Standard

Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation. / Mangerud, Jan; Jakobsson, Martin; Alexanderson, Helena; Astakhov, Valery; Clarke, Garry K.C.; Henriksen, Mona; Hjort, Christian; Krinner, Gerhard; Lunkka, Juha Pekka; Möller, Per; Murray, Andrew; Nikolskaya, Olga; Saarnisto, Matti; Svendsen, John Inge.

In: Quaternary Science Reviews, Vol. 23, No. 11-13, 01.06.2004, p. 1313-1332.

Research output: Contribution to journal › Article › peer-review

Harvard

Mangerud, J, Jakobsson, M, Alexanderson, H, Astakhov, V, Clarke, GKC, Henriksen, M, Hjort, C, Krinner, G, Lunkka, JP, Möller, P, Murray, A, Nikolskaya, O, Saarnisto, M & Svendsen, JI 2004, 'Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation', Quaternary Science Reviews, vol. 23, no. 11-13, pp. 1313-1332. https://doi.org/10.1016/j.quascirev.2003.12.009

APA

Mangerud, J., Jakobsson, M., Alexanderson, H., Astakhov, V., Clarke, G. K. C., Henriksen, M., Hjort, C., Krinner, G., Lunkka, J. P., Möller, P., Murray, A., Nikolskaya, O., Saarnisto, M., & Svendsen, J. I. (2004). Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation. Quaternary Science Reviews, 23(11-13), 1313-1332. https://doi.org/10.1016/j.quascirev.2003.12.009

Vancouver

Mangerud J, Jakobsson M, Alexanderson H, Astakhov V, Clarke GKC, Henriksen M et al. Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation. Quaternary Science Reviews. 2004 Jun 1;23(11-13):1313-1332. https://doi.org/10.1016/j.quascirev.2003.12.009

Author

Mangerud, Jan ; Jakobsson, Martin ; Alexanderson, Helena ; Astakhov, Valery ; Clarke, Garry K.C. ; Henriksen, Mona ; Hjort, Christian ; Krinner, Gerhard ; Lunkka, Juha Pekka ; Möller, Per ; Murray, Andrew ; Nikolskaya, Olga ; Saarnisto, Matti ; Svendsen, John Inge. / Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation. In: Quaternary Science Reviews. 2004 ; Vol. 23, No. 11-13. pp. 1313-1332.

BibTeX

@article{92abfb78e5c94bf483b016901e317416,
title = "Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation",
abstract = "During the Quaternary period, ice sheets centred over the Barents and Kara seas expanded several times onto mainland Russia and blocked northflowing rivers, such as the Yenissei, Ob, Pechora and Mezen. Large ice-dammed lakes with reversed outlets, e.g. toward the Caspian Sea, formed south of these ice sheets. Some lakes are reconstructed from shorelines and lacustrine sediments, others mainly from ice-sheet configuration. Ice-dammed lakes, considerably larger than any lake on Earth today, are reconstructed for the periods 90-80 and 60-50ka. The ages are based on numerous optically stimulated luminescence (OSL) dates. During the global Last Glacial Maximum (LGM, about 20ka) the Barents-Kara Ice Sheet was too small to block these eastern rivers, although in contrast to the 90-80 and 60-50ka maxima, the Scandinavian Ice Sheet grew large enough to divert rivers and meltwater across the drainage divide from the Baltic Basin to the River Volga, and that way to the Caspian Sea. Climate modelling shows that the lakes caused lower summer temperatures on the continent and on the lower parts of the ice sheet. The final drainage of the best mapped lake is modelled, and it is concluded that it probably emptied within few months. We predict that this catastrophic outburst had considerable impact on sea-ice formation in the Arctic Ocean and on the climate of a much larger area.",
author = "Jan Mangerud and Martin Jakobsson and Helena Alexanderson and Valery Astakhov and Clarke, {Garry K.C.} and Mona Henriksen and Christian Hjort and Gerhard Krinner and Lunkka, {Juha Pekka} and Per M{\"o}ller and Andrew Murray and Olga Nikolskaya and Matti Saarnisto and Svendsen, {John Inge}",
year = "2004",
month = jun,
day = "1",
doi = "10.1016/j.quascirev.2003.12.009",
language = "English",
volume = "23",
pages = "1313--1332",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier",
number = "11-13",

}

RIS

TY - JOUR

T1 - Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation

AU - Mangerud, Jan

AU - Jakobsson, Martin

AU - Alexanderson, Helena

AU - Astakhov, Valery

AU - Clarke, Garry K.C.

AU - Henriksen, Mona

AU - Hjort, Christian

AU - Krinner, Gerhard

AU - Lunkka, Juha Pekka

AU - Möller, Per

AU - Murray, Andrew

AU - Nikolskaya, Olga

AU - Saarnisto, Matti

AU - Svendsen, John Inge

PY - 2004/6/1

Y1 - 2004/6/1

N2 - During the Quaternary period, ice sheets centred over the Barents and Kara seas expanded several times onto mainland Russia and blocked northflowing rivers, such as the Yenissei, Ob, Pechora and Mezen. Large ice-dammed lakes with reversed outlets, e.g. toward the Caspian Sea, formed south of these ice sheets. Some lakes are reconstructed from shorelines and lacustrine sediments, others mainly from ice-sheet configuration. Ice-dammed lakes, considerably larger than any lake on Earth today, are reconstructed for the periods 90-80 and 60-50ka. The ages are based on numerous optically stimulated luminescence (OSL) dates. During the global Last Glacial Maximum (LGM, about 20ka) the Barents-Kara Ice Sheet was too small to block these eastern rivers, although in contrast to the 90-80 and 60-50ka maxima, the Scandinavian Ice Sheet grew large enough to divert rivers and meltwater across the drainage divide from the Baltic Basin to the River Volga, and that way to the Caspian Sea. Climate modelling shows that the lakes caused lower summer temperatures on the continent and on the lower parts of the ice sheet. The final drainage of the best mapped lake is modelled, and it is concluded that it probably emptied within few months. We predict that this catastrophic outburst had considerable impact on sea-ice formation in the Arctic Ocean and on the climate of a much larger area.

AB - During the Quaternary period, ice sheets centred over the Barents and Kara seas expanded several times onto mainland Russia and blocked northflowing rivers, such as the Yenissei, Ob, Pechora and Mezen. Large ice-dammed lakes with reversed outlets, e.g. toward the Caspian Sea, formed south of these ice sheets. Some lakes are reconstructed from shorelines and lacustrine sediments, others mainly from ice-sheet configuration. Ice-dammed lakes, considerably larger than any lake on Earth today, are reconstructed for the periods 90-80 and 60-50ka. The ages are based on numerous optically stimulated luminescence (OSL) dates. During the global Last Glacial Maximum (LGM, about 20ka) the Barents-Kara Ice Sheet was too small to block these eastern rivers, although in contrast to the 90-80 and 60-50ka maxima, the Scandinavian Ice Sheet grew large enough to divert rivers and meltwater across the drainage divide from the Baltic Basin to the River Volga, and that way to the Caspian Sea. Climate modelling shows that the lakes caused lower summer temperatures on the continent and on the lower parts of the ice sheet. The final drainage of the best mapped lake is modelled, and it is concluded that it probably emptied within few months. We predict that this catastrophic outburst had considerable impact on sea-ice formation in the Arctic Ocean and on the climate of a much larger area.

UR - http://www.scopus.com/inward/record.url?scp=2642557360&partnerID=8YFLogxK

U2 - 10.1016/j.quascirev.2003.12.009

DO - 10.1016/j.quascirev.2003.12.009

M3 - Article

AN - SCOPUS:2642557360

VL - 23

SP - 1313

EP - 1332

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

IS - 11-13

ER -

ID: 50790720