scholarly journals Tree-Ring Based Chronology of Landslides in the Shirakami Mountains, Japan

Water ◽  
2021 ◽  
Vol 13 (9) ◽  
pp. 1185
Author(s):  
Kinuko Noguchi ◽  
Ching-Ying Tsou ◽  
Yukio Ishikawa ◽  
Daisuke Higaki ◽  
Chun-Yi Wu

The N-Ohkawa landslide, and the southern section of the Ohkawa landslide, occurred during the snow-melt seasons of 1999 and 2006, respectively, in the Shirakami Mountains, Japan. This paper examines the response of trees in the Shirakami Mountains to landslides, and also investigates the spatio-temporal occurrence patterns of landslide events in the area. Dendrogeomorphological analysis was used to identify growth suppression and growth increase (GD) markers in tilted deciduous broadleaved trees and also to reveal the timing of the establishment of shade-intolerant tree species. Analysis of the GD markers detected in tree-ring width series revealed confirmatory evidence of landslide events that occurred in 1999 and 2006 and were observed by eyewitnesses, as well as signals from eight additional (previously unrecorded) landslide events during 1986–2005. Furthermore, shade-intolerant species were found to have become established on the N-Ohkawa and southern Ohkawa landslides, but with a lag of up to seven years following the landslide events causing the canopy opening.

Polar Biology ◽  
2017 ◽  
Vol 40 (9) ◽  
pp. 1761-1775 ◽  
Author(s):  
David G. Ainley ◽  
Ken Lindke ◽  
Grant Ballard ◽  
Phil O’B. Lyver ◽  
Scott Jennings ◽  
...  

The Holocene ◽  
2002 ◽  
Vol 12 (6) ◽  
pp. 759-789 ◽  
Author(s):  
Keith R. Briffa ◽  
Timothy J. Osborn ◽  
Fritz H. Schweingruber ◽  
Philip D. Jones ◽  
Stepan G. Shiyatov ◽  
...  

Trees ◽  
2011 ◽  
Vol 26 (3) ◽  
pp. 715-729 ◽  
Author(s):  
F. Lebourgeois ◽  
P. Mérian ◽  
F. Courdier ◽  
J. Ladier ◽  
P. Dreyfus

2015 ◽  
Vol 38 (6) ◽  
pp. 2019-2030 ◽  
Author(s):  
Peter M. Yates ◽  
Michelle R. Heupel ◽  
Andrew J. Tobin ◽  
Colin A. Simpfendorfer

Atmosphere ◽  
2021 ◽  
Vol 12 (7) ◽  
pp. 878
Author(s):  
Chang-Hyun Park ◽  
Ui-Cheon Lee ◽  
Soo-Chul Kim ◽  
Kwang-Hee Lee

To analyze the relationship between climatic factors (monthly mean temperature and total precipitation) and tree-ring growths of Pinus densiflora from the central region of the Republic of Korea, more than 20 trees were sampled from three national parks. The tree-ring chronology of Mt. Bukhan covering the period of 1917–2016 was assessed, as well as that of Mt. Seorak across 1687–2017 and Mt. Worak across 1777–2017. After cross-dating, each ring-width series was double-standardized by first fitting a logarithmic curve and then a 50 year cubic spline. Climate-growth relationships were computed with bootstrap correlation functions. The result of the analysis showed a positive response from the current March temperature and May precipitations for tree-ring growth of Pinus densiflora. It indicates that a higher temperature supply during early spring season and precipitation during cambium activity are important for radial growths of Pinus densiflora from the central region in the Republic of Korea.


2021 ◽  
Vol 303 ◽  
pp. 108394
Author(s):  
Nathsuda Pumijumnong ◽  
Piyarat Songtrirat ◽  
Supaporn Buajan ◽  
Sineenart Preechamart ◽  
Uthai Chareonwong ◽  
...  

Forests ◽  
2021 ◽  
Vol 12 (3) ◽  
pp. 283
Author(s):  
Burkhard Neuwirth ◽  
Inken Rabbel ◽  
Jörg Bendix ◽  
Heye R. Bogena ◽  
Boris Thies

The European heat wave of 2018 was characterized by extraordinarily dry and hot spring and summer conditions in many central and northern European countries. The average temperatures from June to August 2018 were the second highest since 1881. Accordingly, many plants, especially trees, were pushed to their physiological limits. However, while the drought and heat response of field crops and younger trees have been well investigated in laboratory experiments, little is known regarding the drought and heat response of mature forest trees. In this study, we compared the response of a coniferous and a deciduous tree species, located in western and central–western Germany, to the extreme environmental conditions during the European heat wave of 2018. Combining classic dendroecological techniques (tree–ring analysis) with measurements of the intra–annual stem expansion (dendrometers) and tree water uptake (sap flow sensors), we found contrasting responses of spruce and oak trees. While spruce trees developed a narrow tree ring in 2018 combined with decreasing correlations of daily sap flow and dendrometer parameters to the climatic parameters, oak trees developed a ring with above–average tree–ring width combined with increasing correlations between the daily climatic parameters and the parameters derived from sap flow and the dendrometer sensors. In conclusion, spruce trees reacted to the 2018 heat wave with the early completion of their growth activities, whereas oaks appeared to intensify their activities based on the water content in their tree stems.


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