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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2021
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Online Access: | https://ges.rgo.ru/jour/article/view/2178 https://doi.org/10.24057/2071-9388-2021-030 |
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ftjges:oai:oai.gesj.elpub.ru:article/2178 |
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Open Polar |
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Geography, Environment, Sustainability (E-Journal) |
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ftjges |
language |
English |
topic |
Hydrological Conditions Of Drained Lake Basins Of The Anadyr Lowland Under Changing Climatic Conditions |
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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 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. [online] URL: https://cyberleninka.ru/article/n/posledstviya-vozmozhnogo-potepleniya-klimata-v-xxi-veke-na-severe-evrazii8 (date of access: 12.07.2021). Kislov A.V., Grebenets V.I., Yevstigneyev V.M., Konishchev V.N., Sidorova M.V., Surkova G.V., Tumel N.V. (2011). Posledstviya vozmozhnogo potepleniya klimata v XXI veke na severe Yevrazii // Vestnik Moskovskogo universiteta. Seriya 5. Geografiya, 3. [online] URL: https://cyberleninka.ru/article/n/posledstviya-vozmozhnogo-potepleniya-klimata-v-xxi-veke-na-severe-evrazii8 (data obrashcheniya: 12.07.2021).] Konischev V.N. (2011). Response of permafrost to climate warming // Cryosphere of the Earth, XV(4), 15-18. Konishchev V.N. (2011). Reaktsiya vechnoy merzloty na potepleniye klimata // Kriosfera Zemli, XV(4), 15-18. Krivoshchekov V.S. (2000). Land reclamation and land development in Chukotka. Magadan: Chukotka branch of SVKNII FEB RAS, 274. Krivoshchekov V.S. (2000). Melioratsiya i osvoyeniye zemel na Chukotke. Magadan: Chukotskiy filial SVKNII DVO RAN, 274. Labrecque S., Lacelle D., Duguay C.R., Lauriol B., Hawkings J. (2009). Contemporary (1951–2001) evolution of lakes in the Old Crow Basin, Northern Yukon, Canada: remote sensing, numerical modeling, and stable isotope analysis // Arctic, 62(2), 225-238. Lantz T., Turner K. (2015). Changes in lake area in response to thermokarst processes and climate in Old Crow Flats, Yukon // J. Geophys. Res. Biogeosci., 120, 513-524, DOI:10.1002/2014JG002744. Luo J., Niu F., Lin. Z., Liu M., Yin G. (2015). Thermokarst lake changes between 1969 and 2010 in the Beilu River Basin, Qinghai–Tibet Plateau, China // Science Bulletin, 60(5), 556-564, DOI:10.1007/s11434-015-0730-2. Lyubomirov A.S. (1990). Chukotka permafrost lakes. Yakutsk: Permafrost Institute of the Siberian Branch of the USSR Academy of Sciences, 176. Lyubomirov A.S. (1990). Ozera kriolitozony Chukotki. Yakutsk: In-t merzlotovedeniya SO AN SSSR, 176. Marsh P., Russell M., Pohl S., Haywood H., Onclin C. (2009). Changes in thaw lake drainage in the Western Canadian Arctic from 1950 to 2000 // Hydrol. Process, 23, 145-158. Nesterova N.V., Makarieva O.M., Fedorov A.N., Shikhov A.N. (2020). 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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. [online] URL: https://cyberleninka.ru/article/n/posledstviya-vozmozhnogo-potepleniya-klimata-v-xxi-veke-na-severe-evrazii8 (date of access: 12.07.2021). Kislov A.V., Grebenets V.I., Yevstigneyev V.M., Konishchev V.N., Sidorova M.V., Surkova G.V., Tumel N.V. (2011). Posledstviya vozmozhnogo potepleniya klimata v XXI veke na severe Yevrazii // Vestnik Moskovskogo universiteta. Seriya 5. Geografiya, 3. [online] URL: https://cyberleninka.ru/article/n/posledstviya-vozmozhnogo-potepleniya-klimata-v-xxi-veke-na-severe-evrazii8 (data obrashcheniya: 12.07.2021).] Konischev V.N. (2011). Response of permafrost to climate warming // Cryosphere of the Earth, XV(4), 15-18. Konishchev V.N. (2011). Reaktsiya vechnoy merzloty na potepleniye klimata // Kriosfera Zemli, XV(4), 15-18. Krivoshchekov V.S. (2000). Land reclamation and land development in Chukotka. Magadan: Chukotka branch of SVKNII FEB RAS, 274. Krivoshchekov V.S. (2000). Melioratsiya i osvoyeniye zemel na Chukotke. Magadan: Chukotskiy filial SVKNII DVO RAN, 274. Labrecque S., Lacelle D., Duguay C.R., Lauriol B., Hawkings J. (2009). Contemporary (1951–2001) evolution of lakes in the Old Crow Basin, Northern Yukon, Canada: remote sensing, numerical modeling, and stable isotope analysis // Arctic, 62(2), 225-238. Lantz T., Turner K. (2015). Changes in lake area in response to thermokarst processes and climate in Old Crow Flats, Yukon // J. Geophys. Res. Biogeosci., 120, 513-524, DOI:10.1002/2014JG002744. Luo J., Niu F., Lin. Z., Liu M., Yin G. (2015). Thermokarst lake changes between 1969 and 2010 in the Beilu River Basin, Qinghai–Tibet Plateau, China // Science Bulletin, 60(5), 556-564, DOI:10.1007/s11434-015-0730-2. Lyubomirov A.S. (1990). Chukotka permafrost lakes. Yakutsk: Permafrost Institute of the Siberian Branch of the USSR Academy of Sciences, 176. Lyubomirov A.S. (1990). Ozera kriolitozony Chukotki. Yakutsk: In-t merzlotovedeniya SO AN SSSR, 176. 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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 |