Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions

The lakes of the Arctic lowlands are both the unique indicator and the result of climatic and permafrost changes. Remote sensing methods and field measurements were used to consider the patterns and features of the morphometric indicators dynamics of the Anadyr lowland lakes over 65 years. We analyz...

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Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Authors: Оleg Tregubov D., Vladimir Glotov E., Pavel Konstantinov Ya., Vladimir Shamov V.
Format: Article in Journal/Newspaper
Language:English
Published: Russian Geographical Society 2021
Subjects:
Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
Anadyr
Anadyr’
Arctic
Anadyr'
permafrost
Permafrost and Periglacial Processes
Polar Geography
The Cryosphere
Thermokarst
Online Access:https://ges.rgo.ru/jour/article/view/2178
https://doi.org/10.24057/2071-9388-2021-030
id ftjges:oai:oai.gesj.elpub.ru:article/2178
record_format openpolar
institution Open Polar
collection Geography, Environment, Sustainability (E-Journal)
op_collection_id ftjges
language English
topic Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
spellingShingle Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
Оleg Tregubov D.
Vladimir Glotov E.
Pavel Konstantinov Ya.
Vladimir Shamov V.
Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
topic_facet Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
description The lakes of the Arctic lowlands are both the unique indicator and the result of climatic and permafrost changes. Remote sensing methods and field measurements were used to consider the patterns and features of the morphometric indicators dynamics of the Anadyr lowland lakes over 65 years. We analyzed the parameters of 36 lakes with an area of 0.02–0.3 km2 located in the bottoms of drained lake basins, in river floodplains, on sea-shore terraces. Field studies were conducted on 22 typical lakes. The considered dynamics of seasonal thawing are based on the monitoring of the active layer for 1994–2020. Due to an increase of mean annual air temperature by 1.8 °C, as well as an increase and then a decrease in the mean annual precipitation by 135 mm, the average share of a lake area in the study area decreased by 24%. It is shown for the first time that cryogenic processes of the lacustrine coastal zone affect the change in the area of lakes simultaneously with the influence of precipitation and air temperature. Based on field observations, we considered two causes of natural drainage: discharge of the lakes through newly formed thermokarst and thermoerosional surface flow channels and decrease in suprapermafrost groundwater recharge as a result of changing depth of seasonally thawed active layer in the coastal zone.
format Article in Journal/Newspaper
author Оleg Tregubov D.
Vladimir Glotov E.
Pavel Konstantinov Ya.
Vladimir Shamov V.
author_facet Оleg Tregubov D.
Vladimir Glotov E.
Pavel Konstantinov Ya.
Vladimir Shamov V.
author_sort Оleg Tregubov D.
title Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
title_short Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
title_full Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
title_fullStr Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
title_full_unstemmed Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions
title_sort hydrological conditions of drained lake basins of the anadyr lowland under changing climatic conditions
publisher Russian Geographical Society
publishDate 2021
url https://ges.rgo.ru/jour/article/view/2178
https://doi.org/10.24057/2071-9388-2021-030
long_lat ENVELOPE(177.510,177.510,64.734,64.734)
ENVELOPE(176.233,176.233,64.882,64.882)
geographic Anadyr
Anadyr’
Arctic
geographic_facet Anadyr
Anadyr’
Arctic
genre Anadyr
Anadyr'
Arctic
Arctic
permafrost
Permafrost and Periglacial Processes
Polar Geography
The Cryosphere
Thermokarst
genre_facet Anadyr
Anadyr'
Arctic
Arctic
permafrost
Permafrost and Periglacial Processes
Polar Geography
The Cryosphere
Thermokarst
op_source GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY; Vol 14, No 4 (2021); 41-54
2542-1565
2071-9388
op_relation https://ges.rgo.ru/jour/article/view/2178/583
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Andresen C.G. and Lougheed V.L. (2015). Disappearing of Arctic tundra ponds: Fine-scale analysis of surface hydrology in drained thaw lake basins over a 65-year period (1948–2013) // J. Geophys. Res. Biogeosci, 120, 466-479, DOI:10.1002/2014JG002778.
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op_doi https://doi.org/10.24057/2071-9388-2021-030
https://doi.org/10.1002/2014JG002778
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spelling ftjges:oai:oai.gesj.elpub.ru:article/2178 2023-05-15T13:24:33+02:00 Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions Оleg Tregubov D. Vladimir Glotov E. Pavel Konstantinov Ya. Vladimir Shamov V. 2021-12-28 application/pdf https://ges.rgo.ru/jour/article/view/2178 https://doi.org/10.24057/2071-9388-2021-030 eng eng Russian Geographical Society https://ges.rgo.ru/jour/article/view/2178/583 Abramov A., Davydov S., Ivashchenko A., Karelin D., Kholodov A., Kraev G., Lupachev A., Maslakov A., Ostroumov V., Rivkina E., Shmelev D., Sorokovikov V., Tregubov O., Veremeeva A., Zamolodchikov D., Zimov S. (2019). Two decades of active layer thickness monitoring in northeastern Asia // Polar Geography, 42(3), 1-17. Andresen C.G. and Lougheed V.L. (2015). Disappearing of Arctic tundra ponds: Fine-scale analysis of surface hydrology in drained thaw lake basins over a 65-year period (1948–2013) // J. Geophys. Res. Biogeosci, 120, 466-479, DOI:10.1002/2014JG002778. Arp C.D., Jones B.M., Liljedahl A.K., Hinkel K.M., and Welker J.A. (2015). Depth, ice thickness, and ice-out timing cause divergent hydrologic responses among Arctic lakes // Water Resources, 51, 9379–9401, DOI:10.1002/2015WR017362. Boike J., Grau T., Heim B., Günther F. et al. (2016). Satellite-derived changes in the permafrost landscapes of Central Yakutia, 2000–2011: Wetting, drying, and fires // Global Planet. Change, 139, 116–127, DOI:10.1016/j.gloplacha.2016.01.001. Bryksina N.A., Polishchuk Yu.M. (2015). Analysis of changes in the number of thermokarst lakes in the permafrost zone of Western Siberia based on satellite images // Cryosphere of the Earth, XIX(2), 114-120.[Bryksina N.A., Polishchuk Yu.M. Analiz izmeneniya chislennosti termokarstovykh ozer v zone mnogoletney merzloty Zapadnoy Sibiri na osnove kosmicheskikh snimkov // Kriosfera Zemli. 2015. T. XIX. № 2. C. 114–120.] Chen M., Rowland J.C., Wilson C.J. et al. (2013). The importance of natural variability in lake areas on the detection of permafrost degradation: a case study in the Yukon Flats, Alaska // Permafrost and Periglacial Processes, 24, 224-240, DOI:10.1002/ppp.1783. Chukotka: Natural-economic essay (1996). Moscow: «Art-Litex», 370. Chukotka: Prirodno-ekonomicheskiy ocherk (1996). Moscow: «Art-Litex», 370. Dneprovskaya V.P., Bryksina N.A., Polishchuk Yu.M. (2009). Izucheniye izmeneniy termokarsta v zone preryvistogo rasprostraneniya vechnoy merzloty Zapadnoy Sibiri na osnove kosmicheskikh snimkov // Issledovaniye zemli iz kosmosa, 4, 1-9. Dneprovskaya V.P., Bryksina N.A., Polishchuk Yu.M. (2009). Study of changes in thermokarst in the zone of discontinuous distribution of permafrost in Western Siberia on the basis of satellite images // Earth research from space, 4, 1-9. General Permafrost Science (1978). / Ed. by V.A. Kudryavtseva. – M.: Publishing house of Moscow University, 464. Geofizika i antropogennyye izmeneniya landshaftov Chukotki (1987). / I.V. Ignatenko, I.M. Papernov, B.A. Pavlov, M.N. Zamoshch, I.N. Skorodumov. Moscow: Nauka, 271. Geophysics and anthropogenic changes in the landscapes of Chukotka (1987). I.V. Ignatenko, I.M. Papernov, B.A. Pavlov, M.N. Zamoshch, I.N. Skorodumov. Moscow: Nauka, 271. Hinkel K.M., Frohn R.C., Nelson F.E., Eisner W.R., and Beck R.A. (2005). Morphometric and spatial analysis of thaw lakes and drained thaw lake basins in the western Arctic coastal plain, Alaska // Permafrost and Periglacial Processes, 16(4), 327-341. Jones B.M., and Arp C.D. (2015). Observing a Catastrophic Thermokarst Lake Drainage in Northern Alaska // Permafrost and Periglac. Process, 26, 119-128, DOI:10.1002/ppp.1842. Jones B.M., Grosse G., Arp C.D., Jones M.C., Anthony K.W., Romanovsky V.E. (2011). Modern thermokarst lake dynamics in the continuous permafrost zone, Northern Seward Peninsula, Alaska // Journal of Geophysical Research, 116: G00M03, DOI:10.1029/2011JG001666. Kapralova V.N. (2014). Regularities of the development of thermokarst processes within the lacustrine-thermokarst plains (based on the approaches of the mathematical morphology of the landscape): dis. . Cand. geological miner. Sciences: 25.00.36. Moscow, 109. Kapralova V.N. (2014). Zakonomernosti razvitiya termokarstovykh protsessov v predelakh ozer-no-termokarstovykh ravnin (na osnove podkhodov matematicheskoy morfologii land-shafta): dis. . kand. geol.-miner. nauk: 25.00.36. Moscow, 109. Kislov A.V., Grebenets V.I., Evstigneev V.M., Konishchev V.N., Sidorova M.V., Surkova G.V., Tumel N.V. (2011). Consequences of possible climate warming in 21st century in the north of Eurasia // Bulletin of Moscow University. Series 5. Geography, 3. 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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 14, No 4 (2021); 41-54 2542-1565 2071-9388 Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftjges https://doi.org/10.24057/2071-9388-2021-030 https://doi.org/10.1002/2014JG002778 https://doi.org/10.1002/2015WR017362 https://doi.org/10.1016/j.gloplacha.2016.01.001 https://doi.org/10.1002/ppp.1783 https://doi.org/10.1002/ppp.1842 https://doi 2022-01-04T17:42:59Z The lakes of the Arctic lowlands are both the unique indicator and the result of climatic and permafrost changes. Remote sensing methods and field measurements were used to consider the patterns and features of the morphometric indicators dynamics of the Anadyr lowland lakes over 65 years. We analyzed the parameters of 36 lakes with an area of 0.02–0.3 km2 located in the bottoms of drained lake basins, in river floodplains, on sea-shore terraces. Field studies were conducted on 22 typical lakes. The considered dynamics of seasonal thawing are based on the monitoring of the active layer for 1994–2020. Due to an increase of mean annual air temperature by 1.8 °C, as well as an increase and then a decrease in the mean annual precipitation by 135 mm, the average share of a lake area in the study area decreased by 24%. It is shown for the first time that cryogenic processes of the lacustrine coastal zone affect the change in the area of lakes simultaneously with the influence of precipitation and air temperature. Based on field observations, we considered two causes of natural drainage: discharge of the lakes through newly formed thermokarst and thermoerosional surface flow channels and decrease in suprapermafrost groundwater recharge as a result of changing depth of seasonally thawed active layer in the coastal zone. Article in Journal/Newspaper Anadyr Anadyr' Arctic Arctic permafrost Permafrost and Periglacial Processes Polar Geography The Cryosphere Thermokarst Geography, Environment, Sustainability (E-Journal) Anadyr ENVELOPE(177.510,177.510,64.734,64.734) Anadyr’ ENVELOPE(176.233,176.233,64.882,64.882) Arctic GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 14 4 41 54

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