First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core

Central Antarctica is characterized by a crucial lack of information on climate variability during the late Holocene. The study of firn cores obtained from the central part of the East Antarctic Ice Sheet is essential for the reconstruction of the paleoclimatic conditions at the continental and regi...

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Published in:Arctic and Antarctic Research
Main Authors: A. N. Veres, A. A. Ekaykin, V. Ya. Lipenkov, A. V. Turkeev, T. V. Khodzer, А. Н. Верес, А. А. Екайкин, В. Я. Липенков, А. В. Туркеев, Т. В. Ходжер
Other Authors: This work is performed as part of the project 5.2 RTR of Roshydromet “Comprehensive oceanological, climatological, glaciological and geophysical studies of Antarctica and the Southern Ocean”. The authors are grateful to the administration of the Russian Antarctic Expedition (RAE) and its chief Klepikov A. V. for the logistical support of the glaciological program at Vostok Station, as well as to the participants of the 62th winter season for their assistance in the drilling work at the VK16 borehole, in particular V. Zarovchatsky and M. Zyukov, Работа выполнялась в рамках проекта 5.2 НИТР Росгидромета «Комплексные океанологические, климатические, гляциологические и геофизические исследования Антарктиды и Южного океана». Авторы благодарят Российскую антарктическую экспедицию и ее начальника А.В. Клепикова за поддержку и логистическое обеспечение полевыхработ в районе станции Восток, а также сотрудников зимовочного состава 62-й РАЭ станции Восток Виталия Заровчатского и Максима Зюкова за помощь в проведении буровых работ на скважине VK16
Format: Article in Journal/Newspaper
Language:Russian
Published: Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт 2020
Subjects:
Rae
Online Access:https://www.aaresearch.science/jour/article/view/321
https://doi.org/10.30758/0555-2648-2020-66-4-482-500
id ftjaaresearch:oai:oai.aari.elpub.ru:article/321
record_format openpolar
institution Open Polar
collection Arctic and Antarctic Research
op_collection_id ftjaaresearch
language Russian
topic температура воздуха
air temperature
firn dating
firn density
firn cores
inventory of volcanic events
Late Holocene
paleoclimate
snow accumulation rate
stable water isotopes
Vostok Station
датировка
керны
летопись вулканических событий
палеоклимат
плотность фирна
поздний голоцен
скорость снегонакопления
стабильные изотопы воды
станция Восток
spellingShingle температура воздуха
air temperature
firn dating
firn density
firn cores
inventory of volcanic events
Late Holocene
paleoclimate
snow accumulation rate
stable water isotopes
Vostok Station
датировка
керны
летопись вулканических событий
палеоклимат
плотность фирна
поздний голоцен
скорость снегонакопления
стабильные изотопы воды
станция Восток
A. N. Veres
A. A. Ekaykin
V. Ya. Lipenkov
A. V. Turkeev
T. V. Khodzer
А. Н. Верес
А. А. Екайкин
В. Я. Липенков
А. В. Туркеев
Т. В. Ходжер
First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core
topic_facet температура воздуха
air temperature
firn dating
firn density
firn cores
inventory of volcanic events
Late Holocene
paleoclimate
snow accumulation rate
stable water isotopes
Vostok Station
датировка
керны
летопись вулканических событий
палеоклимат
плотность фирна
поздний голоцен
скорость снегонакопления
стабильные изотопы воды
станция Восток
description Central Antarctica is characterized by a crucial lack of information on climate variability during the late Holocene. The study of firn cores obtained from the central part of the East Antarctic Ice Sheet is essential for the reconstruction of the paleoclimatic conditions at the continental and regional scales over the past 2,000 years (the Late Holocene). Based on glaciological and isotopic data from the shallow VK16 core drilled in the vicinity of Vostok Station over the periods of the 62th (2016-2017) and 63th (2017-2018) summer seasons of RAE, climatic characteristics have been reconstructed for the period 216 BC - 2010 AD. Studies of the VK16 core were carried out in two stages: firn density and electrical conductivity measurement (ECM), as well as sampling, was performed in the glaciological laboratory of the 5G drilling complex (Vostok Station) soon after the firn recovery, while the isotopic composition of the core samples was measured by a Picarro L-2120i laser analyzer in the Climate and Environmental Research Laboratory of AARI. In the ECM profile of the core, we discovered 14 absolute age markers (layers containing the products of known volcanic eruptions). These markers have allowed us to develop a robust chronostratigraphic scale for this core. We have shown that the main feature of the Late Holocene climate in this part of Antarctica is that the near-surface air temperature remained essentially constant throughout the whole time period under consideration. At the same time, the snow accumulation rate varied significantly around a mean value of 1.83 g cm-2 year-1, while the last 200 years were characterized by the highest snow accumulation rate, equal to 2.08 g cm-2 year-1. In this paper, we describe methods for studying firn cores, which can be useful for further research, and present first preliminary data on the climate variability in the vicinity of Vostok Station during the late Holocene. Климатическая изменчивость в Восточной Антарктиде за последние 2000 лет мало изучена. Бурение и ...
author2 This work is performed as part of the project 5.2 RTR of Roshydromet “Comprehensive oceanological, climatological, glaciological and geophysical studies of Antarctica and the Southern Ocean”. The authors are grateful to the administration of the Russian Antarctic Expedition (RAE) and its chief Klepikov A. V. for the logistical support of the glaciological program at Vostok Station, as well as to the participants of the 62th winter season for their assistance in the drilling work at the VK16 borehole, in particular V. Zarovchatsky and M. Zyukov
Работа выполнялась в рамках проекта 5.2 НИТР Росгидромета «Комплексные океанологические, климатические, гляциологические и геофизические исследования Антарктиды и Южного океана». Авторы благодарят Российскую антарктическую экспедицию и ее начальника А.В. Клепикова за поддержку и логистическое обеспечение полевыхработ в районе станции Восток, а также сотрудников зимовочного состава 62-й РАЭ станции Восток Виталия Заровчатского и Максима Зюкова за помощь в проведении буровых работ на скважине VK16
format Article in Journal/Newspaper
author A. N. Veres
A. A. Ekaykin
V. Ya. Lipenkov
A. V. Turkeev
T. V. Khodzer
А. Н. Верес
А. А. Екайкин
В. Я. Липенков
А. В. Туркеев
Т. В. Ходжер
author_facet A. N. Veres
A. A. Ekaykin
V. Ya. Lipenkov
A. V. Turkeev
T. V. Khodzer
А. Н. Верес
А. А. Екайкин
В. Я. Липенков
А. В. Туркеев
Т. В. Ходжер
author_sort A. N. Veres
title First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core
title_short First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core
title_full First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core
title_fullStr First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core
title_full_unstemmed First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core
title_sort first data on the climate variability in the vicinity of vostok station (central antarctica) over the past 2,000 years based on the study of a snow-firn core
publisher Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт
publishDate 2020
url https://www.aaresearch.science/jour/article/view/321
https://doi.org/10.30758/0555-2648-2020-66-4-482-500
long_lat ENVELOPE(-44.600,-44.600,-60.750,-60.750)
ENVELOPE(106.837,106.837,-78.464,-78.464)
geographic Antarctic
East Antarctic Ice Sheet
Rae
Vostok Station
geographic_facet Antarctic
East Antarctic Ice Sheet
Rae
Vostok Station
genre Annals of Glaciology
Antarc*
Antarctic
Antarctica
Arctic
Ice Sheet
Journal of Glaciology
The Cryosphere
Антарктида
genre_facet Annals of Glaciology
Antarc*
Antarctic
Antarctica
Arctic
Ice Sheet
Journal of Glaciology
The Cryosphere
Антарктида
op_source Arctic and Antarctic Research; Том 66, № 4 (2020); 482-500
Проблемы Арктики и Антарктики; Том 66, № 4 (2020); 482-500
2618-6713
0555-2648
10.30758/0555-2648-2020-66-4
op_relation https://www.aaresearch.science/jour/article/view/321/182
Проект CLIVASH2k. URL: http://pastglobalchanges.org/ini/wg/2k-network/projects/clivash (дата обращения 01.08.2020)
Проект IPICS. URL: http://pastglobalchanges.org/science/end-aff/ipics/intro (дата обращения 01.08.2020)
Проект PAGES2k. URL: http://pastglobalchanges.org/science/wg/2k-network/intro (дата обращения 01.08.2020)
Ahmed M., Anchukaitis K. J., Asrat A. et al. Continental-scale temperature variability during the past two millennia // Nature geoscience. 2013. V 6. № 5. P. 339-346.
Stenni B., Curran M.A.J., Abram N.J., Orsi A., Goursaud S., Masson-Delmotte V., Neukom R., Goosse H., Divine D., van Ommen T., Steig E.J., Dixon D.A., Thomas E.R., Bertler N.A.N., Isaksson E., Ekaykin A., Werner M., Frezzotti M. Antarctic climate variability on regional and continental scales over the last 2000 years // Climate of the Past. 2017. V. 13. P. 1609-1634.
Thomas E.R., van Wessem J.M., Roberts J., Isaksson E., Schlosser E., Fudge T.J., Vallelonga P., Medley B., Lenaerts J., Bertler N., van den Broeke M.R., Dixon D.A., Frezzotti M., Stenni B., Curran M., Ekaykin A.A. Regional Antarctic snow accumulation over the past 1000 years // Climate of the Past. 2017. V. 13. P. 1491-1513.
Ekaykin A.A., Kozachek A.V., Lipenkov V.Ya., Shibaev Yu.A. Multiple climate shifts in the Southern Hemisphere over the past three centuries based on central Antarctic snow pits and core studies // Annals of Glaciology. 2014. V. 55. № 66. P. 259-266.
Petit J.R., Jouzel J., Raynaud D., Barkov N.I., Barnola J.-M., Basile I., Bender M., Chappellaz J., Davisk M., Delaygue G., Delmotte M., Kotlyakov V.M., Legrand M., Lipenkov V.Ya., Lorius C., Pe’pin L., Ritz C., Saltzmank E., Stievenard M. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica // Nature. 1999. V. 399. № 6735. P. 429-436.
Veres D., Bazin L., Landais A., Toye Mahamadou Kele H., Lemieux-Dudon B., Parrenin F., Martinerie P., Blayo E., Blunier T., Capron E., Chappellaz J., Rasmussen S.O., Severi M., Svensson A., Vinther B., Wolff E.W. The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years // Climate of the Past. 2013. V. 9. P. 1733-1748.
Munch T., Kipfstuhl S., Freitag J., Meyer H., Laepple T. Regional climate signal vs. local noise: a two-dimensional view of water isotopes in Antarctic firn at Kohnen Station, Dronning Maud Land // Climate of the Past. 2016. V. 12. P. 1565-1581.
Екайкин А.А., Тебенькова Н.А., Липенков В.Я., Чихачев К.Б., Верес А.Н., Рихтер А. Недооценка скорости снегонакопления в центральной части Антарктиды (станция Восток) по данным реечных наблюдений // Метеорология и гидрология. 2020. № 2. С. 114-125.
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Toohey M., Sigl M. Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE // Earth System Science Data. 2017. V. 9. P. 809-831.
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https://www.aaresearch.science/jour/article/view/321
doi:10.30758/0555-2648-2020-66-4-482-500
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op_doi https://doi.org/10.30758/0555-2648-2020-66-4-482-50010.30758/0555-2648-2020-66-410.1029/2004JD005259
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spelling ftjaaresearch:oai:oai.aari.elpub.ru:article/321 2024-06-23T07:45:38+00:00 First data on the climate variability in the vicinity of Vostok Station (central Antarctica) over the past 2,000 years based on the study of a snow-firn core Первые данные о климатической изменчивости в районе ст. Восток (Центральная Антарктида) за последние 2000 лет по результатам изучения снежно-фирнового керна A. N. Veres A. A. Ekaykin V. Ya. Lipenkov A. V. Turkeev T. V. Khodzer А. Н. Верес А. А. Екайкин В. Я. Липенков А. В. Туркеев Т. В. Ходжер This work is performed as part of the project 5.2 RTR of Roshydromet “Comprehensive oceanological, climatological, glaciological and geophysical studies of Antarctica and the Southern Ocean”. The authors are grateful to the administration of the Russian Antarctic Expedition (RAE) and its chief Klepikov A. V. for the logistical support of the glaciological program at Vostok Station, as well as to the participants of the 62th winter season for their assistance in the drilling work at the VK16 borehole, in particular V. Zarovchatsky and M. Zyukov Работа выполнялась в рамках проекта 5.2 НИТР Росгидромета «Комплексные океанологические, климатические, гляциологические и геофизические исследования Антарктиды и Южного океана». Авторы благодарят Российскую антарктическую экспедицию и ее начальника А.В. Клепикова за поддержку и логистическое обеспечение полевыхработ в районе станции Восток, а также сотрудников зимовочного состава 62-й РАЭ станции Восток Виталия Заровчатского и Максима Зюкова за помощь в проведении буровых работ на скважине VK16 2020-11-28 application/pdf https://www.aaresearch.science/jour/article/view/321 https://doi.org/10.30758/0555-2648-2020-66-4-482-500 rus rus Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт https://www.aaresearch.science/jour/article/view/321/182 Проект CLIVASH2k. URL: http://pastglobalchanges.org/ini/wg/2k-network/projects/clivash (дата обращения 01.08.2020) Проект IPICS. URL: http://pastglobalchanges.org/science/end-aff/ipics/intro (дата обращения 01.08.2020) Проект PAGES2k. URL: http://pastglobalchanges.org/science/wg/2k-network/intro (дата обращения 01.08.2020) Ahmed M., Anchukaitis K. J., Asrat A. et al. Continental-scale temperature variability during the past two millennia // Nature geoscience. 2013. V 6. № 5. P. 339-346. Stenni B., Curran M.A.J., Abram N.J., Orsi A., Goursaud S., Masson-Delmotte V., Neukom R., Goosse H., Divine D., van Ommen T., Steig E.J., Dixon D.A., Thomas E.R., Bertler N.A.N., Isaksson E., Ekaykin A., Werner M., Frezzotti M. Antarctic climate variability on regional and continental scales over the last 2000 years // Climate of the Past. 2017. V. 13. P. 1609-1634. Thomas E.R., van Wessem J.M., Roberts J., Isaksson E., Schlosser E., Fudge T.J., Vallelonga P., Medley B., Lenaerts J., Bertler N., van den Broeke M.R., Dixon D.A., Frezzotti M., Stenni B., Curran M., Ekaykin A.A. Regional Antarctic snow accumulation over the past 1000 years // Climate of the Past. 2017. V. 13. P. 1491-1513. Ekaykin A.A., Kozachek A.V., Lipenkov V.Ya., Shibaev Yu.A. Multiple climate shifts in the Southern Hemisphere over the past three centuries based on central Antarctic snow pits and core studies // Annals of Glaciology. 2014. V. 55. № 66. P. 259-266. Petit J.R., Jouzel J., Raynaud D., Barkov N.I., Barnola J.-M., Basile I., Bender M., Chappellaz J., Davisk M., Delaygue G., Delmotte M., Kotlyakov V.M., Legrand M., Lipenkov V.Ya., Lorius C., Pe’pin L., Ritz C., Saltzmank E., Stievenard M. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica // Nature. 1999. V. 399. № 6735. P. 429-436. Veres D., Bazin L., Landais A., Toye Mahamadou Kele H., Lemieux-Dudon B., Parrenin F., Martinerie P., Blayo E., Blunier T., Capron E., Chappellaz J., Rasmussen S.O., Severi M., Svensson A., Vinther B., Wolff E.W. The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years // Climate of the Past. 2013. V. 9. P. 1733-1748. Munch T., Kipfstuhl S., Freitag J., Meyer H., Laepple T. Regional climate signal vs. local noise: a two-dimensional view of water isotopes in Antarctic firn at Kohnen Station, Dronning Maud Land // Climate of the Past. 2016. V. 12. P. 1565-1581. Екайкин А.А., Тебенькова Н.А., Липенков В.Я., Чихачев К.Б., Верес А.Н., Рихтер А. Недооценка скорости снегонакопления в центральной части Антарктиды (станция Восток) по данным реечных наблюдений // Метеорология и гидрология. 2020. № 2. С. 114-125. Lipenkov V.Ya., Salamatin A.N., Duval P. Bubbly-ice densification in ice sheets: II. Applications // Journal of Glaciology. 1997. V. 43. № 145. P. 397-407. Castellano E., Becagli S., Hansson M., Hutterli M., Petit J.R., Rampino M.R., Severi M., Steffensen J.P., Traversi R., Udisti R. Holocene volcanic history as recorded in the sulfate stratigraphy of the European Project for Ice Coring in Antarctica Dome C (EDC96) ice core // Journal of Geophysical Research. 2005. V. 110. P. D06114. doi:10.1029/2004JD005259. Osipov E.Y., Khodzher T.V., Golobokova L.P., Onischuk N.A., Lipenkov V.Ya., Ekaykin A.A., Shibaev Yu.A., Osipova O.P. High-resolution 900 year volcanic and climatic record from the Vostok area, East Antarctica // The Cryosphere. 2014. V. 8. P. 843-851. Toohey M., Sigl M. Volcanic stratospheric sulphur injections and aerosol optical depth from 500 BCE to 1900 CE // Earth System Science Data. 2017. V. 9. P. 809-831. SiglM, WinstrupM., McConnell J.R., Welten K.C., PlunkettG., LudlowF, Buntgen U., CaffeeM, Chellman N., Dahl-Jensen D., Fischer H., Kipfstuhl S., Kostick C., Maselli O.J., Mekhaldi F., Mulvaney R., Muscheler R., Pasteris D.R., Pilcher J.R., Salzer M., Schupbach S., Steffensen J.P., Vinther B.M., Woodruff T.E. Timing and climate forcing of volcanic eruptions for the past 2,500 years // Nature. 2015. V. 523. P. 543-549. Ekaykin A.A., Lipenkov V.Ya., Kuzmina I.N., Petit J.R., Masson-Delmotte V., Johnsen S.J. 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Arctic and Antarctic Research; Том 66, № 4 (2020); 482-500 Проблемы Арктики и Антарктики; Том 66, № 4 (2020); 482-500 2618-6713 0555-2648 10.30758/0555-2648-2020-66-4 температура воздуха air temperature firn dating firn density firn cores inventory of volcanic events Late Holocene paleoclimate snow accumulation rate stable water isotopes Vostok Station датировка керны летопись вулканических событий палеоклимат плотность фирна поздний голоцен скорость снегонакопления стабильные изотопы воды станция Восток info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2020 ftjaaresearch https://doi.org/10.30758/0555-2648-2020-66-4-482-50010.30758/0555-2648-2020-66-410.1029/2004JD005259 2024-05-31T03:22:51Z Central Antarctica is characterized by a crucial lack of information on climate variability during the late Holocene. The study of firn cores obtained from the central part of the East Antarctic Ice Sheet is essential for the reconstruction of the paleoclimatic conditions at the continental and regional scales over the past 2,000 years (the Late Holocene). Based on glaciological and isotopic data from the shallow VK16 core drilled in the vicinity of Vostok Station over the periods of the 62th (2016-2017) and 63th (2017-2018) summer seasons of RAE, climatic characteristics have been reconstructed for the period 216 BC - 2010 AD. Studies of the VK16 core were carried out in two stages: firn density and electrical conductivity measurement (ECM), as well as sampling, was performed in the glaciological laboratory of the 5G drilling complex (Vostok Station) soon after the firn recovery, while the isotopic composition of the core samples was measured by a Picarro L-2120i laser analyzer in the Climate and Environmental Research Laboratory of AARI. In the ECM profile of the core, we discovered 14 absolute age markers (layers containing the products of known volcanic eruptions). These markers have allowed us to develop a robust chronostratigraphic scale for this core. We have shown that the main feature of the Late Holocene climate in this part of Antarctica is that the near-surface air temperature remained essentially constant throughout the whole time period under consideration. At the same time, the snow accumulation rate varied significantly around a mean value of 1.83 g cm-2 year-1, while the last 200 years were characterized by the highest snow accumulation rate, equal to 2.08 g cm-2 year-1. In this paper, we describe methods for studying firn cores, which can be useful for further research, and present first preliminary data on the climate variability in the vicinity of Vostok Station during the late Holocene. Климатическая изменчивость в Восточной Антарктиде за последние 2000 лет мало изучена. Бурение и ... Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Antarctica Arctic Ice Sheet Journal of Glaciology The Cryosphere Антарктида Arctic and Antarctic Research Antarctic East Antarctic Ice Sheet Rae ENVELOPE(-44.600,-44.600,-60.750,-60.750) Vostok Station ENVELOPE(106.837,106.837,-78.464,-78.464) Arctic and Antarctic Research 66 4 482 500