Aims of research

Recovery of a sediment core from the Lombach fan delta (Berner Oberland, Switzerland; 21.09.2007, © by N. Moreno)

Figure 3: Recovery of a sediment core from the Lombach fan delta (Berner Oberland, Switzerland; 21.09.2007, © by N. Moreno).

FluVAlps aims at the reconstruction of the past 3000 years of Alpine fluvial environments using high- and medium-resolution proxy data from fan delta deposits, pollen records and documentary sources. FluVAlps addresses the influence of external factors, such as climatic variability and land use, on aggradation processes and paleofloods in alpine catchments.

Currently the significance of flood magnitude, frequency and causes in mountain regions are discussed in the context of Global Change. After the 2005 Lütschine flood event these variables are discussed once more on a local scale. From a Holocene perspective, we highlight the following key points:

  • Can fan delta deposits in the Alps provide high-resolution paleoclimate proxies? And if so, how do these natural archives correlate with local, regional and global climate variability? Exist an synchronous or asynchronous response of different Alpine catchments? Attention will be paid particularly to climate phases as e.g. the maximum and minimum solar anomalies. Regarding the characterization of post LIA climate change, a special relevance is attributed to the environmental conditions recorded during warmer climate phases as the Medieval Warm Period and the Roman Climate Optimum.
  • To which extend did land uses modify the environment and geomorphic processes in the catchments? Are there significant changes in flood magnitude or frequency before and after the shift from natural dominated to human dominated ecosystems?
  • Concerning a mayor accuracy of past discharge models and future flood scenarios, the understanding of timing of mayor floods (during cooler or warmer or transitional Holocene periods), is as crucial as the cross calibration of natural archives, written sources and instrumental flood records. From the calibration the question emerges which were the mayor controlling mechanisms of floods and aggradation processes in the past. The improvement of this knowledge will provide a good starting point to test flood models and to assess natural hazards in Alpine catchments.
Relevant publications

L. Schulte1, J. C. Peña, F. Carvalho, T. Schmidt, R. Julià, J. Llorca, and H. Veit, 2015.

A 2600-year history of floods in the Bernese Alps, Switzerland: frequencies, mechanisms and climate forcing

Hydrol. Earth Syst. Sci., 19, 3047-3072, 2015


J. C. Peña1, L. Schulte, A. Badoux, M. Barriendos, and A. Barrera-Escoda, 2015.

Influence of solar forcing, climate variability and modes of low-frequency atmospheric variability on summer floods in Switzerland

Hydrol. Earth Syst. Sci., 19, 3807-3827, 2015


L. Schulte, J.C. Peña, R. Julià, F. Carvalho, J. Llorca, J. Losada, F. Burjachs, T. Schmidt, P. Rubio, H. Veit, 2014.

CLIMATE FORCING OF PALEOFLOODS IN THE SWISS ALPS

Avances de la Geomorfología en España 2012-2014. Editores: Susanne Schnabel y Álvaro Gómez Gutiérrez. XIII Reunión Nacional de Geomorfología, Cáceres, 2014. pp. 143-146

Universitat de BarcelonaICREA - Institució Catalana de Recerca i Estudis AvançatsUniversität BernServei Meteorològic de CatalunyaGobierno de España - Ministerio de Educación y CienciaAlexander von Humboldt Foundation