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Morphological response to river engineering and management in alluvial channels in Italy

Nicola Surian, +1 more
- 01 Mar 2003 - 
- Vol. 50, Iss: 4, pp 307-326
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TLDR
In this article, the authors reviewed all existing published studies and available data, and aimed to reconstruct a general outline of the main channel adjustments that have occurred in Italian rivers during the past 100 years.
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This article is published in Geomorphology.The article was published on 2003-03-01 and is currently open access. It has received 580 citations till now. The article focuses on the topics: Channel pattern & Fluvial.

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Climate change and the world's river basins: anticipating management options

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Human influence and the changing geomorphology of Mediterranean deltas and coasts over the last 6000 years: From progradation to destruction phase?

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Sediment mining in alluvial channels: physical effects and management perspectives

TL;DR: In this paper, a review of a number of documented case studies from various countries and a detailed analysis of sediment exploitation from five rivers in Italy and Poland is presented, where the authors discuss alluvial river response to extensive sediment mining.
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Human impacts on fluvial systems in the Mediterranean region

TL;DR: The long history of substantial human impacts on the landscape of the Mediterranean region, and their effects on fluvial systems, is documented in this paper, where the importance of analysing the connectivity within different land units and of the spatial position of human activity within a catchment is illustrated.
References
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Journal ArticleDOI

Bed-level adjustments in the Arno River, central Italy

TL;DR: In this paper, two distinct phases of bed-level adjustment over the last 150 years are identified for the principal alluvial reaches of the Arno River (Upper Valdarno and Lower Varno).
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Changes in river regime after the construction of upstream reservoirs

TL;DR: In this paper, the authors present and analyze many years of investigations in China on the fluvial processes downstream of impounding and detention reservoirs, covering the change in hydrograph, the recovering of sediment concentration along the river course, the degradation of stream bed, the adjustment of longitudinal profile, the coarsening of bed material, the changes in channel width, and the trend of channel pattern variation for alluvial streams downstream of alluvials.
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Channel and floodplain response to recent abrupt climate change: The tyne basin, Northern England

TL;DR: In this paper, the authors examined the timing, nature and magnitude of river response in upland, piedmont and lowland reaches of the Tyne basin, northern England, to high-frequency (20-30 year) changes in climate and flood regime since 1700 AD.
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