The Polar Center and Department of Biology, Penn State University, 208 Mueller Lab, University Park, Pennsylvania 16802, USA.
Nat Commun. 2013;4:2514. doi: 10.1038/ncomms3514.
The contribution of declining Arctic sea ice to warming in the region through Arctic amplification suggests that sea ice decline has the potential to influence ecological dynamics in terrestrial Arctic systems. Empirical evidence for such effects is limited, however, particularly at the local population and community levels. Here we identify an Arctic sea ice signal in the annual timing of vegetation emergence at an inland tundra system in West Greenland. According to the time series analyses presented here, an ongoing advance in plant phenology at this site is attributable to the accelerating decline in Arctic sea ice, and contributes to declining large herbivore reproductive performance via trophic mismatch. Arctic-wide sea ice metrics consistently outperform other regional and local abiotic variables in models characterizing these dynamics, implicating large-scale Arctic sea ice decline as a potentially important, albeit indirect, contributor to local-scale ecological dynamics on land.
北极海冰的减少通过北极放大效应导致该地区变暖,这表明海冰的减少有可能影响北极陆地系统的生态动态。然而,这种影响的经验证据是有限的,特别是在当地种群和群落层面。在这里,我们在格陵兰岛西部的一个内陆冻原生态系统中发现了年度植被出现时间的北极海冰信号。根据这里呈现的时间序列分析,该地点植物物候的持续提前归因于北极海冰的加速减少,并通过营养不匹配导致大型食草动物繁殖性能下降。在描述这些动态的模型中,北极海冰指标在一致性上优于其他区域和局部非生物变量,这表明大规模的北极海冰减少可能是陆地局部生态动态的一个重要但间接的贡献因素。