Olsson Cecilia, Olin Stefan, Lindström Johan, Jönsson Anna Maria
Department of Physical Geography and Ecosystem Science Lund University Lund Sweden.
Centre for Mathematical Sciences Lund University Lund Sweden.
Ecol Evol. 2017 Oct 22;7(23):9954-9969. doi: 10.1002/ece3.3476. eCollection 2017 Dec.
Budburst is regulated by temperature conditions, and a warming climate is associated with earlier budburst. A range of phenology models has been developed to assess climate change effects, and they tend to produce different results. This is mainly caused by different model representations of tree physiology processes, selection of observational data for model parameterization, and selection of climate model data to generate future projections. In this study, we applied (i) Bayesian inference to estimate model parameter values to address uncertainties associated with selection of observational data, (ii) selection of climate model data representative of a larger dataset, and (iii) ensembles modeling over multiple initial conditions, model classes, model parameterizations, and boundary conditions to generate future projections and uncertainty estimates. The ensemble projection indicated that the budburst of Norway spruce in northern Europe will on average take place 10.2 ± 3.7 days earlier in 2051-2080 than in 1971-2000, given climate conditions corresponding to RCP 8.5. Three provenances were assessed separately (one early and two late), and the projections indicated that the relationship among provenance will remain also in a warmer climate. Structurally complex models were more likely to fail predicting budburst for some combinations of site and year than simple models. However, they contributed to the overall picture of current understanding of climate impacts on tree phenology by capturing additional aspects of temperature response, for example, chilling. Model parameterizations based on single sites were more likely to result in model failure than parameterizations based on multiple sites, highlighting that the model parameterization is sensitive to initial conditions and may not perform well under other climate conditions, whether the change is due to a shift in space or over time. By addressing a range of uncertainties, this study showed that ensemble modeling provides a more robust impact assessment than would a single phenology model run.
芽萌动受温度条件调控,气候变暖与更早的芽萌动相关。已开发出一系列物候模型来评估气候变化影响,且这些模型往往会产生不同结果。这主要是由树木生理过程的不同模型表示、用于模型参数化的观测数据选择以及用于生成未来预测的气候模型数据选择导致的。在本研究中,我们应用:(i)贝叶斯推断来估计模型参数值,以解决与观测数据选择相关的不确定性;(ii)选择代表更大数据集的气候模型数据;以及(iii)在多个初始条件、模型类别、模型参数化和边界条件上进行集合建模,以生成未来预测和不确定性估计。集合预测表明,在代表RCP 8.5的气候条件下,北欧挪威云杉的芽萌动在2051 - 2080年将比1971 - 2000年平均提前10.2 ± 3.7天。分别评估了三个种源(一个早期种源和两个晚期种源),预测表明种源之间的关系在气候变暖时也将保持。与简单模型相比,结构复杂的模型在某些地点和年份的组合中更有可能无法预测芽萌动。然而,它们通过捕捉温度响应的其他方面(例如低温需求),为当前对气候对树木物候影响的理解全貌做出了贡献。基于单个地点的模型参数化比基于多个地点的参数化更有可能导致模型失败,这突出表明模型参数化对初始条件敏感,并且在其他气候条件下可能表现不佳,无论这种变化是由于空间转移还是随时间变化。通过解决一系列不确定性,本研究表明集合建模比单个物候模型运行提供了更稳健的影响评估。