Extreme climatic events in the Altai Republic according to dendrochronological data

被引:9
|
作者
Barinov, V. V. [1 ]
Myglan, V. S. [1 ,5 ]
Nazarov, A. N. [1 ]
Vaganov, E. A. [1 ]
Agatova, A. R. [2 ,3 ]
Nepop, R. K. [2 ,4 ]
机构
[1] Siberian Fed Univ, Pr Svobodnyi 79, Krasnoyarsk 660041, Russia
[2] Russian Acad Sci, Siberian Branch, Inst Geol & Mineral, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia
[3] Ural Fed Univ, Ul Mira 19, Ekaterinburg 620002, Russia
[4] Novosibirsk State Univ, Ul Pirogova 2, Novosibirsk 630090, Russia
[5] Russian Acad Sci, Siberian Branch, Sukachev Inst Forestry, Akademgorodok 50,Str 28, Krasnoyarsk 660036, Russia
基金
俄罗斯科学基金会; 俄罗斯基础研究基金会;
关键词
RINGS;
D O I
10.1134/S1062359016020023
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
The results of dating of extreme climatic events by damage to the anatomical structure and missing tree rings of the Siberian larch in the upper forest boundary of the Altai Republic are given. An analysis of the spatial distribution of the revealed dates over seven plots (Kokcy, Chind, Ak-ha, Jelo, Tute, Tara, and Sukor) allowed us to distinguish the extreme events on interregional (1700, 1783, 1788, 1812, 1814, 1884), regional (1724, 1775, 1784, 1835, 1840, 1847, 1850, 1852, 1854, 1869, 1871, 1910, 1917, 1927, 1938, 1958, 1961), and local (1702, 1736, 1751, 1785, 1842, 1843, 1874, 1885, 1886, 1919, 2007, and 2009) scales. It was shown that the events of an interregional scale correspond with the dates of major volcanic eruptions (Grimsvotn, Lakagigar, Etna, Awu, Tambora, Soufriere St. Vinsent, Mayon, and Krakatau volcanos) and extreme climatic events, crop failures, lean years, etc., registered in historical sources.
引用
收藏
页码:152 / 161
页数:10
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