Precipitation variation since AD 1748 in the central Lesser Khingan Mountains, Northeast China

Inter-annual variations of precipitation play important roles in forest management and agricultural production. This study presents a 270-year precipitation reconstruction of winter to early growing season for the central Lesser Khingan Mountains, Northeast China based on tree-ring width data of 99...

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Bibliographic Details
Main Authors: Deng, G. (Author), Li, M. (Author), Shao, X. (Author), Yin, Z.-Y (Author)
Format: Article
Language:English
Published: Elsevier B.V. 2021
Subjects:
Online Access:View Fulltext in Publisher
LEADER 02870nam a2200565Ia 4500
001 10.1016-j.ecolind.2021.107969
008 220427s2021 CNT 000 0 und d
020 |a 1470160X (ISSN) 
245 1 0 |a Precipitation variation since AD 1748 in the central Lesser Khingan Mountains, Northeast China 
260 0 |b Elsevier B.V.  |c 2021 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1016/j.ecolind.2021.107969 
520 3 |a Inter-annual variations of precipitation play important roles in forest management and agricultural production. This study presents a 270-year precipitation reconstruction of winter to early growing season for the central Lesser Khingan Mountains, Northeast China based on tree-ring width data of 99 tree-ring cores of Korean pine from two sampling sites near Yichun city. The reconstruction explained 46% of the variance in precipitation from the previous October to current June during the calibration period CE 1959–2017. At decadal scale, we identified four dry periods that occurred during CE 1748–1759, 1774–1786, 1881–1886 and 1918–1924, and four wet periods occurring during CE 1790–1795, 1818–1824, 1852–1859 and 2008–2017, and the period CE 2008–2017 was the wettest in the past 270 years. Power spectral analysis and wavelet analysis revealed cyclic patterns on the inter-annual (2–3 years) and inter-decadal (~11 and ~30–60 years) timescales in the reconstructed series. In addition, the Asian polar vortex has an important effect on the precipitation in our study area. © 2021 The Author(s) 
650 0 4 |a Agricultural productions 
650 0 4 |a annual variation 
650 0 4 |a China 
650 0 4 |a forest management 
650 0 4 |a Forestry 
650 0 4 |a growing season 
650 0 4 |a Growing season 
650 0 4 |a Heilongjiang 
650 0 4 |a Interannual variation 
650 0 4 |a Landforms 
650 0 4 |a Northeast China 
650 0 4 |a Northeast China 
650 0 4 |a Pinus koraiensis 
650 0 4 |a polar vortex 
650 0 4 |a Power spectral analyse and wavelet analyse 
650 0 4 |a Power spectral analysis and wavelet analysis 
650 0 4 |a precipitation assessment 
650 0 4 |a precipitation intensity 
650 0 4 |a Precipitation reconstruction 
650 0 4 |a Precipitation reconstruction 
650 0 4 |a Precipitation variation 
650 0 4 |a sampling 
650 0 4 |a spectral analysis 
650 0 4 |a Spectrum analysis 
650 0 4 |a The lesser khingan mountain 
650 0 4 |a The Lesser Khingan Mountains 
650 0 4 |a tree ring 
650 0 4 |a Tree rings 
650 0 4 |a Tree-ring 
650 0 4 |a Tree-ring width 
650 0 4 |a wavelet analysis 
650 0 4 |a Wavelet analysis 
650 0 4 |a Xiao Hinggan Mountains 
700 1 |a Deng, G.  |e author 
700 1 |a Li, M.  |e author 
700 1 |a Shao, X.  |e author 
700 1 |a Yin, Z.-Y.  |e author 
773 |t Ecological Indicators