Harvey Jill E, Smiljanić Marko, Scharnweber Tobias, Buras Allan, Cedro Anna, Cruz-García Roberto, Drobyshev Igor, Janecka Karolina, Jansons Āris, Kaczka Ryszard, Klisz Marcin, Läänelaid Alar, Matisons Roberts, Muffler Lena, Sohar Kristina, Spyt Barbara, Stolz Juliane, van der Maaten Ernst, van der Maaten-Theunissen Marieke, Vitas Adomas, Weigel Robert, Kreyling Jürgen, Wilmking Martin
Institute of Botany and Landscape Ecology, University of Greifswald, Greifswald, Germany.
Natural Resources Canada, Canadian Forest Service, Northern Forestry Centre, Edmonton, AB, Canada.
Glob Chang Biol. 2020 Apr;26(4):2505-2518. doi: 10.1111/gcb.14966. Epub 2020 Jan 25.
The role of future forests in global biogeochemical cycles will depend on how different tree species respond to climate. Interpreting the response of forest growth to climate change requires an understanding of the temporal and spatial patterns of seasonal climatic influences on the growth of common tree species. We constructed a new network of 310 tree-ring width chronologies from three common tree species (Quercus robur, Pinus sylvestris and Fagus sylvatica) collected for different ecological, management and climate purposes in the south Baltic Sea region at the border of three bioclimatic zones (temperate continental, oceanic, southern boreal). The major climate factors (temperature, precipitation, drought) affecting tree growth at monthly and seasonal scales were identified. Our analysis documents that 20th century Scots pine and deciduous species growth is generally controlled by different climate parameters, and that summer moisture availability is increasingly important for the growth of deciduous species examined. We report changes in the influence of winter climate variables over the last decades, where a decreasing influence of late winter temperature on deciduous tree growth and an increasing influence of winter temperature on Scots pine growth was found. By comparing climate-growth responses for the 1943-1972 and 1973-2002 periods and characterizing site-level growth response stability, a descriptive application of spatial segregation analysis distinguished sites with stable responses to dominant climate parameters (northeast of the study region), and sites that collectively showed unstable responses to winter climate (southeast of the study region). The findings presented here highlight the temporally unstable and nonuniform responses of tree growth to climate variability, and that there are geographical coherent regions where these changes are similar. Considering continued climate change in the future, our results provide important regional perspectives on recent broad-scale climate-growth relationships for trees across the temperate to boreal forest transition around the south Baltic Sea.
未来森林在全球生物地球化学循环中的作用将取决于不同树种对气候的响应。解读森林生长对气候变化的响应需要了解季节性气候对常见树种生长影响的时空模式。我们构建了一个新的年轮宽度年表网络,该网络由310个年轮宽度年表组成,这些年表来自波罗的海南部地区(处于三个生物气候带——温带大陆性、海洋性、北方南部——的交界处)为不同生态、管理和气候目的收集的三种常见树种(欧洲栎、欧洲赤松和欧洲山毛榉)。确定了在月度和季节尺度上影响树木生长的主要气候因素(温度、降水、干旱)。我们的分析表明,20世纪苏格兰松和落叶树种的生长通常受不同气候参数控制,并且夏季水分供应对所研究的落叶树种生长越来越重要。我们报告了过去几十年冬季气候变量影响的变化,发现冬末温度对落叶树生长的影响在减弱,而冬季温度对苏格兰松生长的影响在增强。通过比较1943 - 1972年和1973 - 2002年期间气候 - 生长响应,并表征站点尺度的生长响应稳定性,空间隔离分析的描述性应用区分了对主要气候参数响应稳定的站点(研究区域东北部)和对冬季气候总体响应不稳定的站点(研究区域东南部)。此处呈现的研究结果突出了树木生长对气候变异性的时间上不稳定且不均匀的响应,并且存在这些变化相似的地理连贯区域。考虑到未来气候持续变化,我们的结果为波罗的海南部周边温带至北方森林过渡带树木近期的大规模气候 - 生长关系提供了重要的区域视角。