Department of Forest Yield and Silviculture, Slovenian Forestry Institute, Večna pot 2, 1000, Ljubljana, Slovenia.
Laboratory for Integral Studies of Forest Dynamics of Eurasia, Siberian Federal University, Akademgorodok St., 50/2, Krasnoyarsk, Russia, 660075.
Int J Biometeorol. 2021 Feb;65(2):311-324. doi: 10.1007/s00484-020-02033-5. Epub 2020 Oct 16.
Norway spruce (Picea abies L.) is among the most sensitive coniferous species to ongoing climate change. However, previous studies on its growth response to increasing temperatures have yielded contrasting results (from stimulation to suppression), suggesting highly site-specific responses. Here, we present the first study that applies two independent approaches, i.e. the nonlinear, process-based Vaganov-Shashkin (VS) model and linear daily response functions. Data were collected at twelve sites in Slovenia differing in climate regimes and ranging elevation between 170 and 1300 m a.s.l. VS model results revealed that drier Norway spruce sites at lower elevations are mostly moisture limited, while moist high-elevation sites are generally more temperature limited. Daily response functions match well the pattern of growth-limiting factors from the VS model and further explain the effect of climate on radial growth: prevailing growth-limiting factors correspond to the climate variable with higher correlations. Radial growth correlates negatively with rising summer temperature and positively with higher spring precipitation. The opposite response was observed for the wettest site at the highest elevation, which positively reacts to increased summer temperature and will most likely benefit from a warming climate. For all other sites, the future radial growth of Norway spruce largely depends on the balance between spring precipitation and summer temperature.
挪威云杉(Picea abies L.)是对正在发生的气候变化最敏感的针叶树种之一。然而,先前关于其生长对气温升高反应的研究结果却存在差异(从刺激到抑制),表明其具有高度特定地点的反应。在这里,我们首次提出了应用两种独立方法的研究,即非线性、基于过程的 Vaganov-Shashkin(VS)模型和线性日响应函数。这些数据是在斯洛文尼亚的 12 个地点收集的,这些地点的气候条件和海拔高度在 170 到 1300 米之间存在差异。VS 模型的结果表明,海拔较低、干燥的挪威云杉地点主要受到水分限制,而湿润的高海拔地点通常受到温度限制。日响应函数与 VS 模型的生长限制因素模式非常吻合,并进一步解释了气候对径向生长的影响:主要的生长限制因素与相关性更高的气候变量相对应。径向生长与夏季气温升高呈负相关,与春季降水增加呈正相关。在海拔最高的最潮湿地点观察到了相反的反应,该地点对夏季气温升高呈正反应,很可能受益于气候变暖。对于所有其他地点,挪威云杉未来的径向生长在很大程度上取决于春季降水和夏季温度之间的平衡。