001.
Surkov G.A. (2001). Thickness of the consolidated layer in first-year hummocks. Proc. 16th Int. Conf. on Port and Ocean Engineering under Arctic Conditions. Ottawa, Ontario, Canada. August 12-17, 2001, pp. 245–252.
Tyshko K.P. & Kharitonov V.V. (2011). Some features of one-year ice hummock formation at multiple ice field motions. Russian Meteorology and Hydrology. No. 10, pp. 53-57.
https://ges.rgo.ru/jour/article/view/819
doi:10.24057/2071-9388-2019-43
op_rights Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal the 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 can 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 acknowledgment 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).The information and opinions presented in the Journal reflect the views of the authors and not of the Journal or its Editorial Board or the Publisher. The GES Journal has used its best endeavors to ensure that the information is correct and current at the time of publication but takes no responsibility for any error, omission, or defect therein.
Авторы, публикующие в данном журнале, соглашаются со следующим:Авторы сохраняют за собой авторские права на работу и предоставляют журналу право первой публикации работы на условиях лицензии Creative Commons Attribution License, которая позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Авторы сохраняют право заключать отдельные контрактные договорённости, касающиеся не-эксклюзивного распространения версии работы в опубликованном здесь виде (например, размещение ее в институтском хранилище, публикацию в книге), со ссылкой на ее оригинальную публикацию в этом журнале.Авторы имеют право размещать их работу
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op_doi https://doi.org/10.24057/2071-9388-2019-43
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spelling ftjges:oai:oai.gesj.elpub.ru:article/819 2023-05-15T14:27:22+02:00 Ice ridges in landfast ice of Shokal'skogo Strait Victor Kharitonov V. 2019-10-03 application/pdf https://ges.rgo.ru/jour/article/view/819 https://doi.org/10.24057/2071-9388-2019-43 eng eng Russian Geographical Society https://ges.rgo.ru/jour/article/view/819/390 Beketsky S.P. & Truskov P.A. (1995). Internal Structure of Ice pressure ridges in the sea of Okhotsk. Proc. of the 13th Int. Conference on Port and Ocean Engineering under Arctic Conditions. August 15-18, 1995. Murmansk, Russia, V. 1, pp. 109-111. Bonath V., Petrich C., Sand B., Fransson L., Cwirzen A. (2018). Morphology, internal structure and formation of ice ridges in the sea around Svalbard. Cold Regions Science and Technology V. 155, pp. 263-279. Bonnemaire B., Høyland K.V., Liferov P. & Moslet P.O. (2003). An ice ridge in the Barents Sea, part I: morphology and physical parameters in-situ. Proc. of the 17th Int. Conf. on Port and Ocean Engineering under Arctic Conditions. June 16-19 2003, Trondheim, Norway. Borodkin V.A, Paramzin A.S., Khotchenkov S.V. (2018). Joint application of a multirotor unmanned aerial vehicle and a scanning sonar to create a three-dimensional digital model of the ice feature relief. Rossiiskie poliarnye issledovaniia. Russian polar research. 2018, 4: 31-35 [In Russian]. http://www.aari.ru/misc/publicat/sources/34/RPR-34el_l_30-34.pdf Ervik Å., Høyland K.V., Shestov A., Nord T.S. (2018). On the decay of first-year ice ridges: Measurements and evolution of rubble macroporosity, ridge drilling resistance and consolidated layer strength. Cold Regions Science and Technology, V. 151, July 2018, pp. 196-207. Grishchenko V.D. (1988). Morphometric characteristics of ice ridges at Arctic basin. Proc. of AARI. V. 401, pp. 46-55 (in Russian with English summary). Høyland Knut V. (2007). Consolidation of first-year sea ice ridges. Journal of Geophysical Research. 107 (C6, 10.1029/2000JC000526). 15,1-15,15. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2000JC000526 Høyland K.V. (2007). Morphology and small-scale strength of ridges in the North-western Barents Sea. Cold Regions Science and Technology, 48, pp. 169-187. Knut V. Høyland & Sveinung Løset. (1999). Experiments and preliminary simulations of the consolidation of a first-year sea ice Ridge. Proc. of the 15th Int. Conf. on Port and Ocean Engineering under Arctic Condition, POAC`99, 1999. Vol. 1, p.49-59. ISO19906 (2010). Petroleum and Natural Gas Industries — Arctic Offshore Structures (2010). Kharitonov V.V. & Morev V.A. (2011). Method of investigation of internal structure of ice hummocks and stamukhas using the thermal drilling technique. Russian Meteorology and Hydrology. V. 36. No. 7: 460-466. http://mig-journal.ru/archive?id=574. Mironov Y.U., Morev V.А., Porubayev V.S. & Kharitonov V.V. (2003). Study of geometry and internal structure of ice ridges and stamukhas using thermal water drilling. Proc. of the 17th Int. Conf. on Port and Ocean Engineering under Arctic Conditions POAC'03. Trondheim, Norway, June 16-19 2003, V. 2, pp. 623-632. Mironov Ye.U. & Porubaev V.S. (2012). Formation of ice ridges in the coastal part of the Kara sea and their morphometric characteristics. Sovremennye problemy nauki i obrazovaniia. Modern problems of science and education. No. 4. URL: http://science-education.ru/ru/article/view?id=6707 (accessed: 05.07.2018). Mironov Ye.U. & Porubaev V.S. (2005). Structural peculiarities of ice features of the offshore of the Caspian Sea, the Sea of Okhotsk and the Pechora Sea. Proc. of the 18th Int. Conf. on Port and Ocean Eng. under Arctic Conditions (POAC). Potsdam, New York, 26-30 June 2005, Vol. 2, pp. 483-492. Morev V.A., Morev A.V. & Kharitonov V.V. (2000). Method of determination of ice ridge and stamukha structure, ice features and boundaries of ice and ground. License of Russia № 2153070, Bulletin of inventions № 20 (in Russian). Pavlov V.A., Kornishin K.A., Efimov Ya.O., Mironov Ye.U. et al. (2016). Peculiarities of consolidated layer growth of the Kara and Laptev Sea ice ridges. Neftyanoe khozyaystvo (Oil industry), No. 11, pp. 49-54 (in Russian with English summary). Strub-Klein L. & Sudom D. (2012). A comprehensive analysis of the morphology of first-year sea ice ridges. Cold Regions Science and Technology. V. 82, pp. 94–109. Sudom D. & Timco G. (2013). Knowledge gaps in sea ice ridge properties. Proc. of the 22nd Int. Conf. on Port and Ocean Engineering under Arctic Conditions (POAC). June 9-13, 2013. Espoo, Finland. Surkov G.A. (2001). Internal structure of first-year hummocks. Proc. of ISOPE, Stavanger, Norway, June 17-22, 2001. Surkov G.A. (2001). Thickness of the consolidated layer in first-year hummocks. Proc. 16th Int. Conf. on Port and Ocean Engineering under Arctic Conditions. Ottawa, Ontario, Canada. August 12-17, 2001, pp. 245–252. Tyshko K.P. & Kharitonov V.V. (2011). Some features of one-year ice hummock formation at multiple ice field motions. Russian Meteorology and Hydrology. No. 10, pp. 53-57. https://ges.rgo.ru/jour/article/view/819 doi:10.24057/2071-9388-2019-43 Authors who publish with this journal agree to the following terms:Authors retain copyright and grant the journal the 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 can 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 acknowledgment 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).The information and opinions presented in the Journal reflect the views of the authors and not of the Journal or its Editorial Board or the Publisher. The GES Journal has used its best endeavors to ensure that the information is correct and current at the time of publication but takes no responsibility for any error, omission, or defect therein. Авторы, публикующие в данном журнале, соглашаются со следующим:Авторы сохраняют за собой авторские права на работу и предоставляют журналу право первой публикации работы на условиях лицензии Creative Commons Attribution License, которая позволяет другим распространять данную работу с обязательным сохранением ссылок на авторов оригинальной работы и оригинальную публикацию в этом журнале.Авторы сохраняют право заключать отдельные контрактные договорённости, касающиеся не-эксклюзивного распространения версии работы в опубликованном здесь виде (например, размещение ее в институтском хранилище, публикацию в книге), со ссылкой на ее оригинальную публикацию в этом журнале.Авторы имеют право размещать их работу CC-BY GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 12, No 3 (2019); 16-26 2542-1565 2071-9388 ice ridge;water thermal drilling;cross-sectional profile;consolidated layer;porosity info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftjges https://doi.org/10.24057/2071-9388-2019-43 https://doi.org/10.1029/2000JC000526). 2021-05-21T07:34:36Z Three first-year ice ridges have been examined with respect to geometry and morphology in landfast ice of Shokal'skogo Strait (Severnaya Zemlya Archipelago) in May 2018. Two of the studied ice ridges were located on the edge of the ridged field and were part of it, because their keels extended for a long distance deep into this field. Ice ridges characteristics are discussed in the paper. These studies were conducted using hot water thermal drilling with computer recording of the penetration rate. Boreholes were drilled along the cross-section of the ridge crest at 0.25 m intervals. Cross-sectional profiles of ice ridges are illustrated. The maximal sail height varied from 2.9 up to 3.2 m, the maximal keel depth varied from 8.5 up to 9.6 m. The average keel depth to sail height ratio varied from 2.8 to 3.3, and the thickness of the consolidated layer was 2.5-3.5 m. The porosity of the non-consolidated part of the keel was about 23-27%. The distributions of porosity versus depth for all ice ridges are presented. Article in Journal/Newspaper Arctic Polar Research Severnaya Zemlya Geography, Environment, Sustainability (E-Journal) Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 12 3 16 26

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