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A parameterization of leaf phenology for the terrestrial ecosystem component of climate models

机译:气候模式中陆地生态系统组成部分的叶片物候参数化

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摘要

Leaf phenology remains one of the most difficult processes to parameterize in terrestrial ecosystem models because our understanding of the physical processes that initiate leaf onset and senescence is incomplete. While progress has been made at the molecular level, for example by identifying genes that are associated with senescence and flowering for selected plant species, a picture of the processes controlling leaf phenology is only beginning to emerge. A variety of empirical formulations have been used with varying degrees of success in terrestrial ecosystem models for both extratropical and tropical biomes. For instance, the use of growing degree-days (GDDs) to initiate leaf onset has received considerable recognition and this approach is used in a number of models. There are, however, limitations when using GDDs and other empirically based formulations in global transient climate change simulations.The phenology scheme developed for the Canadian Terrestrial Ecosystem Model (CTEM), designed for inclusion in the Canadian Centre for Climate Modelling and Analysis coupled general circulation model, is described. The representation of leaf phenology is general enough to be applied over the globe and sufficiently robust for use in transient climate change simulations. Leaf phenology is functionally related to the (possibly changing) climate state and to atmospheric composition rather than to geographical boundaries or controls implicitly based on current climate. In this approach, phenology is controlled by environmental conditions as they affect the carbon balance. A carbon-gain-based scheme initiates leaf onset when it is beneficial for the plant, in carbon terms, to produce new leaves. Leaf offset is initiated by unfavourable environmental conditions that incur carbon losses and these include shorter day length, cooler temperatures, and dry soil moisture conditions. The comparison of simulated leaf onset and offset times with observation-based estimates for temperate and boreal deciduous, tropical evergreen, and tropical deciduous plant functional types at selected locations indicates that the phenology scheme performs satisfactorily. Model simulated leaf area index and stem and root biomass are also compared with observational estimates to illustrate the performance of CTEM.
机译:叶片物候学仍然是陆地生态系统模型中最难参数化的过程之一,因为我们对引发叶片发作和衰老的物理过程的理解还不完整。虽然已经在分子水平上取得了进展,例如通过鉴定与选定植物物种的衰老和开花相关的基因,但控制叶片物候的过程才刚刚开始。在热带生态系统和热带生物群落的陆地生态系统模型中,已经使用了各种经验公式,并取得了不同程度的成功。例如,使用生长日数(GDD)来启动叶片发作已获得相当多的认可,并且该方法已在许多模型中使用。但是,在全球瞬态气候变化模拟中使用GDD和其他基于经验的公式时存在局限性。为加拿大陆地生态系统模型(CTEM)开发的物候方案设计为包含在加拿大气候建模与分析中心耦合的普通循环中模型,进行描述。叶片物候学的表示法已经足够广泛地应用到全球各地,并且足够健壮,可用于瞬时气候变化模拟。叶片物候学在功能上与(可能正在变化的)气候状态和大气成分有关,而不是与地理边界或基于当前气候隐含的控制有关。在这种方法中,物候受环境条件的控制,因为它们会影响碳平衡。当以碳为单位对植物有利于产生新的叶子时,基于碳的获取方案会启动叶子发作。叶片偏移是由不利的环境条件引起的,该环境条件导致碳损失,其中包括较短的日长,较低的温度和干燥的土壤湿度条件。将模拟的叶片起伏和偏移时间与在选定位置的温带和寒带落叶,热带常绿和热带落叶植物功能类型的基于观测的估计值进行比较,表明物候方案表现令人满意。模型模拟叶面积指数,茎和根生物量也与观测值进行了比较,以说明CTEM的性能。

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