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Environmental heterogeneity and community structure of the Kobuk River, Alaska, in response to climate change

机译:应对气候变化的阿拉斯加科布克河环境异质性和群落结构

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The Kobuk River runs west along the southern Brooks Range from Gates of the Arctic National Park in Alaska, USA, to the Chukchi Sea. It is highly vulnerable to changes in climate due to its sub‐Arctic location, unique geography, and permafrost foundation. Combined with its pristine condition, these qualities make the Kobuk an ideal system upon which to build a conceptual model for predicting ecosystem effects of climate change. We constructed a conceptual ecosystem model for the Kobuk River synthesizing surveyed baseline hydrologic, geomorphic and biotic conditions with literature on Arctic rivers. While the mainstem Kobuk has limited biological productivity, it provides spawning habitat and connectivity for large resident and migratory fish that rely upon off‐channel habitat for food resources. System function is dependent largely on intermittent pulse flows that connect riverine habitats, allowing periods of late summer high productivity in off‐channel habitat. Spring break‐up and hill slope processes are critically important for maintaining habitat complexity and inter‐connectivity. Climate change models predict the region will experience a disproportionate increase in average winter air temperature relative to summer temperatures, in the number of ice‐free days, and in annual rainfall. Our conceptual model predicts that changes to fish and invertebrate populations on the Kobuk River will result not from physiological responses to increased temperatures, but rather to shifts in two main physical drivers: 1) spring break‐up intensity, resulting in changes to scour rate and sediment deposition; and 2) discontinuous permafrost melt, resulting in widespread heterogeneous zones of active layer thickening and thermokarsting. The interaction of these two drivers offers four potential scenarios of geomorphic change in the system and four dramatically different biological outcomes. This model should help managers and scientists evaluate the magnitude and direction of ecosystem changes as they occur within the Kobuk system and potentially other sub‐Arctic river systems.
机译:Kobuk河沿布鲁克斯山脉的南部向西延伸,从美国阿拉斯加的北极国家公园大门到楚科奇海。由于其位于亚北极地区,独特的地理环境和多年冻土基础,因此极易受到气候变化的影响。结合其原始状况,这些品质使Kobuk成为理想的系统,可在此系统上构建预测气候变化的生态系统影响的概念模型。我们为科布克河建立了一个概念性的生态系统模型,利用北极河上的文献综合了调查的基线水文,地貌和生物条件。虽然主干科布克的生物生产力有限,但它为依赖离岸生境获取食物资源的大型居民和and游鱼类提供了产卵栖息地和连通性。系统功能在很大程度上取决于连接河流生境的间歇性脉冲流,从而使夏末时期的河外生境具有较高的生产力。春季拆解和山坡倾斜过程对于维持栖息地的复杂性和相互联系至关重要。气候变化模型预测,该地区冬季平均气温相对于夏季气温,无冰天数和年降雨量将成比例增加。我们的概念模型预测,科布克河上鱼类和无脊椎动物种群的变化将不是由温度升高引起的生理反应引起的,而是由两个主要物理驱动因素的变化引起的:1)春季破坏强度,导致冲刷率的变化和沉积物沉积2)不连续的永冻土融化,导致活动层增厚和热岩溶的广泛非均质区。这两个驱动因素的相互作用提供了系统中地貌变化的四种可能情况以及四种生物学结果截然不同的情况。该模型应帮助管理人员和科学家评估生态系统变化的幅度和方向,这些变化发生在科布克系统和潜在的其他亚北极河流系统内。

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