This paper focuses on the contribution of fluvial geomorphology to flood management. We define what fluvial geomorphologists understand by “fluvial risk” and examine the relationship between fluvial geomorphology and fluvial hazards. The paper details how fluvial geomorphology can present innovative approaches to flood prevention, river maintainance and floodplain restoration. Management of soil erosion and floodwaters is the key question in the plateaus and plains of northern France. In mountainous terrain, strong connectivity between the slopes and high order streams induces permanent risk for local people living near the river, on alluvial fans or on the lower river terraces as demonstrated in the French Alps and in Nepal Himalayas. Management of debris flows resulting from interaction of erosion processes on the slopes and valley bottom is of fundamental importance. The paper highlights the diversity of concepts and methods, such as hydrogeomorphological mapping, sediment budget and functional flood areas, developed by fluvial geomorphologists in order to understand spatio-temporal variability of flood hazard and induced flood risk in temperate, Mediterranean and mountainous areas. The discussion places the existing research in the context of the main ecological issues, future climate change and the constraints imposed by the land-use conflicts, political and social choices and the need to preserve natural heritage.

Mountains are specific ecosystems, characterised by their diversity and complexity (Messerli and Ives, 1997). Steep topographic, climatic and biological gradients combined with sharp seasonal contrasts favour the triggering of extreme climatic and geomorphic events, which may in turn strongly affect ecological and human environments (Ives and Messerli, 1989; Price, 1999; Beniston, 2002; Viviroli et al., 2007; Hüggel et al., 2010; Körner, 2013). Mountain populations are quite diverse in their ...

Pokhara (ca. 850 m a.s.l.), Nepal's second-largest city, lies at the foot of the Higher Himalayas and has more than tripled its population in the past 3 decades. Construction materials are in high demand in rapidly expanding built-up areas, and several informal settlements cater to unregulated sand and gravel mining in the Pokhara Valley's main river, the Seti Khola. This river is fed by the Sabche glacier below Annapurna III (7555 m a.s.l.), some 35 km upstream of the city, and traverses one of the steepest topographic gradients in the Himalayas. In May 2012 a sudden flood caused >70 fatalities and intense damage along this river and rekindled concerns about flood risk management. We estimate the flow dynamics and inundation depths of flood scenarios using the hydrodynamic model HEC-RAS (Hydrologic Engineering Center’s River Analysis System). We simulate the potential impacts of peak discharges from 1000 to 10 000 m³ s⁻¹ on land cover based on high-resolution Maxar satellite imagery and OpenStreetMap data (buildings and road network). We also trace the dynamics of two informal settlements near Kaseri and Yamdi with high potential flood impact from RapidEye, PlanetScope, and Google Earth imagery of the past 2 decades. Our hydrodynamic simulations highlight several sites of potential hydraulic ponding that would largely affect these informal settlements and sites of sand and gravel mining. These built-up areas grew between 3- and 20-fold, thus likely raising local flood exposure well beyond changes in flood hazard. Besides these drastic local changes, about 1 % of Pokhara's built-up urban area and essential rural road network is in the highest-hazard zones highlighted by our flood simulations. Our results stress the need to adapt early-warning strategies for locally differing hydrological and geomorphic conditions in this rapidly growing urban watershed.

Studies on large and rapid mass movements have become a challenging issue in relation to paraglacial and morpho-tectonic evolution of mountain slopes. Rockfalls, rockslides and rock avalanches will be considered here on the basis of selected sites in the French and Swiss Alps and in the Himalayas. The main topics developed relate firstly to the modes of emplacement of, and the internal structures observed in, the body of the runout deposits and the influence of the surface (bedrock, superficial deposits, glacier, lake) over which the propagation takes place. The impacts of these rockslope failures on geomorphic systems (damming effects, storage, control on sediment fluxes) are then considered. Finally, the possible influence of climate change on high-alpine rockwalls, and potential threat to adjacent inhabited areas, are presented.