On the possibility to restore the climatic signal in the disturbed record of stable water isotope content in the old (0.4–1.2 Ma) Vostok ice (Central Antarctica)

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Led i Sneg-Ice and Snow Pub Date : 2019-12-01 DOI:10.15356/2076-6734-2019-4-463

A. Ekaykin, V. Lipenkov, A. Veres, A. Kozachek, A. Skakun

引用次数: 2

Abstract

О возможности реконструкции климатического сигнала в нарушенной записи изотопного состава древнего льда (0,4–1,2 млн лет назад) в керне станции Восток (Центральная Антарктида) © 2019 г. А.А. Екайкин1,2*, В.Я. Липенков1, А.Н. Верес1,2, А.В. Козачек1, А.А. Скакун1,3 1Арктический и Антарктический научноисследовательский институт, СанктПетербург, Россия; 2Институт наук о Земле, СанктПетербургский государственный университет, СанктПетербург, Россия; 3Центральная астрономическая (Пулковская) обсерватория, СанктПетербург, Россия *ekaykin@aari.ru

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古(0.4 ~ 1.2 Ma) Vostok冰稳定水同位素扰动记录恢复气候信号的可能性

改造可能性气候信号记录违反同位素为古老的冰(0.4 - 1.2万年前)的科恩(中央车站东南极洲aa)©2019年Екайкин1,2 *、В.Я.Липенков1,aa,舍夫Верес1,2 av:Козачек1Скакун1,3 1арктическ和南极科学研究所、俄罗斯,圣彼得堡;社会2Институт地球科学,圣彼得堡国立大学、俄罗斯,圣彼得堡;3центральн天文(пулковск)、俄罗斯,圣彼得堡* ekaykin@aari.ru天文台

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来源期刊

Led i Sneg-Ice and Snow GEOSCIENCES, MULTIDISCIPLINARY-

CiteScore

1.50

自引率

42.90%

发文量

审稿时长

8 weeks

期刊介绍： The journal was established with the aim of publishing new research results of the Earth cryosphere. Results of works in physics, mechanics, geophysics, and geochemistry of snow and ice are published here together with geographical aspects of the snow-ice phenomena occurrence in their interaction with other components of the environment. The challenge was to discuss the latest results of investigations carried out on Russia’s territory and works performed by Russian investigators together with foreign colleagues. Editorial board works in collaboration with Glaciological Association that is professional community of specialists in glaciology from all republics of the Former Soviet Union which are now new independent states. The journal serves as a platform for the presentation and discussion of new discoveries and results which help to elucidate the state of the Earth’s cryosphere and the characteristics of the evolution of the snow-ice processes and phenomena under the current conditions of rapid climate change.