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Effects of observed and experimental climate change on terrestrial ecosystems in northern Canada: results from the Canadian IPY program

机译:气候变化对加拿大北部陆地生态系统的影响:加拿大IPY计划的结果

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Tundra and taiga ecosystems comprise nearly 40% of the terrestrial landscapes of Canada. These permafrost ecosystems have supported humans for more than 4500 years, and are currently home to ca. 115,000 people, the majority of whom are First Nations, Inuit and Metis. The responses of these ecosystems to the regional warming over the past 30-50 years were the focus of four Canadian IPY projects. Northern residents and researchers reported changes in climate and weather patterns and noted shifts in vegetation and other environmental variables. In forest-tundra areas tree growth and reproductive effort correlated with temperature, but seedling establishment was often hindered by other factors resulting in site-specific responses. Increased shrub cover has occurred in sites across the Arctic at the plot and landscape scale, and this was supported by results from experimental warming. Experimental warming increased vegetation cover and nutrient availability in most tundra soils; however, resistance to warming was also found. Soil microbial diversity in tundra was no different than in other biomes, although there were shifts in mycorrhizal diversity in warming experiments. All sites measured were sinks for carbon during the growing season, with expected seasonal and latitudinal patterns. Modeled responses of a mesic tundra system to climate change showed that the sink status will likely continue for the next 50-100 years, after which these tundra systems will likely become a net source of carbon dioxide to the atmosphere. These IPY studies were the first comprehensive assessment of the state and change in Canadian northern terrestrial ecosystems and showed that the inherent variability in these systems is reflected in their site-specific responses to changes in climate. They also showed the importance of using local traditional knowledge and science, and provided extensive data sets, sites and researchers needed to study and manage the inevitable changes in the Canadian North.
机译:苔原和针叶林生态系统构成了加拿大近40%的陆地景观。这些多年冻土生态系统已经为人类提供了超过4500年的支持,并且目前是大约2000年的家园。 115,000人,其中大多数是原住民,因纽特人和梅蒂斯。这些生态系统对过去30至50年间区域变暖的响应是加拿大四个IPY项目的重点。北部居民和研究人员报告了气候和天气模式的变化,并注意到植被和其他环境变量的变化。在森林冻原地区,树木的生长和繁殖力与温度相关,但是幼苗的生长通常受到其他因素的阻碍,从而导致特定地点的反应。在该地块和景观范围内,整个北极地区的灌木丛增加了,这一点得到了实验变暖的支持。实验性增温增加了大多数苔原土壤的植被覆盖率和养分利用率;但是,还发现了对变暖的抵抗力。尽管变暖实验中的菌根多样性发生了变化,但苔原中的土壤微生物多样性与其他生物群落没有差异。在生长季节,所有测得的地点都是碳汇,具有预期的季节性和纬度模式。模拟的苔原苔原系统对气候变化的响应表明,下沉状态可能持续50-100年,此后这些苔原系统很可能成为大气中二氧化碳的净来源。这些IPY研究是对加拿大北部陆地生态系统状态和变化的首次全面评估,表明这些系统的固有变异性反映在它们对气候变化的特定地点响应中。他们还表明了利用当地传统知识和科学的重要性,并提供了广泛的数据集,站点和研究人员,以研究和管理加拿大北部不可避免的变化。

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