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风对林木的影响 总被引：7，自引：0，他引：7
风除对森林造成了危害外,还对树木的生长、形态以及森林生态等产生影响。随着全球气候变化的发展,更多和更强的暴风出现的危险性日益增加。为了更好地理解风害对树木、林分和森林生态系统的影响,为森林经营管理提供依据,本文对近10年来国际上有关风对林木影响内容进行归纳总结。结果表明,风对林木影响的研究主要在以下几个方面取得了重要的进展：1)风与林木的空气动力学关系;2)树木在风力荷载下其适应性的生长机理;3)树木对风的生理响应：4)森林风害的危险评估。所有这些研究大都在人工用材林中进行的。此外,本文还介绍了该研究领域需要开展的其它研究,如1)天然林或天然次生林的风害研究;2)风害形成的林窗和森林动态研究;3)风害对森林生态主要过程的影响研究;4)．风害与森林管理研究。图3参61。 相似文献
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在当代林学理论与实践中,十分强调树种的综合评定和系统方法;这对林木遗传与选种、林木良种繁育、引种和造林尤为重要。 在森林的活动中,气候、土壤、地形、地质结构组成,常常影响森林的形成、森林的生产力和森林的质量。同时,树种的生物学特性,树种彼此间及它们与周围环境条件存在着复杂关系。但不能忽视人为因素以及对相应的生长条件和森林类型营建高产林分起主导作用的经济因素。 每个被定名的种群不必划分成更小的构成单位,因为这些种群群体能够总体有机地反映出对树木生长发育的影响。同样,通过人为活动也能改变有关的周围环境条件,但最终起决定作用的还是树木本身的生物学特性。因此,为了提高林分生产力,改善林分的质量成分,应该采用综合方法研究森林的生命、生长发育和生长规律。 目前在评定某个或另一个森林树种或树木,或评定种子繁育场的无性系时,已不满足于只了解1～2种性状,如树高和胸径。通过林业生产实践和科学研究可知,在林木选种、良种繁育,引种和造林时,除了用已规定的指标评定外,还广泛用树木地上部分和地下部份的生物量(气干或绝对干重),主根和针叶的长度,树冠的结构和冠 相似文献
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陈森 《中南林业调查规划》1989,(3)
森林是大量树木的集合,森林生长量是这些树木生长量的统计值。而林木生长受到树种生物学特性、树木年龄、立地条件、人为活动、经营措施等因素的制约,且森林分布广,生长周期长等特点,使得森林生长量调查错综复杂。研究并掌握林木的生长规律,从而采取相应的经营措施,改善生长状况,提高生长量,达到速生丰产、永续经营。所以,对林木和林分进行生长量测定,分析研究其变化规律,在林业生产上有着重要意义。 相似文献
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3.生长伐。生长伐林木的七种类型。一必须采伐其他用途的森林（如开矿,修建水库、公路,建立工业企业,种植农业和林业作物等）;二根据可行性技术研究或主管部门批准的项目,要采伐低产量的退化林并重新种植更高产的树木； 相似文献
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森林生态系统林木生长与耗水研究进展 总被引：1，自引：0，他引：1
张晓宇 《内蒙古林业调查设计》2018,(1):95-97
森林生态系统林木的生长和耗水是森林水分利用的研究重点,对当前推进节水林发展、抗旱树种筛选具有重要意义。文章对森林生态系统林木生长的研究方法进行了综述,指出常见的林木生长方法有普通测定法、年轮法、树木径向变化记录仪等,并对3个林木生长模型(全林分模型、径阶分布模型、单木生长模型)的优劣和使用范围进行了比较;从叶片尺度、单株尺度、林分尺度和区域尺度分别比较了林木耗水方法的差异和优劣。通过综述,确定各方法的优劣和使用范围,以更好的指导科学实验,得出精确结果。 相似文献
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Dario Martin-Benito Vincent KintMiren del Río Bart MuysIsabel Cañellas 《Forest Ecology and Management》2011,262(6):1030-1040
Positive and negative effects of climate change on forest growth have been observed in different parts of the world. However, much is still unknown about how forest structure and productivity might affect climate-growth relationships in the future. We examined the effects of climate, site quality, and competition on tree basal area growth of black pine (Pinus nigra Arn.) between 1964 and 2005 in 21 sites in the Iberian Peninsula. We used a new approach to simultaneously account for climate-growth relationships, inter-annual growth variability, and stand structural changes, by fitting a linear mixed effects model (LMEM) for basal area increments (BAI) using climate data, tree-ring chronologies, and repeated forest inventory data. This approach showed the potential to improve our understanding of climate effects on tree growth and to include climate in empirical forest growth models. We used the LMEM to make projections of BAI growth under two CO2 emission scenarios and two global circulation models (GCM). The main climate drivers for growth were precipitation from previous autumn to summer and winter temperature with a positive effect, and temperature in spring-summer which had a negative effect. Tree response to climate was modulated by stand conditions, tree competition, and productivity. The more productive stands showed greater ability to either maintain or increase growth at warmer spring-summer temperatures under different levels of autumn-summer precipitation. Growth projections showed important regional differences. In general, growth under future climate is predicted to decrease although moderate growth increases might be expected in the northern region for highly and moderately productive stands. 相似文献
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气候变化情景下河北省3个优势树种适宜分布区预测 总被引：2，自引：0，他引：2
【目的】探究河北省3个优势树种分布与气候因子的关系,并进行适宜分布区预测,以期为评估气候变化的影响及制定适宜未来气候变化的森林经营策略提供理论依据。【方法】依据河北省森林资源调查数据,选取华北落叶松、蒙古栎和油松这3个主要树种,采用ClimateAP气候模型生成当前及未来(2040—2069年和2070—2099年)与降水和温度相关的10个气候因子,利用MaxEnt生态位模型和基于3个气候变化情景(温室气体最低排放,RCP2.6;中度稳定排放,RCP4.5;高度排放,RCP8.5)的一致性预测,模拟3个树种当前和未来的潜在适宜分布区,并采取响应曲线分析主要气候因子对3个树种适宜分布区的影响。【结果】3个树种MaxEnt模型的受试者工作特征曲线下面积(AUC值)都大于0.85,具有较好的预测能力;当前3个树种主要适宜分布在燕山和太行山地区;影响3个树种分布的主导气候因子存在差异,华北落叶松主要受小于0℃年积温和湿季降水量的影响,蒙古栎则主要受最热月平均气温、Hargreaves水分亏缺和湿季降水量的影响,而最热月平均气温、湿季降水量、大于5℃年积温和年均气温是影响油松分布的主要气候因子;一致性预测表明,在2040—2069年,河北省华北落叶松分布面积明显扩大,蒙古栎分布面积变化较小,而油松分布面积显著缩小;在2070—2099年,3个树种的适宜分布面积都显著缩小,幅度均超过3%。【结论】随着气候变化,3个树种均有向高海拔地区迁移的趋势,但在经纬度方向上的分布变化不大。在未来3个树种的适宜分布区,采取人工手段(如造林)辅助树种扩散以适应气候变化,有利于提高森林生产力,构建健康稳定的森林生态系统。 相似文献
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We analyzed tree rings over the past 100 years to understand the response of Quercus ilex L. to climate change at four different sites along a temperature gradient in a highly anthropogenically transformed ecosystem. To test the hypothesis of a climate change related decrease in productivity at warmer sites, we discuss the effect of historical management on the growth of forest stands and the spatio-temporal variability of growth in response to climate, analyzing departures from linearity in that relationship. We reconstructed stand history and investigated past growth trends using tree-rings. Then we used a dendroecological approach to study the regional, local and age-dependent response to climate, analyzing the relationship between precipitation and tree growth using non-linear mixed models. Tree rings reflected the origin of the studied landscape, mainly a simplification of an original closed forest and progressive canopy opening for agrosilvopastoral purposes after the mid 1800s. As expected, trees were principally responding to water availability, and regional growth (as expressed by the first principal component from the matrix of chronologies) was highly responsive to hydrological year precipitation (r = 0.7). In this water limited ecosystem, the response of growth to precipitation was asymptotic and independent of age, but variable in time. Maximum growth was variable at the different sites and the non-linear function of growth saturated (i.e. reached an asymptote) at temperature dependent site specific precipitation levels within the range considered in the region to lead a shift towards deciduous species dominated woodlands (around 600 mm, variable with mean temperature). Only trees at warmer sites showed symptoms of growth decline, most likely explained by water stress increase in the last decades affecting the highly transformed open (i.e. low competition) tree structure. Stands at colder locations did not show any negative growth trend and may benefit from the current increase in winter temperatures. Coinciding with the decrease in productivity, trees at warmer sites responded more to moisture availability, exhibited a slower response to precipitation and reached maximum growth at higher precipitation levels than trees at colder sites. This suggests that warmer stands are threatened by climate change. The non-linear response of growth to precipitation described is meaningful for different ecological applications and provides new insights in the way trees respond to climate. 相似文献
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Larix olgensis is a dominant tree species in the forest ecosystems of the Changbai Mountains of northeast China.To assess the growth response of this species to global climate change,we developed three tree-ring width and biomass chronologies across a range of elevations in the subalpine forests on the eastern slope of the Changbai Mountains.We used dendroclimatic analyses to study key factors limiting radial growth in L.olgensis and its variation with elevation.The statistical characteristics of chronologies suggested that elevation is a determinant of tree growth patterns in the study area.Response function analysis of chronologies with climate factors indicated that climate–growth relationships changed with increasing elevation:tree growth at high elevation was strongly limited by June temperatures of the previous year,and as elevation decreases,the importance of temperature decreased;tree radial growth at mid-elevation was mainly controlled by precipitation towards the end of the growing season of the current year.Biomass chronologies reflected a stronger climatic signal than tree-ring width chronologies.Spatial correlation with gridded climate data revealed that our chronologies contained a strong regional temperature signal for northeast China.Trees growing below timberline appeared to be more sensitive to climate,thus optimal sites for examining growth trends as a function of climate variation are considered to be just below timberline.Our study objective was to provide information for more accurate prediction of the growth response of L.olgensis to future climate change on the eastern slope of the Changbai Mountains,and to provide information for future climate reconstructions using this tree species in humid and semi humid regions. 相似文献
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Dapao Yu Qingwei Wang Yue Wang Wangming Zhou Hong Ding Xiangmin Fang Shenwei Jiang Limin Dai 《Annals of Forest Science》2011,68(5):921-933
? Introduction
Information on spatial variability in tree radial growth is essential for improving predictions of forest ecosystem responses to climate change. To date, researchers have designed models to simulate the potential distribution area of major forest types under different climate change scenarios in Northeast China, but little is known about the spatial variability of tree growth in response to climate.? Materials and methods
We used a dendroecological technique to examine the climate–growth relationship of six dominant tree species on seven sites varying in altitude on Changbai Mountain in Northeast China, to explore whether the spatial variability of tree growth is an indicator of regional climatic forces, and whether simulation results generated by models can accurately reflect this in tree radial growth.? Results
Fifteen site-specific species can be distinguished species at or near their upper limit distribution from those at the lower distributions. Species differences were more important than altitude differences in influencing species’ site-specific radial growth. Precipitation, temperature, and soil moisture together constitute the major factors limiting tree radial growth.? Conclusion
We found the distribution area of dominant tree species on Changbai Mountain will shift upward; growth of Korean pine will not decline at its lower limit of distribution and will not eventually even disappear from forest communities in those areas. 相似文献17.
Bruno Vila Michel Vennetier Christian Ripert Olivier Chandioux Eryuan Liang Frédéric Guibal Franck Torre 《Annals of Forest Science》2008,65(7):709-709
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【目的】探讨川西亚高山地区各海拔生境处岷江冷杉和紫果云杉径向生长对气候因子的响应,为进一步揭示当地森林对气候变化的响应机制提供依据。【方法】分别获取王朗自然保护区中海拔与高海拔生境处岷江冷杉和紫果云杉的标准年表,分析年表同气候因子间的关系。【结果】中海拔生境处岷江冷杉生长在1990年后与年均气温存在一定程度的“分离效应”;中海拔生境处岷江冷杉和紫果云杉生长与上年生长季(上年7月和8月)气温和上年生长季末(上年10月)降水量显著负相关( P <0.05),岷江冷杉生长与当年9月气温和降水量显著负相关( P <0.05),紫果云杉生长与当年2、6月月均最低气温显著正相关( P <0.05);高海拔生境处岷江冷杉和紫果云杉生长均与当年生长季前(上年11月、当年1月、当年2月)、当年生长季(当年7月)和上年生长季(上年6月)气温显著正相关( P <0.05),岷江冷杉生长还与当年6月份的降水量及上年8月份的气温显著负相关( P <0.05);滑动相关分析和年表特征年气候分析结果充分印证了各年表对月气候因子响应的可靠性。【结论】上年生长季气温的“滞后效应”对中海拔生境处的岷江冷杉、紫果云杉以及高海拔生境处的岷江冷杉生长均有显著影响;近几十年来,上年生长季末降水对中海拔生境处的岷江冷杉、紫果云杉以及高海拔生境处的紫果云杉生长都具有稳定而显著的抑制作用。 相似文献
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Xiongwen Chen 《Journal of Sustainable Forestry》2019,38(1):54-67
Integrated analysis of forest dynamics under both anthropogenic influence and climatic change is crucial to indicating emergent patterns and meeting objectives of climate change mitigation. In this study, a long-term forest inventory data (1960s-2010s) in Alabama, USA were analyzed for patterns in relation to human activities and climate fluctuation. The results indicated that the species (or species groups) composition in Alabama’s forests was significantly different between all reported times, except for 2012–2015 based on Simpson’s index. Eastern hemlock trees declined dramatically. The overall forest communities became less homogeneous. Positive or negative correlation existed in the abundance of many species. The distribution of tree abundance along diameters for tree species followed exponential models. Both annual tree mortality and net growth rate increased from the 1960s. The total volume of growing stock increased from 14.4 million cubic feet in 1963 to 39.5 million cubic feet in 2016. The average volume of growing stock per acre also increased linearly with annual average air temperature, but not with annual precipitation. Based on the patterns of Alabama’s forests under climate fluctuation and human activities, some suggestions on developing strategies for the sustainability of Alabama forest were discussed. 相似文献
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IntroductionItissurethatpresentelevatiollsofCO2a11dotllergrcc11-housegasesinducedbyhumanactivitiesaren1akli1gglobalclimategothroughinexperielICedcl1anges(Scl1le-subgerl987).Thecurrentquasi-equilibriulllstatesofbio-sphereecosystCm,esPeciallyterrestrialecosystems,wouldbebrokenbecausetl1estructure,fu11ction,distributio11andtlledynamicsofanyexistedecosystemsareIberesultsoflongtermadaptationofbio-systemtocurrentclin1ate.Theec()systemsdistributedinhighlatitlldeareawouldhavemuchbiggerchai1ge(Bona… 相似文献