River confinement and braiding loss in Canterbury region, Aotearoa New Zealand

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Victoria Barlow, Peter Ashmore
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引用次数: 0

Abstract

In relation to the wider concern that rivers in Aotearoa New Zealand have been narrowed by river control and land-use encroachment, and that iconic braided patterns are being lost, nine braided rivers from the Canterbury region were studied to compare river width, pattern type and braiding intensity between the mid-1900s and the present based on mapping from aerial images. Channel narrowing occurred along >90% (~490 km) of the length of the rivers studied, 375 km of which were historically braided. In total, the rivers narrowed by an average of 43% (48% for braided reaches). Coinciding with narrowing, braided reaches lost 1.3 channels, on average. Overall, 20% (over 100 km) length of the rivers recorded a change from braided to more simple pattern types including wandering (~18%) and single channel (~1%). The relationship of channel width and pattern change demonstrates the predictability of braiding change based on channel narrowing. As channels narrow, the likelihood of pattern simplification and change increases, although the amount of narrowing required to induce change depends on the initial width and pattern. Narrowing causes a reduction of braiding intensity even when the channel pattern remains braided. Based on these results, a predictor of channel pattern change and reduction of braiding intensity, based only on channel width and width change, can be applied to aid room-for-river management plans for conserving or restoring braided river morphologies. Channel width provides a general criterion for the prediction of braiding intensity and channel pattern threshold illustrating the scale-related effects on channel pattern.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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