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Quantifying geomorphic and vegetation change at sandbar campsites in response to flow regulation and controlled floods, Grand Canyon National Park, Arizona

机译:亚利桑那州大峡谷国家公园,根据流量调节和受控洪水,量化沙洲营地的地貌和植被变化

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摘要

Sandbars along the Colorado River in Grand Canyon National Park, USA, are an important recreational resource used as campsites by over 25,000 river runners and hikers annually. The number and size of campsites decreased following the completion of Glen Canyon Dam in 1963 due to reductions of sediment that replenish sandbars and increases in vegetation cover caused by flow regulation. Campsite area continues to decrease despite the use of controlled floods to rebuild sandbars. We quantify the relative magnitude of factors that contribute to changes in campsite size, such as fluvial deposition and erosion, gullying, and vegetation expansion with analysis of four-band aerial imagery and digital elevation models. Campsite area declined by 37% between 2002 and 2016 (an average of 161 m(2) per site at long-term monitoring sites). Two drivers contributed to campsite area change: (a) short-term gains and losses associated with controlled floods and flood-deposit erosion and (b) long-term one-directional loss of campsite area caused by vegetation encroachment. There was more erosion and slope change at sites in critical reaches-sections of river where campsites are infrequent or in high demand-than in noncritical reaches. Vegetation continues to expand at campsites under flow regulation, particularly in noncritical reaches. Although controlled floods have contributed to short-term increases in sandbar size, long-term increases in campsite area have not occurred because of sandbar erosion between controlled floods and vegetation expansion. Manual vegetation removal may need to be considered in future management strategies.
机译:美国大峡谷国家公园的科罗拉多河沿岸的沙洲是重要的休闲资源,每年有超过25,000名河跑步者和徒步旅行者用作露营地。 1963年格伦峡谷大坝竣工后,露营地的数量和规模有所减少,原因是由于流量调节所致的沉积物减少(补充沙洲)和植被覆盖率增加。尽管使用受控洪水重建沙洲,营地面积仍在继续减少。我们通过分析四波段航拍图像和数字高程模型,量化了影响营地规模变化的因素的相对大小,例如河流沉积和侵蚀,沟壑和植被扩展。在2002年至2016年期间,营地面积下降了37%(长期监测点平均每个场址161 m(2))。导致营地面积变化的两个因素:(a)与受控洪水和洪水冲刷侵蚀有关的短期收益和损失,以及(b)由植被侵占引起的营地面积的长期单向损失。与非关键河段相比,在露营地很少或需求量大的河流关键河段的地点,侵蚀和坡度变化更大。受流量调节,露营地的植被继续扩大,特别是在非关键河段。尽管受控洪水导致了沙洲规模的短期增加,但由于受控洪水与植被扩张之间的沙洲侵蚀,营地面积的长期增长并未发生。在未来的管理策略中可能需要考虑手动清除植被。

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