Сибирский федеральный университет

Тип публикации: статья из журнала

Год издания: 2016

Идентификатор DOI: 10.1088/1748-9326/11/7/074021

Ключевые слова: boreal forest, climate variability, dendroecology, Eurasia, forest productivity, global warming, high northern latitudes, 20TH-CENTURY SUMMER WARMTH, TREE-RING CHRONOLOGY, SCOTS PINE, 2 MILLENNIA, TEMPERATURE VARIABILITY, NORTHERN-HEMISPHERE, CENTRAL SIBERIA, WORLDS FORESTS, WHITE SPRUCE, CARBON-CYCLE, Carbon, Climate change, Complex networks, Productivity, Boreal forests, Northern latitudes, Forestry, Larix decidua, Picea

Аннотация: The area covered by boreal forests accounts for similar to 16% of the global and 22% of the Northern Hemisphere landmass. Changes in the productivity and functioning of this circumpolar biome not only have strong effects on species composition and diversity at regional to larger scales, but also on the Earth's carbon cycle. Although temporal inconsistency in the response of tree growth to temperature has been reported from some locations at the higher northern latitudes, a systematic dendroecological network assessment is still missing for most of the boreal zone. Here, we analyze the geographical patterns of changes in summer temperature and precipitation across northern Eurasia >60 degrees N since 1951 AD, as well as the growth trends and climate responses of 445 Pinus, Larix and Picea ring width chronologies in the same area and period. In contrast to widespread summer warming, fluctuations in precipitation and tree growth are spatially more diverse and overall less distinct. Although the influence of summer temperature on ring formation is increasing with latitude and distinct moisture effects are restricted to a few southern locations, growth sensitivity to June-July temperature variability is only significant at 16.6% of all sites (p

Журнал: Environmental Research Letters

Выпуск журнала: Vol. 11, Is. 7

Номера страниц: 74021

ISSN журнала: 17489326

Место издания: BRISTOL

Издатель: IOP PUBLISHING LTD

• Hellmann Lena (Oeschger Ctr Climate Change Res, Bern, Switzerland;; )
• Agafonov Leonid (Inst Plant & Anim Ecol UD RAS, Ekaterinburg, Russia;; )
• Ljungqvist Fredrik Charpentier (Stockholm Univ, Dept Hist, Stockholm, Sweden;; ; Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden;; )
• Churakova Olga V. (Swiss Fed Inst Technol, Inst Terr Ecosyst, Zurich, Switzerland;; )
• Duethorn Elisabeth (Johannes Gutenberg Univ Mainz, Mainz, Germany;; )
• Esper Jan (Johannes Gutenberg Univ Mainz, Mainz, Germany;; )
• Hulsmann Lisa (Swiss Fed Inst Technol, Inst Terr Ecosyst, Zurich, Switzerland;; )
• Kirdyanov Alexander V. (VN Sukachev Inst Forest SB RAS, Krasnoyarsk, Russia;; ; Siberian Fed Univ, Krasnoyarsk, Russia;; )
• Moiseev Pavel (Inst Plant & Anim Ecol UD RAS, Ekaterinburg, Russia;; )
• Myglan Vladimir S. (Siberian Fed Univ, Krasnoyarsk, Russia;; )
• Nikolaev Anatoly N. (North Eastern Fed Univ, Yakutsk, Russia;; ; Melnikov Permafrost Inst, Yakutsk, Russia;; )
• Reinig Frederick
• Schweingruber Fritz H.
• Solomina Olga (RAS, Inst Geog, Moscow, Russia;; )
• Tegel Willy (WSL, Swiss Fed Res Inst, Birmensdorf, Switzerland;; ; Univ Freiburg, Inst Forest Sci IWW, Freiburg, Germany)
• Buntgen Ulf (Oeschger Ctr Climate Change Res, Bern, Switzerland;; )

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