Luca Ziliani
University of Padua
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Aquatic Sciences | 2016
Angela M. Gurnell; Massimo Rinaldi; B. Belletti; Simone Bizzi; Bernadette Blamauer; G. Braca; Anthonie D. Buijse; M. Bussettini; B. Camenen; Francesco Comiti; L. Demarchi; D. García de Jalón; M. González del Tánago; Robert C. Grabowski; I. D. M. Gunn; Helmut Habersack; Dimmie Hendriks; Alexander J. Henshaw; Mario Klösch; B. Lastoria; A. Latapie; Paweł Marcinkowski; Vanesa Martínez-Fernández; Erik Mosselman; J. O. Mountford; Laura Nardi; Tomasz Okruszko; Matthew T. O’Hare; M. Palma; C. Percopo
This paper introduces this special issue of Aquatic Sciences. It outlines a multi-scale, hierarchical framework for developing process-based understanding of catchment to reach hydromorphology that can aid design and delivery of sustainable river management solutions. The framework was developed within the REFORM (REstoring rivers FOR effective catchment Management) project, funded by the European Union’s FP7 Programme. Specific aspects of this ‘REFORM framework’ and some applications are presented in other papers in this special issue. The REFORM framework is founded on previous hierarchical frameworks, sixteen examples of which are reviewed. However, the REFORM framework has some particular properties that reflect the European context for which it was developed. The framework delineates regional landscapes into nested spatial units at catchment, landscape unit, segment, reach, geomorphic unit and finer scales. Reaches, regardless of their ‘naturalness’, are assigned to a river type based on valley confinement, planform and bed material. Indicators are quantified at each spatial scale to feed three groups of assessments. First, contemporary indicators at reach and geomorphic unit scales investigate present processes, forms and human pressures within each reach. These feed assessments of present reach hydromorphological function/alteration, including whether the reach is functioning appropriately for its type; riparian corridor function and alteration; and hydromorphological adjustment. Second, indicators at catchment to segment scales investigate water and sediment production and delivery to reaches and how these are affected by human pressures now and in the past. These are used to construct an inventory of changes over space and time. Third, historical reach and geomorphic unit scale indicators are used to construct the trajectory of reach-scale changes. Contemporary reach-scale assessments, space–time inventory, and trajectory of changes are then combined to establish how river reaches of different type, subject to different human pressures, and located in different environmental contexts behave in response to changes at all considered spatial scales. These support forecasts of the likely responses of reaches to future scenarios (e.g., changes in climate, land cover, channel interventions).
Aquatic Sciences | 2016
Luca Ziliani; Nicola Surian
This paper focuses on the temporal elements of the REFORM hydromorphological framework, illustrating these elements with an analysis of information from the lower Tagliamento river, Italy. It presents an analysis of historical channel adjustments at segment and reach scales over the last two centuries, reflecting human pressures that are summarised but not fully developed in this paper, and an analysis of data from aerial photographs, topographic surveys, and river flow records. This is followed by an assessment of likely future changes over the period 2012–2035 based upon both a conceptual model founded on the historical analysis and numerical modelling. The Tagliamento river has gone through three main phases of adjustment. The first two phases, characterized by narrowing and incision, were driven primarily by human interventions (i.e. sediment mining and channelization). The most recent phase represents an attempt of the river to achieve a new equilibrium condition and is mainly controlled by flow regime (i.e. frequency and magnitude of formative discharges) and vegetation establishment. As for future channel evolution, both models showed that slight width changes are likely to occur over the period 2012–2035. Channel widening, that could be expected as a response to an excess of unit stream power, will be hampered by vegetation establishment. Finally, the “no intervention” strategy seems to be the best option for leading the river towards a new equilibrium condition and to achieve different goals (e.g. flood mitigation, conservation or improvement of ecological status).
River Research and Applications | 2009
Walter Bertoldi; Angela M. Gurnell; Nicola Surian; Klement Tockner; Luca Zanoni; Luca Ziliani; Guido Zolezzi
River Research and Applications | 2009
Nicola Surian; Luca Ziliani; Francesco Comiti; Mario Aristide Lenzi; Luca Mao
Geomorphology | 2012
Luca Ziliani; Nicola Surian
Earth Surface Processes and Landforms | 2009
Nicola Surian; Luca Mao; Matteo Giacomin; Luca Ziliani
Geological Society of America Special Papers | 2009
Nicola Surian; Massimo Rinaldi; Luisa Pellegrini; Chiara Audisio; Franca Maraga; Liliana Beatriz Teruggi; Ornella Turitto; Luca Ziliani
Earth Surface Processes and Landforms | 2015
Nicola Surian; Matteo Barban; Luca Ziliani; Giovanni Monegato; Walter Bertoldi; Francesco Comiti
Journal of Geophysical Research | 2013
Luca Ziliani; Nicola Surian; Tom J. Coulthard; Stefano Tarantola
Archive | 2014
Simone Bizzi; Bernadette Blamauer; G. Braca; M. Bussettini; B. Camenen; Francesco Comiti; L. Demarchi; D. García de Jalón; M. González del Tánago; Robert C. Grabowski; Angela M. Gurnell; Helmut Habersack; B. Lastoria; A. Latapie; Vanesa Martínez-Fernández; J. O. Mountford; Laura Nardi; Matthew T. O'Hare; C. Percopo; Massimo Rinaldi; Nicola Surian; C. Weissteiner; Luca Ziliani