Changing land-atmosphere interactions in Arctic tundra

北极苔原不断变化的陆地-大气相互作用

• 批准号: RGPIN-2018-05308
• 负责人: Humphreys, Elyn
• 金额: $ 6.27万
• 依托单位: Carleton University
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2022
• 资助国家: 加拿大
• 起止时间: 2022-01-01 至 2023-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=754910
• 关键词: Changing; land; atmosphere; interactions; Arctic

Climate change is impacting the Arctic's vast and varied terrestrial landscape. Disturbances such as fire, herbivory, and long-term warming are restructuring plant communities and changing how much and when water, energy and carbon flows between Arctic tundra and the atmosphere. This is especially concerning as Arctic soils with permafrost are huge reservoirs of carbon. The proposed research addresses the critical question are the ongoing changes in the Arctic tundra accelerating or mitigating climate warming? Field research at the Daring Lake Tundra Ecosystem Research Station will measure year-round carbon dioxide and methane exchange between four different tundra ecosystems and the atmosphere over the next five years. This will allow us for the first time to evaluate the annual carbon sink/source strength of these ecosystems and the importance of fall, winter and spring carbon and water cycling. Our long record of growing season fluxes shows this tundra is a substantial sink for carbon dioxide, especially with greater shrub cover, which is encroaching onto tundra regions across the Arctic. However, it is likely much of the carbon gained in summer will be lost through decomposition throughout the remaining months of the year. We will identify the factors which influence these losses of carbon, the age of this carbon and how much of it leaves as carbon dioxide, as methane, and as dissolved carbon in spring when snowmelt saturates the tundra. Finally, the data we collect and what we learn with this research will be used to continue to develop a land surface model. This model is used in the family of Canadian Climate Models and Earth System Models, which will help improve Canada's climate projections on both national and regional scales.

气候变化正在影响北极广阔多样的陆地景观。火灾、食草动物和长期变暖等干扰正在重组植物群落，并改变水、能源和碳在北极苔原和大气之间流动的数量和时间。这尤其令人担忧，因为北极的永久冻土土壤是巨大的碳库。拟议的研究解决了一个关键问题：北极苔原的持续变化是加速还是减缓气候变暖？达令湖苔原生态系统研究站的实地研究将测量未来五年四种不同苔原生态系统与大气之间的全年二氧化碳和甲烷交换。这将使我们能够首次评估这些生态系统的年度碳汇/源强度以及秋季、冬季和春季碳和水循环的重要性。我们对生长季节通量的长期记录表明，这片苔原是二氧化碳的重要汇，特别是在灌木覆盖范围更大的情况下，它正在侵蚀整个北极的苔原地区。然而，夏季获得的大部分碳可能会在一年中剩余的几个月中通过分解而损失掉。我们将确定影响这些碳损失的因素、这些碳的年龄以及其中有多少以二氧化碳、甲烷和春季融雪饱和苔原时溶解的碳的形式离开。最后，我们收集的数据和我们在这项研究中学到的知识将用于继续开发地表模型。该模型用于加拿大气候模型和地球系统模型系列，这将有助于改善加拿大在国家和区域尺度上的气候预测。