Extreme Mediterranean rainfall impact on sedimentary routing systems: what can we learn from Storm Alex using in situ detrital 10Be?

Understanding how extreme meteorological events influence sediment transport is critical for predicting landscape evolution under a changing climate. Detrital cosmogenic 10 Be can provide insights into sediment dynamics following extreme rainfall, but high-resolution datasets tracking 10 Be variations before and after a storm, alongside long-term records, remain rare. The Var catchment (French Southern Alps) presents a unique case study, as its 10 Be signal was well-documented before the October 2020 Storm Alex (>500 mm of rainfall/24 h), which triggered flash floods, mobilized large sediment volumes, and formed a 10 km-long sediment plume in the Mediterranean Sea. We compare 10 Be concentrations in river sediments collected pre-storm (2016–2018), and at +7 days, +21 days, +4 months, and +7 months post-storm. We also use a historical offshore sample and contextualize these results with a 75 ka-long 10 Be record from deep-sea sediment cores. At the Var outlet, 10 Be concentrations initially increased by ∼25 % at +7 and +21 days, attributed to the mobilization of 10 Be-rich sediments from the upstream Var and Tinée sub-catchments. Concentrations returned to pre-storm levels within four months, primarily due to dilution with 10 Be-poor sediments from the Vésubie sub-catchment fluvioglacial terraces. While short-term 10 Be fluctuations at the Var outlet reflect complex sediment sourcing, our comparison with the 0–75 ka record confirms that major glaciation events and potential anthropic influences remain distinguishable, demonstrating that 10 Be is a robust proxy of denudation changes, even when extreme events are involved. • Extreme rainfall reshaped sediment transport altering 10 Be concentration in river sediments. • Storm-induced floods temporarily raised in situ 10 Be by ∼25 % at the Var outlet. • Post-storm 10 Be trends vary, with sediment sources driving spatially distinct responses. • High-res spatial, temporal sampling critical for constraining storm impact on 10 Be

Authors

Institutions

Publication Details

Journal
Geomorphology
Published
2025-10-15
DOI
https://doi.org/10.1016/j.geomorph.2025.110061
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Extreme Mediterranean rainfall impact on sedimentary routing systems: what can we learn from Storm Alex using in situ detrital 10Be?

Apolline Mariotti, Julien Charreau, Pierre‐Henri Blard, Samuel Toucanne et al.
Geomorphology
Geology and Paleoclimatology Research
article

Extreme Mediterranean rainfall impact on sedimentary routing systems: what can we learn from Storm Alex using in situ detrital 10Be?

Apolline Mariotti, Julien Charreau, Pierre‐Henri Blard, Samuel Toucanne, Stéphan Jorry, Olivier Joseph
article en

Abstract

Understanding how extreme meteorological events influence sediment transport is critical for predicting landscape evolution under a changing climate. Detrital cosmogenic 10 Be can provide insights into sediment dynamics following extreme rainfall, but high-resolution datasets tracking 10 Be variations before and after a storm, alongside long-term records, remain rare. The Var catchment (French Southern Alps) presents a unique case study, as its 10 Be signal was well-documented before the October 2020 Storm Alex (>500 mm of rainfall/24 h), which triggered flash floods, mobilized large sediment volumes, and formed a 10 km-long sediment plume in the Mediterranean Sea. We compare 10 Be concentrations in river sediments collected pre-storm (2016–2018), and at +7 days, +21 days, +4 months, and +7 months post-storm. We also use a historical offshore sample and contextualize these results with a 75 ka-long 10 Be record from deep-sea sediment cores. At the Var outlet, 10 Be concentrations initially increased by ∼25 % at +7 and +21 days, attributed to the mobilization of 10 Be-rich sediments from the upstream Var and Tinée sub-catchments. Concentrations returned to pre-storm levels within four months, primarily due to dilution with 10 Be-poor sediments from the Vésubie sub-catchment fluvioglacial terraces. While short-term 10 Be fluctuations at the Var outlet reflect complex sediment sourcing, our comparison with the 0–75 ka record confirms that major glaciation events and potential anthropic influences remain distinguishable, demonstrating that 10 Be is a robust proxy of denudation changes, even when extreme events are involved. • Extreme rainfall reshaped sediment transport altering 10 Be concentration in river sediments. • Storm-induced floods temporarily raised in situ 10 Be by ∼25 % at the Var outlet. • Post-storm 10 Be trends vary, with sediment sources driving spatially distinct responses. • High-res spatial, temporal sampling critical for constraining storm impact on 10 Be

GeomorphologyVol. 492
Musée de la Civilisation (CA), Centre National de la Recherche Scientifique (FR), Université Libre de Bruxelles (BE), Ifremer (FR), Université de Bretagne Occidentale (FR), Centre de Recherches Pétrographiques et Géochimiques (FR), GFZ Helmholtz Centre for Geosciences (DE), Université de Lorraine (FR)
Openalex Percentile: Top 66%
Geology and Paleoclimatology Research
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.