Chemical, isotopic and gas composition of the first-year sea ice in 2013-2015 from the data of cores taken at the BARNEO drifting stations

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY Led i Sneg-Ice and Snow Pub Date : 2019-09-21 DOI:10.15356/2076-6734-2019-3-387

A. Kizyakov, I. Streletskaya, A. Savenko, I. A. Kraynyukova, I. Tokarev

引用次数: 0

Abstract

Химический, изотопный и газовый состав однолетнего морского льда по данным кернов дрейфующих станций БАРНЕО за 2013–2015 гг. © 2019 г. А.И. Кизяков1*, И.Д. Стрелецкая1, А.В. Савенко1, И.А. Крайнюкова2, И.В. Токарев2 1Московский государственный университет имени М .В . Ломоносова, Москва, Россия; 2Ресурсный центр «Рентгенодифракционные методы исследования», Научный парк СанктПетербургского государ ственного университета, СанктПетербург, Россия *akizyakov@mail .ru

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一年生海冰的化学同位素和天然气构成数据kern车站为2013 - 2015年间已经漂移©2019年人工智能身份证Стрелецкая1Кизяков1 *,av:Савенко1Крайнюкова2中学,静脉Токарев2 1московскm正是《国立大学。洛蒙诺索夫，莫斯科，俄罗斯;2ресурснx光衍射方法研究中心”,社会科技园圣彼得堡纯真国王大学、俄罗斯,圣彼得堡* ru akizyakov@mail

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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.