Historical cartographic and topo-bathymetric database on the French Rhône River (17th–20th century)

Abstract

Abstract. Space and time analyses of channel changes, especially within large rivers subject to high levels of human impact, are critical to address multiple questions about rivers in the Anthropocene era. The reconstruction of long-term (> 150 year) evolutionary trajectories permits an understanding of how natural and anthropogenic factors impact hydromorphological and ecological processes in rivers, helps with the design of sustainable management and restoration options, and may also help in the assessment of future changes. However, the reconstruction of channel changes can be challenging: historical data are often scattered across many archives, and the quantity and accuracy of information generally decreases as one goes back in time. This data article provides a historical database of 350 cartographic and topo-bathymetric resources on the French Rhône River (530 km in length) compiled from the 17th to mid-20th century, with a temporal focus prior to extensive river training (1860s). The data were collected in 14 national, regional, and departmental archive services. A table describes the properties of each archived data item and its associated iconographic files. Some of the historical maps are available in a georeferenced format. A GIS layer enables one-click identification of all archive data available for a given reach of the French Rhône River. This database provides substantial new material for deeper analyses of channel changes over a longer time period and at a finer time step compared with previously available data. The database has several potential applications in geomorphology, retrospective hydraulic modelling, historical ecology, and river restoration, as well as permitting comparisons with other multi-impacted rivers worldwide. The dataset is available at https://doi.org/10.1594/PANGAEA.922437 (Arnaud et al., 2020a). Iconographic extracts of the 350 archived items are available at http://photo.driihm.fr/index.php/category/52 (last access: 2 May 2021).

Dike Fields as Drivers and Witnesses of 20th Century Hydrosedimentary Changes in Highly Engineered Rivers

“…Planimetric evolution of terrestrialization Terrestrialization is first assessed by studying the planimetric evolution based on photograph archives georeferenced on GIS as it is now done classically (e.g., Bryant and Gilvear, 1999;Winterbottom, 2000;Gilvear and Bryant, 2003). On the Rhône River, many studies have already used the available map and photographic archives to follow the evolution of the side channels and floodplains but do not focus on the dike field evolution (Riquier et al, 2015;2017;Dépret et al, 2017;Tena et al, 2020;Arnaud et al, 2021).…”

The social connectivity of subsurface flows: Towards a better integration of the vertical dimension in socio‐hydrosystem studies

“…Over time, the literature on river restoration has expanded its focus to include two additional dimensions in the exploration of connectivity within hydrosystems: the temporal dimension (Amoros et al, 1987; Arnaud et al, 2021; Eschbach et al, 2018; Ward, 1989) and more recently the socio‐cultural one (Boyer et al, 2018; Kondolf & Pinto, 2017; Pradilla et al, 2021; Wantzen, 2022; Wölfle‐Erskine, 2017). Cultural and territorial attachment, along with the inclusion of local political dynamics are both acknowledged as central components in the implementation of water conservation and river restoration projects.…”