VS-oscilloscope: A new tool to parameterize tree radial growth based on climate conditions

被引:81
作者
Shishov, Vladimir V. [1 ]
Tychkov, Ivan I. [1 ]
Popkova, Margarita I. [1 ]
Ilyin, Victor A. [1 ]
Bryukhanova, Marina V. [2 ]
Kirdyanov, Alexander V. [1 ,2 ]
机构
[1] Siberian Fed Univ, Math Methods & IT Dept, Krasnoyarsk 660075, Russia
[2] VN Sukachev Inst Forest SB RAS, Lab Tree Ring Struct, Krasnoyarsk 660036, Russia
基金
俄罗斯科学基金会;
关键词
VS-model; Parameterization; VS-oscilloscope; Central Siberia; Permafrost; Tree-ring width; Tree-ring growth; Climate signal; Non-linear response; Tree-ring growth rates; Larch; Spruce; RING WIDTH; CENTRAL SIBERIA; LARIX-GMELINII; TEMPERATURE; VARIABILITY; XYLOGENESIS; PATTERNS; NORTH; LARCH; MODEL;
D O I
10.1016/j.dendro.2015.10.001
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
It is generally assumed in dendroecological studies that annual tree-ring growth is adequately determined by a linear function of local or regional precipitation and temperature with a set of coefficients that are temporally invariant. However, various researchers have maintained that tree-ring records are the result of multivariate, often nonlinear biological and physical processes. To describe critical processes linking climate variables with tree-ring formation, the process-based tree-ring Vaganov-Shashkin model (VS-model) was successfully used. However, the VS-model is a complex tool requiring a considerable number of model parameters that should be re-estimated for each forest stand. Here we present a new visual approach of process-based tree-ring model parameterization (the so-called VS-oscilloscope) which allows the simulation of tree-ring growth and can,be easily used by researchers and students. The VS-oscilloscope was tested on tree-ring data for two species (Larix gmeliniiand Picea obovata) growing in the permafrost zone of Central Siberia. The parameterization of the VS-model provided highly significant positive correlations (p < 0.0001) between simulated growth curves and original tree-ring chronologies for the period 1950-2009. The model outputs have shown differences in seasonal tree-ring growth between species that were well supported by the field observations. To better understand seasonal tree-ring growth and to verify the VS-model findings, a multi-year natural field study is needed, including seasonal observation of the thermo-hydrological regime of the soil, duration and rate of tracheid development, as well as measurements of their anatomical features. (C) 2015 Elsevier GmbH. All rights reserved.
引用
收藏
页码:42 / 50
页数:9
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