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首页> 外文期刊>Лесной журнал >LONG-TERM GROWTH TRENDS ANALYSIS OF NORWAY SPRUCE STANDS IN RELATION TO POSSIBLE CLIMATE CHANGE: CASE STUDY OF LENINGRAD REGION
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LONG-TERM GROWTH TRENDS ANALYSIS OF NORWAY SPRUCE STANDS IN RELATION TO POSSIBLE CLIMATE CHANGE: CASE STUDY OF LENINGRAD REGION

机译:挪威云杉的长期增长趋势分析与可能的气候变化有关:列宁格勒地区的案例研究

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摘要

The Lisino training and experimental forest of the Saint-Petersburg State Forest Technical University was chosen as a study area. The forest is located in the central part of the Leningrad region and has a high level of protection as a forest of scientific and historical value. According to the official data, mean annual temperature in the region increased by 0.6 °C within 10 years as well as precipitation. The impact determination of changing climate conditions on Norway spruce trees growth was theaim of this study. Three most representative compartments dominated by Norway spruce {Picea abies (L.) Karst.) were selected for data collection. Core samples were taken by the Pressler increment borer from 107 dominant trees while climatic data were obtained from the nearest weather stations. Tree rings were measured and analyzed using WinDendro software while climate data were processed by Microsoft Excel. Tree ring data cover the time interval from 1848 to 2011, each ring was characterized by width,calendar year, age and diameter of the tree. Radial growth was analyzed within age and diameter classes. Annual rings widths were varied from 0.1 to 6 mm. There was a positive trend in age classes of 0-20, 21-40 and 41-60 years old. The growth was veryslow in the age classes of 61-80, 81-100 and >100. Diameters are larger in the age classes of 20-40 and 41-60 as compare to the local diameter growth table which was developed in the 19th century. Diameters for age classes older than 41-60 years were less than prescribed by the diameter growth table. Annual rings width for all age classes also demonstrate cyclic dynamics, moreover, the decline in growth sometimes occurred in recent decades. Multiple regression was used for developing the response function of growth to changes in climatic conditions. There was revealed a high correlation (90 %) and low influence of vegetation period climate data on growth during 1848-2011 (0.08102 mm/°C and 0.00085 mm/mm). Likewise, analysis shows that growth is higherin young and middle-aged than mature and over mature stands. Overall, climate change impact has a positive effect on the radial growth of Norway spruce for the studied area, however, not for all age and diameter classes.
机译:选择了圣彼得堡州林业技术大学的丽溪培训和实验森林作为研究区。森林位于列宁格勒地区的中心部分,并具有高度保护,作为科学和历史价值的森林。根据官方数据,该地区的平均温度在10年内增加0.6°C以及降水量。改变挪威云杉树木增长的气候条件的影响决定是本研究的胫骨。由挪威云杉统治的三个最具代表性的隔间{Picea Abies(L.)喀斯特。)被选为数据收集。核心样本由来自107个显性树木的压力机增量挖掘机拍摄,而从最近的气象站获得气候数据。测量树圈并使用Windenro软件进行测量并分析,而Microsoft Excel处理气候数据。树环数据覆盖从1848年到2011年的时间间隔,每个环的特征在于宽度,日历年,年龄和直径的树木。在年龄和直径的课程内分析径向生长。年环宽度从0.1到6毫米变化。年龄阶级为0-20,21-40和41-60岁的正趋势。在61-80,81-100和> 100的年龄课程中的增长非常出现。直径在20-40和41-60的年龄等级中,与19世纪开发的局部直径增长表相比。年龄课程的直径超过41-60岁的直径比直径增长表规定。所有年龄课程的年环宽度也展示了循环动力学,而且,近几十年来的增长下降有时发生。使用多元回归用于在气候条件的变化中发展增长的响应函数。揭示了高相关(90%)和植被时期气候数据对1848 - 2011年增长的影响(0.08102mm /℃和0.00085mm / mm)。同样,分析表明,增长高于年轻人和中年比成熟和成熟的立场。总体而言,气候变化影响对学习区域的挪威云杉的径向增长产生了积极影响,但不适用于所有年龄和直径的课程。

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