Dual carbon and oxygen isotopes in Siberian tree rings as indicator of millennia sunshine duration changes

Описание

Тип публикации: статья из журнала

Год издания: 2024

Идентификатор DOI: 10.1016/j.scitotenv.2024.172042

Аннотация: The current lack of information on past summer sunshine duration variability from annually resolved palaeoclimatological archives is hindering progress in the understanding and modelling of the earth climate system. We show that a combination of tree-ring carbon and oxygen isotopes from Siberia provides robust information on summerПоказать полностьюsunshine duration, which we use for an annual 1505-year reconstruction of July sunshine duration variability (1,5K-SIB-JSDR). We found that the Medieval maximum is 56 % higher than the average over 1505 years. Rapid and drastic decreases in sunshine duration up to 60 % correspond to major stratospheric volcanic eruptions. Grand Solar Minima and total sunspot numbers are also well preserved in the 1,5K-SIB-JSDR. Coherency with a global air temperature composite and spring Arctic Oscillation indicate that a large-scale climate signal is retained in our sunshine reconstruction.

Ссылки на полный текст

Издание

Журнал: Science of the Total Environment

Выпуск журнала: Т. 927

Номера страниц: 172042

ISSN журнала: 00489697

Издатель: Elsevier Science Publishing Company, Inc.

Персоны

  • Churakova (Sidorova) Olga V. (Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Zürcherstrasse 111, CH-8903 Birmensdorf, Switzerland)
  • Siegwolf Rolf T.W. (Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Zürcherstrasse 111, CH-8903 Birmensdorf, Switzerland)
  • Zharkov Mikhail S.
  • Saurer Matthias (Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Zürcherstrasse 111, CH-8903 Birmensdorf, Switzerland)

Вхождение в базы данных