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首页> 外文期刊>Global change biology >Emergent climate and CO2 sensitivities of net primary productivity in ecosystem models do not agree with empirical data in temperate forests of eastern North America
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Emergent climate and CO2 sensitivities of net primary productivity in ecosystem models do not agree with empirical data in temperate forests of eastern North America

机译:生态系统模型中净初级生产率的紧急气候和二氧化碳敏感性不同意北美东部温带森林的经验数据

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Ecosystem models show divergent responses of the terrestrial carbon cycle to global change over the next century. Individual model evaluation and multimodel comparisons with data have largely focused on individual processes at subannual to decadal scales. Thus far, data-based evaluations of emergent ecosystem responses to climate and CO2 at multidecadal and centennial timescales have been rare. We compared the sensitivity of net primary productivity (NPP) to temperature, precipitation, and CO2 in ten ecosystem models with the sensitivities found in tree-ring reconstructions of NPP and raw ring-width series at six temperate forest sites. These model-data comparisons were evaluated at three temporal extents to determine whether the rapid, directional changes in temperature and CO2 in the recent past skew our observed responses to multiple drivers of change. All models tested here were more sensitive to low growing season precipitation than tree-ring NPP and ring widths in the past 30 years, although some model precipitation responses were more consistent with tree rings when evaluated over a full century. Similarly, all models had negative or no response to warm-growing season temperatures, while tree-ring data showed consistently positive effects of temperature. Although precipitation responses were least consistent among models, differences among models to CO2 drive divergence and ensemble uncertainty in relative change in NPP over the past century. Changes in forest composition within models had no effect on climate or CO2 sensitivity. Fire in model simulations reduced model sensitivity to climate and CO2, but only over the course of multiple centuries. Formal evaluation of emergent model behavior at multidecadal and multicentennial timescales is essential to reconciling model projections with observed ecosystem responses to past climate change. Future evaluation should focus on improved representation of disturbance and biomass change as well as the feedbacks with moisture balance and CO2 in individual models.
机译:生态系统模型显示了下个世纪陆地碳循环对全球变化的发散回应。具有数据的个人模型评估和多模型比较主要集中在贱民以外的单个过程上。到目前为止,基于数据的基于数据对气候和CO2的基于数据的评估,并且是百年期间的群体的答复。我们将净初级生产率(NPP)的敏感性与在六个温带森林地点的NPP和原始环形宽度系列中的树木重建中发现的敏感性。这些模型数据比较在三个时间范围内进行评估,以确定最近过去的温度和CO2的快速,定向变化,我们观察到对多个变革驱动程序的响应。在过去30年中,此处测试的所有模型对低生长季节降水量比树木NPP和环宽度更敏感,尽管在全世纪评估时,某些模型降水应答与树圈更加一致。同样,所有模型都对温暖的季节温度产生负面或没有反应,而树木数据显示出温度的始终如一的积极作用。虽然降水反应在模型中最不一致,但在过去的世纪中,模型的模型与CO2驱动分歧的差异和集成不确定性。模型内森林成分的变化对气候或二氧化碳敏感性没有影响。模型模拟中的火灾减少了对气候和二氧化碳的模型敏感性,但只在多个世纪的过程中。 Multimecadal和多期间时间表的紧急模型行为进行正式评估对于调和模型预测与观察到的生态系统对过去的气候变化进行调整。未来的评估应专注于改善干扰和生物质变化的表现,以及各个模型中的水分平衡和二氧化碳的反馈。

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