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Channel and landscape dynamics in the alluvial forest mosaic of the Carmanah River valley, British Columbia, Canada

机译:加拿大不列颠哥伦比亚省卡曼纳河谷冲积森林马赛克中的河道和景观动力学

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The highly diverse shifting-mosaic of forest patches of an alluvial forest within the Carmanah River valley on the west coast of Vancouver Island, British Columbia was studied to examine the hydrogeomorphic disturbance regime that structures it. We used a landscape-scale analysis to quantify historical channel migrations and changes in the extent of specific forest types. This CIS-based analysis using a 70-year aerial photographic record was complemented by field-based research. Thirty-eight plots containing 4509 trees were sampled for forest structure, age, and elevation above the contemporary channel. These data, including a vegetation chronosequence spanning over 500 years, were used to examine channel and landscape dynamics. Our findings support a general conceptual model that describes cycles of patch development and destruction in unconfined alluvial forests of the Pacific Coastal Ecoregion. Over the past century, Carmanah River has eroded nearly 30% of the alluvial forest in this study area, and approximately 65% over the past 500 years. At least 80% of the 2007 channel was forested area within the past 70 years. Younger landforms were disturbed more frequently than mature forest patches, which suggest that as biogeomorphic succession progresses the likelihood of future disturbance decreases. Estimated half lives of landforms ranged from 24 years for pioneer bars to over 1500 years for old growth terraces. Years of regional high magnitude floods resulted in a net loss of floodplain forest area indicating that disturbance was climate driven in this pluvial watershed, whereby rain events result in flood disturbance that converted forests to channel. These events initiate a subsequent course of vegetation succession and geomorphic development, and often result in the deposition of large wood that modifies the channel environment and contributes to channel avulsion and further hydrogeomorphic disturbance. The composition of the landscape is a reflection of the balance between the disturbance rate and successional development We also observed a relationship between landscape composition and watershed size. Specifically, the ratio of mature to developing alluvial forests was higher in this smaller watershed compared to larger watersheds in the region. Results imply that larger flood events predicted to occur with climate change may change the disturbance regime of floodplain forests and alter landscape composition.
机译:研究了不列颠哥伦比亚省温哥华岛西海岸的卡马纳河谷内冲积森林的高度分散的森林斑块转变马赛克,以研究构成其的水文地貌扰动机制。我们使用景观尺度分析来量化历史通道迁移和特定森林类型范围内的变化。这种基于CIS的使用70年航空摄影记录的分析得到了野外研究的补充。对38个包含4509棵树的样地进行了采样,以了解其森林结构,年龄和海拔高度高于现代通道的情况。这些数据,包括跨越500年的植被时间序列,被用于检查渠道和景观动态。我们的发现支持一个通用的概念模型,该模型描述了太平洋沿岸生态区的无限制冲积林中斑块发育和破坏的周期。在过去的一个世纪中,卡玛纳河侵蚀了该研究区近30%的冲积林,而在过去500年中,这一侵蚀率约为65%。在过去的70年中,至少有80%的2007年通道是林区。与成熟的森林斑块相比,年轻的地貌受到的干扰更多,这表明随着生物地貌演替的进行,未来受到干扰的可能性降低。地貌的估计半衰期从先锋酒吧的24年到旧的生长梯田的1500年以上不等。多年的区域性高洪灾导致洪泛区森林面积净损失,这表明在这个小流域,气候是由干扰驱动的,降雨事件导致洪水干扰,使森林转变为河道。这些事件启动了植被演替和地貌发育的后续过程,并经常导致大木材的沉积,从而改变了河道环境,并助长了河道侵蚀和进一步的水力地貌扰动。景观组成反映了扰动率与演替发展之间的平衡。我们还观察到景观组成与流域规模之间的关系。具体而言,与该地区较大的流域相比,在较小的流域,成熟冲积森林与发育冲积森林的比例更高。结果表明,预计随着气候变化将发生更大的洪水事件,可能会改变洪泛区森林的干扰状况并改变景观组成。

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