A Multivariate Regression Model to Explain the Altitudinal Distribution of Timberlines on the Eurasian Continent

IF 1.1 4区 生物学 Q3 PLANT SCIENCES Acta Societatis Botanicorum Poloniae Pub Date : 2022-08-15 DOI:10.5586/asbp.918
Fang Zhao, Abdul Shakoor, G. Zaib, Bai-ping Zhang, Xincan Lan, Jiale Tang
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Abstract

The altitude of alpine timberline elevation has been considered to correlate with certain climatic factors. Many related isotherms (e.g., warmest month 10 °C isotherm) have been proposed to explain the altitudinal distribution of alpine timberline at the global scale. However, any climatic index actually has a wide range at the alpine timberline position worldwide. The altitudinal position of the alpine timberline is related to far more than just one climatic factor. Therefore, we developed a multivariable model for timberline elevation variability by collecting data from 473 timberline sites on the Eurasian continent. We analyzed 12 climatic variables that potentially account for timberline variation. Principal component and regression analyses were used to mine four climatic variables. The mean temperature of the warmest month (MTWM), mean temperature of the coldest month (MTCM), climatic continentality (K), and annual precipitation (AP) explained 95% of the variability of timberline elevation. MTWM, MTCM, K, and AP contributed 18%, 41.28%, 34.9%, and 5.82%, respectively, to the altitudinal distribution of alpine timberline on the whole continent; 20%, 44%, 28.86%, and 7.14% in the eastern continent; and 17.71%, 39.79%, 40.21%, and 2.29% in the western continent. We showed that MTWM, MTCM, K, and AP are deterministic factors for the altitudinal distribution of alpine timberline in the Eurasian continent. MTCM and K contributed to explaining the altitudinal distribution of timberline both in the entire, eastern, and western parts of the Eurasian continent. Our research highlights the significance of MTCM for the altitudinal distribution of timberline.
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欧亚大陆树带线海拔分布的多元回归模型
高寒树带线海拔高度被认为与某些气候因子有关。许多相关的等温线(如最暖月10°C等温线)被提出来解释全球尺度上高山树带线的高度分布。然而,在世界范围内,任何气候指数实际上在高山树带线位置都有很大的变化范围。高山树带线的海拔位置与不止一种气候因素有关。因此,我们通过收集欧亚大陆473个树带线站点的数据,建立了一个多变量的树带线高程变化模型。我们分析了12个可能导致树带界线变化的气候变量。采用主成分分析和回归分析对四个气候变量进行了挖掘。最暖月平均温度(MTWM)、最冷月平均温度(MTCM)、气候大陆性(K)和年降水量(AP)解释了95%的林线高程变异。MTWM、MTCM、K和AP对全大陆高寒树带线海拔分布的贡献率分别为18%、41.28%、34.9%和5.82%;东部大陆分别为20%、44%、28.86%和7.14%;西部大陆分别为17.71%、39.79%、40.21%和2.29%。结果表明,MTWM、MTCM、K和AP是欧亚大陆高寒树带线高度分布的决定性因子。MTCM和K有助于解释欧亚大陆东部、西部和整个大陆的树带线高度分布。我们的研究强调了MTCM对树带线高度分布的重要意义。
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来源期刊
CiteScore
2.00
自引率
10.00%
发文量
18
审稿时长
1 months
期刊介绍: The journal has been published since 1923 and offers Open Access publication of original research papers, short communications, and reviews in all areas of plant science, including evolution, ecology, genetics, plant structure and development, physiology and biochemistry.
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