Eco-physiological response of conifers from high-latitude and -altitude eurasian regions to stratospheric volcanic eruptions | Научно-инновационный портал СФУ

Eco-physiological response of conifers from high-latitude and -altitude eurasian regions to stratospheric volcanic eruptions

Тип публикации: статья из журнала

Год издания: 2020

Идентификатор DOI: 10.17516/1997-1389-0313

Ключевые слова: air temperature, cell wall thickness, maximum latewood density, precipitation, sunshine duration, tree-ring width, vapor pressure deficit, δ13c and δ18o in tree-ring cellulosethis work was supported by the rfbi 16-55-76012 era_a granted to e.a. vaganov to perform analysis of volcanic eruptions based on tree/ring width from eurasian subarctic and eranet rus plus snf izrpz0_16473, granted to m. stoffel (“effects of large volcanic eruptions on eurasian climate and societies: unravelling past evidence to predict future impacts”, to perform analysis of volcanic eruptions based on stable carbon and oxygen isotopes in tree-ring cellulose for eurasian subarctic), russian science foundation rsf 19-14-00028 granted to v.s. myglan (“extreme (catastrophic) droughts in the south of siberia over the past thousand years” for performing stable carbon and oxygen isotope analyses, measurements of wood anatomical parameters for extreme years, characterized by dry conditions in the altai-sayan mountain region), marie-curie individual fellowship granted to o.v. churakova (sidorova) within eu_isotrec 235122, 909122 (“climatic and environmental changes in the eurasian subarctic inferred from tree-ring and stable isotope chronologies for the past and recent periods” for revealing climatic and environmental changes after major volcanic eruptions in eurasian subarctic), and rfbr 18-45-240001-р_а (“prognosis of region-specific responses of siberian mountain forests to global environmental changes and of the landscape development trajectories for mitigation of environmental risks and an effective long-term planning in various economic sectors”, for analysis and estimation of climate in siberian subarctic regions after global anomaly events). the authors are grateful to anonymous reviewers for comments and valuable suggestions.

Аннотация: Stratospheric volcanic eruptions have had significant impacts on the radiation budget, atmospheric and surface temperatures, precipitation and regional weather patterns, resulting in global climatic changes. The changes associated with such eruptions most commonly result in cooling during several years after events. This study aimed to reveal eco-physiological response of larch trees from northeastern Yakutia (YAK), eastern Taimyr (TAY) and Altai (ALT) regions to climatic anomalies after major volcanic eruptions CE 535, 540, 1257, 1641, 1815 and 1991 using new multiple tree-ring parameters: Tree-ring width (TRW), maximum latewood density (MXD), cell wall thicknesses (CWT), δ13C and δ18O in tree-ring cellulose. This investigation showed that TRW, CWT, MXD and δ18O chronologies recorded temperature signal, while information about precipitation and vapor pressure deficit was captured by δ13C chronologies. Sunshine duration was well recorded in δ18O from YAK and ALT. Tree-ring parameters recorded cold, wet and cloudy summer anomalies during the 6th and 13th centuries. However, significant summer anomalies after Tambora (1815) and Pinatubo (1991) eruptions were not captured by any tree-ring parameters. © 2020 JMIR Human Factors.All right reserved.

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Издание

Журнал: Journal of Siberian Federal University - Biology

Выпуск журнала: Vol. 13, Is. 1

Номера страниц: 5-24

ISSN журнала: 19971389

Авторы

  • Churakova O.V. (Siberian Federal University, Krasnoyarsk, Russian Federation, University of Geneva, Geneva, Switzerland, Swiss Federal Research Institute for Forest, Snow and Landscape WSL, Birmensdorf, Switzerland)
  • Fonti M.V. (Siberian Federal University, Krasnoyarsk, Russian Federation, Swiss Federal Research Institute for Forest, Snow and Landscape WSL, Birmensdorf, Switzerland)
  • Kirdyanov A.V. (Siberian Federal University, Krasnoyarsk, Russian Federation, Sukachev Institute of Forest SB RASFRC "Krasnoyarsk Science Center SB RAS", Krasnoyarsk, Russian Federation, University of Cambridge, Cambridge, United Kingdom)
  • Myglan V.S. (Siberian Federal University, Krasnoyarsk, Russian Federation)
  • Barinov V.V. (Siberian Federal University, Krasnoyarsk, Russian Federation)
  • Sviderskaya I.V. (Siberian Federal University, Krasnoyarsk, Russian Federation)
  • Naumova O.V. (Siberian Federal University, Krasnoyarsk, Russian Federation)
  • Ovchinnikov D.V. (Sukachev Institute of Forest SB RASFRC "Krasnoyarsk Science Center SB RAS", Krasnoyarsk, Russian Federation)
  • Shashkin A.V. (Sukachev Institute of Forest SB RASFRC "Krasnoyarsk Science Center SB RAS", Krasnoyarsk, Russian Federation)
  • Saurer M. (Swiss Federal Research Institute for Forest, Snow and Landscape WSL, Birmensdorf, Switzerland, Paul Scherrer Institute Villigen - PSI, Switzerland)
  • Guillet S. (University of Geneva, Geneva, Switzerland)
  • Corona C. (Université Blaise Pascal Clermont-Ferrand, France)
  • Fonti P. (Swiss Federal Research Institute for Forest, Snow and Landscape WSL, Birmensdorf, Switzerland)
  • Panyushkina I.P. (University of Arizona, Tucson, United States)
  • Büntgen U. (Swiss Federal Research Institute for Forest, Snow and Landscape WSL, Birmensdorf, Switzerland, University of Cambridge, Cambridge, United Kingdom)
  • Hughes M.K. (University of Arizona, Tucson, United States)
  • Siegwolf R.T.W. (Swiss Federal Research Institute for Forest, Snow and Landscape WSL, Birmensdorf, Switzerland, Université Blaise Pascal Clermont-Ferrand, France)
  • Stoffel M. (University of Geneva, Geneva, Switzerland)
  • Vaganov E.A. (Siberian Federal University, Krasnoyarsk, Russian Federation, Sukachev Institute of Forest SB RASFRC "Krasnoyarsk Science Center SB RAS", Krasnoyarsk, Russian Federation)

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