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Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia. / Mikhalenko, V.; Sokratov, S.; Kutuzov, S.; Ginot, P.; Legrand, M.; Preunkert, S.; Lavrentiev, I.; Kozachek, A.; Ekaykin, A.; Fain, X.; Lim, S.; Schotterer, U.; Lipenkov, V.; Toropov, P.

в: Cryosphere, Том 9, № 6, 2015, стр. 2253-2270.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Mikhalenko, V, Sokratov, S, Kutuzov, S, Ginot, P, Legrand, M, Preunkert, S, Lavrentiev, I, Kozachek, A, Ekaykin, A, Fain, X, Lim, S, Schotterer, U, Lipenkov, V & Toropov, P 2015, 'Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia', Cryosphere, Том. 9, № 6, стр. 2253-2270. https://doi.org/10.5194/tc-9-2253-2015

APA

Mikhalenko, V., Sokratov, S., Kutuzov, S., Ginot, P., Legrand, M., Preunkert, S., Lavrentiev, I., Kozachek, A., Ekaykin, A., Fain, X., Lim, S., Schotterer, U., Lipenkov, V., & Toropov, P. (2015). Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia. Cryosphere, 9(6), 2253-2270. https://doi.org/10.5194/tc-9-2253-2015

Vancouver

Mikhalenko V, Sokratov S, Kutuzov S, Ginot P, Legrand M, Preunkert S и пр. Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia. Cryosphere. 2015;9(6):2253-2270. https://doi.org/10.5194/tc-9-2253-2015

Author

Mikhalenko, V. ; Sokratov, S. ; Kutuzov, S. ; Ginot, P. ; Legrand, M. ; Preunkert, S. ; Lavrentiev, I. ; Kozachek, A. ; Ekaykin, A. ; Fain, X. ; Lim, S. ; Schotterer, U. ; Lipenkov, V. ; Toropov, P. / Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia. в: Cryosphere. 2015 ; Том 9, № 6. стр. 2253-2270.

BibTeX

@article{7262aa01902d41669939688992831854,
title = "Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia",
abstract = "A 182m ice core was recovered from a borehole drilled into bedrock on the western plateau of Mt. Elbrus (43 degrees 20' 53.9 '' N, 42 degrees 25'36.0 '' E; 5115ma.s.l.) in the Caucasus, Russia, in 2009. This is the first ice core in the region that represents a paleoclimate record that is practically undisturbed by seasonal melting. Relatively high snow accumulation rates at the drilling site enabled the analysis of the intraseasonal variability in climate proxies. Borehole temperatures ranged from -17 degrees C at 10m depth to -2.4 degrees C at 182 m. A detailed radio-echo sounding survey showed that the glacier thickness ranged from 45m near the marginal zone of the plateau up to 255m at the glacier center. The ice core has been analyzed for stable isotopes (delta O-18 and delta D), major ions (K+, Na+, Ca2+, Mg2+, NH4+, SO42-, NO3-, Cl-, F-), succinic acid (HOOCCH2COOH), and tritium content. The mean annual net accumulation rate of 1455mmw : e : for the last 140 years was estimated from distinct annual osc",
author = "V. Mikhalenko and S. Sokratov and S. Kutuzov and P. Ginot and M. Legrand and S. Preunkert and I. Lavrentiev and A. Kozachek and A. Ekaykin and X. Fain and S. Lim and U. Schotterer and V. Lipenkov and P. Toropov",
year = "2015",
doi = "10.5194/tc-9-2253-2015",
language = "English",
volume = "9",
pages = "2253--2270",
journal = "Cryosphere",
issn = "1994-0416",
publisher = "Copernicus GmbH ",
number = "6",

}

RIS

TY - JOUR

T1 - Investigation of a deep ice core from the Elbrus western plateau, the Caucasus, Russia

AU - Mikhalenko, V.

AU - Sokratov, S.

AU - Kutuzov, S.

AU - Ginot, P.

AU - Legrand, M.

AU - Preunkert, S.

AU - Lavrentiev, I.

AU - Kozachek, A.

AU - Ekaykin, A.

AU - Fain, X.

AU - Lim, S.

AU - Schotterer, U.

AU - Lipenkov, V.

AU - Toropov, P.

PY - 2015

Y1 - 2015

N2 - A 182m ice core was recovered from a borehole drilled into bedrock on the western plateau of Mt. Elbrus (43 degrees 20' 53.9 '' N, 42 degrees 25'36.0 '' E; 5115ma.s.l.) in the Caucasus, Russia, in 2009. This is the first ice core in the region that represents a paleoclimate record that is practically undisturbed by seasonal melting. Relatively high snow accumulation rates at the drilling site enabled the analysis of the intraseasonal variability in climate proxies. Borehole temperatures ranged from -17 degrees C at 10m depth to -2.4 degrees C at 182 m. A detailed radio-echo sounding survey showed that the glacier thickness ranged from 45m near the marginal zone of the plateau up to 255m at the glacier center. The ice core has been analyzed for stable isotopes (delta O-18 and delta D), major ions (K+, Na+, Ca2+, Mg2+, NH4+, SO42-, NO3-, Cl-, F-), succinic acid (HOOCCH2COOH), and tritium content. The mean annual net accumulation rate of 1455mmw : e : for the last 140 years was estimated from distinct annual osc

AB - A 182m ice core was recovered from a borehole drilled into bedrock on the western plateau of Mt. Elbrus (43 degrees 20' 53.9 '' N, 42 degrees 25'36.0 '' E; 5115ma.s.l.) in the Caucasus, Russia, in 2009. This is the first ice core in the region that represents a paleoclimate record that is practically undisturbed by seasonal melting. Relatively high snow accumulation rates at the drilling site enabled the analysis of the intraseasonal variability in climate proxies. Borehole temperatures ranged from -17 degrees C at 10m depth to -2.4 degrees C at 182 m. A detailed radio-echo sounding survey showed that the glacier thickness ranged from 45m near the marginal zone of the plateau up to 255m at the glacier center. The ice core has been analyzed for stable isotopes (delta O-18 and delta D), major ions (K+, Na+, Ca2+, Mg2+, NH4+, SO42-, NO3-, Cl-, F-), succinic acid (HOOCCH2COOH), and tritium content. The mean annual net accumulation rate of 1455mmw : e : for the last 140 years was estimated from distinct annual osc

U2 - 10.5194/tc-9-2253-2015

DO - 10.5194/tc-9-2253-2015

M3 - Article

VL - 9

SP - 2253

EP - 2270

JO - Cryosphere

JF - Cryosphere

SN - 1994-0416

IS - 6

ER -

ID: 3987222