Institute of Northern Engineering, Water & Environmental Research Center, University of Alaska, Fairbanks, AK, 99775-9500, USA.
Institute of Arctic Biology, University of Alaska, Fairbanks, AK, 99775-9500, USA.
Glob Chang Biol. 2016 Jan;22(1):208-19. doi: 10.1111/gcb.13058. Epub 2015 Nov 3.
Warming during the 20th century has changed the arctic landscape, including aspects of the hydrology, vegetation, permafrost, and glaciers, but effects on wildlife have been difficult to detect. The primary aim of this study is to examine the physical and biological processes contributing to the expanded riparian habitat and range of snowshoe hares (Lepus americanus) in northern Alaska. We explore linkages between components of the riparian ecosystem in Arctic Alaska since the 1960s, including seasonality of stream flow, air temperature, floodplain shrub habitat, and snowshoe hare distributions. Our analyses show that the peak discharge during spring snowmelt has occurred on average 3.4 days per decade earlier over the last 30 years and has contributed to a longer growing season in floodplain ecosystems. We use empirical correlations between cumulative summer warmth and riparian shrub height to reconstruct annual changes in shrub height from the 1960s to the present. The effects of longer and warmer growing seasons are estimated to have stimulated a 78% increase in the height of riparian shrubs. Earlier spring discharge and the estimated increase in riparian shrub height are consistent with observed riparian shrub expansion in the region. Our browsing measurements show that snowshoe hares require a mean riparian shrub height of at least 1.24-1.36 m, a threshold which our hindcasting indicates was met between 1964 and 1989. This generally coincides with observational evidence we present suggesting that snowshoe hares became established in 1977 or 1978. Warming and expanded shrub habitat is the most plausible reason for recent snowshoe hare establishment in Arctic Alaska. The establishment of snowshoe hares and other shrub herbivores in the Arctic in response to increasing shrub habitat is a contrasting terrestrial counterpart to the decline in marine mammals reliant on decreasing sea ice.
在 20 世纪期间,变暖改变了北极景观,包括水文学、植被、永冻土和冰川等方面,但野生动物的影响却难以察觉。本研究的主要目的是检验导致北阿拉斯加雪兔(Lepus americanus)的河岸栖息地和范围扩大的物理和生物过程。我们探索了自 20 世纪 60 年代以来北极阿拉斯加河岸生态系统的组成部分之间的联系,包括溪流流量、空气温度、洪泛区灌木栖息地和雪兔分布的季节性。我们的分析表明,在过去 30 年中,春季融雪期间的峰值流量平均每十年提前 3.4 天发生,这导致了洪泛区生态系统的生长季节延长。我们使用累积夏季温暖度与河岸灌木高度之间的经验相关性,从 20 世纪 60 年代至今重建了灌木高度的年际变化。较长和较暖的生长季节的影响估计刺激了河岸灌木高度增加了 78%。较早的春季流量和估计的河岸灌木高度增加与该地区观察到的河岸灌木扩展是一致的。我们的啃食测量表明,雪兔需要至少 1.24-1.36 米的平均河岸灌木高度,这一阈值是我们的回溯分析表明在 1964 年至 1989 年之间达到的。这大致与我们提出的观测证据相吻合,表明雪兔在 1977 年或 1978 年就已在北极地区定居。在北极,变暖和扩展的灌木栖息地是最近雪兔在阿拉斯加北极地区建立的最合理原因。雪兔和其他依赖于减少海冰的灌木食草动物在北极的建立,是对依赖于减少海冰的海洋哺乳动物减少的陆地对比。