The Effects of Trees on Peatland Evapotranspiration Across Scales

树木对不同尺度泥炭地蒸散量的影响

• 批准号: RGPIN-2017-04182
• 负责人: Petrone, Richard
• 金额: $ 3.42万
• 依托单位: University of Waterloo
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2017
• 资助国家: 加拿大
• 起止时间: 2017-01-01 至 2018-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=633986
• 关键词: Effects; Trees; Peatland; Evapotranspiration; Across

The Western Boreal Plain (WBP) of Canada, provides important ecosystem services such as water and carbon storage and also represents a substantial component of Canada’s economic engine through its resource-based industries (mineral mining, forestry, oil and gas), the most significant of which is the oil sands development region. In the generally dry climate of the WBP, water availability is limited, making the peatlands that dominate this region vulnerable to climate variability as well as stresses from intense industrial pressures that affect peatland ecological and hydrological functioning. Understanding the internal and external ecohydrological and climatological processes that permit peatland ecosystems to efficiently use available moisture is important for managing these systems in light of climate and landuse change. The literature suggests that carbon, energy and water exchange can be strongly influenced by external local boundary layer conditions in addition to internal biophysical controls. However, little work has been done on peatlands in general and much of the research thus far has focused on bog ecosystems rather than fens in this climatically tenuous region. Internally, feedbacks exist between changes in surface cover, particularly tree density, soil conditions and evapotranspiration losses. Externally, the landscape mosaic of wetlands and forestlands suggests that not only do peatlands provide water to forested uplands, but that the forested uplands shelter peatlands, limiting evaporative losses. Understanding the mechanism of how peatlands protect themselves against moisture stress will refine our predictive capacity of how these systems will respond to climate change, as well as permit us to design more robust and resilient reclaimed systems.

加拿大的西部北方平原（WBP）提供重要的生态系统服务，如水和碳储存，也是加拿大经济引擎的重要组成部分，通过其资源型工业（采矿、林业、石油和天然气），其中最重要的是油砂开发区。在WBP普遍干燥的气候中，水的可用性是有限的，使得主导该地区的泥炭地容易受到气候变化的影响，以及来自影响泥炭地生态和水文功能的强烈工业压力的压力。了解内部和外部的生态水文和气候过程，使泥炭地生态系统有效地利用现有的水分是重要的管理这些系统的气候和土地利用变化。文献表明，碳，能量和水的交换可以强烈影响外部的局部边界层条件，除了内部的生物物理控制。然而，总体而言，对泥炭地的研究很少，迄今为止的大部分研究都集中在这个气候脆弱地区的沼泽生态系统而不是沼泽。从内部看，地表覆盖变化，特别是树木密度、土壤条件和蒸散量损失之间存在反馈。从外部看，湿地和林地的景观镶嵌图表明，泥炭地不仅为森林高地提供了水源，而且森林高地还保护了泥炭地，限制了蒸发损失。了解泥炭地如何保护自己免受水分胁迫的机制将提高我们对这些系统如何应对气候变化的预测能力，并使我们能够设计出更强大和更有弹性的再生系统。