Тип публикации: статья из журнала
Год издания: 2013
Идентификатор DOI: 10.1007/s10584-013-0805-5
Ключевые слова: Climate condition, Hydrological changes, Oxygen isotopic, Precipitation reconstruction, Stable carbon isotopes, Stable isotope data, Stable isotopes, Temperature signal, Isotopes, Forestry, carbon isotope, chronology, climate conditions, coniferous tree, extreme event, hydrological change, oxygen isotope, precipitation (climatology), reconstruction, stable isotope, temperature profile, tree ring, Carbon, Rings, Trees, Altay [Russian Federation], Russian Federation
Аннотация: We present new tree-ring width, delta C-13, and delta O-18 chronologies from the Koksu site (49A degrees N, 86A degrees E, 2,200 m asl), situated in the Russian Altai. A strong temperature signal is recorded in the tree-ring width (June-July) and stable isotope (July-August) chronologies, a July precipitation signal captured by theПоказать полностьюstable isotope data. To investigate the nature of common climatic patterns, our new chronologies are compared with previously published tree-ring and stable isotope data from other sites in the Altai region. The temperature signal preserved in the conifer trees is strongly expressed at local and regional scales for all studied sites, resulting in even stronger temperature and precipitation signals in combined average chronologies compared to separate chronologies. This enables the reconstruction of June-July and July-August temperatures for the last 200 years using tree-ring and stable carbon isotopes. A July precipitation reconstruction based on oxygen isotopic variability recorded in tree-rings can potentially improve the understanding of hydrological changes and the occurrence of extreme events in the Russian Altai.
Журнал: CLIMATIC CHANGE
Выпуск журнала: Vol. 120, Is. 1-2
Номера страниц: 153-167
ISSN журнала: 01650009
Место издания: DORDRECHT
Издатель: SPRINGER