Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, AK, 99775, USA.
Glob Chang Biol. 2014 Apr;20(4):1211-24. doi: 10.1111/gcb.12500. Epub 2014 Feb 11.
Many areas of the Arctic are simultaneously affected by rapid climate change and rapid industrial development. These areas are likely to increase in number and size as sea ice melts and abundant Arctic natural resources become more accessible. Documenting the changes that have already occurred is essential to inform management approaches to minimize the impacts of future activities. Here, we determine the cumulative geoecological effects of 62 years (1949-2011) of infrastructure- and climate-related changes in the Prudhoe Bay Oilfield, the oldest and most extensive industrial complex in the Arctic, and an area with extensive ice-rich permafrost that is extraordinarily sensitive to climate change. We demonstrate that thermokarst has recently affected broad areas of the entire region, and that a sudden increase in the area affected began shortly after 1990 corresponding to a rapid rise in regional summer air temperatures and related permafrost temperatures. We also present a conceptual model that describes how infrastructure-related factors, including road dust and roadside flooding are contributing to more extensive thermokarst in areas adjacent to roads and gravel pads. We mapped the historical infrastructure changes for the Alaska North Slope oilfields for 10 dates from the initial oil discovery in 1968-2011. By 2010, over 34% of the intensively mapped area was affected by oil development. In addition, between 1990 and 2001, coincident with strong atmospheric warming during the 1990s, 19% of the remaining natural landscapes (excluding areas covered by infrastructure, lakes and river floodplains) exhibited expansion of thermokarst features resulting in more abundant small ponds, greater microrelief, more active lakeshore erosion and increased landscape and habitat heterogeneity. This transition to a new geoecological regime will have impacts to wildlife habitat, local residents and industry.
北极地区的许多区域同时受到快速气候变化和快速工业发展的影响。随着海冰融化,北极丰富的自然资源变得更容易获取,这些区域的数量和规模可能会增加。记录已经发生的变化对于制定管理措施以最大程度地减少未来活动的影响至关重要。在这里,我们确定了普里多湾油田(北极地区最古老、最广泛的工业综合体,以及一个拥有丰富富冰永久冻土的地区,对气候变化极为敏感)在基础设施和气候相关变化下的 62 年(1949-2011 年)的累积地球生态效应。我们证明,热喀斯特地貌最近已经影响了整个地区的广大区域,而自 1990 年以来,受影响区域的突然增加始于 1990 年左右,这与该地区夏季空气温度的快速上升以及相关的永久冻土温度有关。我们还提出了一个概念模型,描述了与基础设施相关的因素(包括道路灰尘和路边洪水)如何导致道路和砾石垫附近区域的热喀斯特地貌更加广泛。我们为阿拉斯加北坡油田的 10 个日期(从 1968 年到 2011 年首次发现石油)绘制了历史基础设施变化图。到 2010 年,超过 34%的高强度测绘区域受到石油开发的影响。此外,在 1990 年至 2001 年期间,与 20 世纪 90 年代大气强烈变暖同时发生,剩余自然景观(不包括基础设施、湖泊和河流泛滥平原覆盖的区域)的 19%显示出热喀斯特特征的扩张,导致更多丰富的小池塘、更大的微地形、更活跃的湖滨侵蚀以及增加的景观和栖息地异质性。这种向新的地球生态系统的转变将对野生动物栖息地、当地居民和工业产生影响。