Landscapes Live
EGU-GM Online Seminars in Geomorphology
Landscapes Live is a weekly online seminar series freely accessible to the international scientific community interested in various aspects of geomorphology. Our talks take place on Zoom every Thursday, starting at 4pm time of Paris/Berlin/Amsterdam. Check your local time here.
Landscapes Live is affiliated to the Geomorphology (GM) division of EGU and contribute to develop its virtual activities. Indeed, EGU is pioneering a new CampFire concept to bring together the geoscience community in between General Assemblies. We hope that this helps us in our transition to a greener future and ensure that our community better serve the needs of all scientists regardless of international mobility.
https://gfz-de.zoom-x.de/meeting/register/94YLJJBST9CgOxxx1D8G0Q
Geomorphic transitions—such as the interface between rivers and floodplains—are critical zones controlling water, sediment, and nutrient transport. In this talk, I examine flux exchanges across these transitions through the lens of connectivity and its variability in space and time. Using the Wax Lake Delta in coastal Louisiana as a testbed, we integrate field observations, numerical modeling, and remote sensing (Delta-X mission) to quantify channel–wetland connectivity. Results show that about 50% of channel discharge enters wetlands, with connectivity strongly modulated by seasonal changes in discharge and vegetation: high in spring, low in summer. Sediment connectivity patterns show that sediment into islands scales mainly with discharge and that mud is retained in islands.
We then scale this analysis to global river deltas in the context of the Surface Water and Ocean Topography (SWOT) mission. Leveraging DeepWaterMap water mask extraction, RivGraph-based network extraction, and graph-theoretic approaches, we estimate discharge partitioning along delta networks. We extend these methods to sediment and solute fluxes using particle tracking and first-order removal models. We are currently incorporating SWOT pixel cloud data to estimate channel-wetland connectivity and account for leakiness.
By combining multi-scale observations with network-based modeling, this work advances our ability to quantify connectivity across geomorphic boundaries and predict how coastal landscapes respond to hydrologic and ecological drivers. These insights are critical for understanding delta resilience and guiding management under climate change and human interventions.
Mountain landscapes evolve through the combined influence of tectonic and climatic processes, with glaciations playing a key role in shaping topography and driving sediment erosion over both short (ka) and long (Ma) timescales. However, quantifying the extent of glacial influence remains a challenge, as the relative contributions of climate and tectonics to denudation rates vary across time scales and different mountain ranges.
On short timescales, evidence from the French Alps reveals a nuanced climatic imprint. In-situ cosmogenic ¹⁰Be from offshore sediment cores provides a continuous 70 ka denudation record for the Var catchment, revealing broadly stable erosion rates despite pronounced climate fluctuations. Only during the Last Glacial Maximum (26–19 ka) do sharply lower ¹⁰Be concentrations indicate a brief but substantial increase in erosion, suggesting that only the most extensive glacial advances triggered a strong catchment-wide response.
Over million-year timescales, however, glaciations exert a much more sustained and transformative impact in the Kyrgyz Tien Shan. Low-temperature thermochronology from multiple elevation profiles shows a marked increase in exhumation rates over the past ~3 Ma, coincident with the onset of major Pleistocene glaciations. New (U–Th–Sm)/He apatite ages from the Ala Archa and Enilcheck valleys record accelerated cooling between 0 and 3 Ma, and 3D thermal modelling attributes this signal to intensified valley incision rather than changes in tectonic uplift. The fact that this incision signal appears across valleys with different tectonic settings underscores the dominance of climate-driven glacial erosion, capable of overprinting local tectonic variability.
Together, these findings reveal the contrasting footprint of glaciation across temporal scales: Alpine denudation responds strongly only during major glacial maxima, whereas long-term exhumation in the Tien Shan is closely tied to the cumulative effects of repeated Pleistocene glaciations. This highlights both the complexity of glacial erosion and the need for multi-proxy approaches to disentangle climatic and tectonic controls on mountain evolution.
Sediment Transport and Flood Risk in Mountain Rivers
Now on LL's Youtube page: https://youtu.be/oRWuKuMw-Tg
Forest-landscape dynamics: Terrestrial Laser Scanning connects forest structure and landscape form in three dimensions
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Cancelled
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Resolving the impacts of earthquakes, storms, and prolonged rainfall on shallow landsliding
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Wiggles in width: Insights into alluvial channel dynamics from variability in high-resolution downstream hydraulic geometry
Talk is now on LL's YouTube channel: https://www.youtube.com/watch?v=BMizP1choAE