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.
For centuries, geologists have debated the erosive power of glaciation. At one extreme, glaciers and ice sheets have been viewed as non-erosive protective blankets, while at the other extreme, they are considered among Earth’s most potent erosive forces. Consequently, the question of whether glaciers or rivers are, on average, more effective erosive agents remains contentious. This problem is further complicated by the “Sadler effect,” which describes how erosion and deposition rates appear to decrease as the timescale of observation increases, posing a considerable challenge for directly comparing glacial and fluvial erosion rates. The Sadlerian dilemma is particularly relevant to discussions of Cenozoic paleoclimate, where intensified erosion due to enhanced glaciation has been argued to be both a cause and consequence of Cenozoic cooling.
In this presentation, we present a comprehensive global compilation of glacial and fluvial erosion rates supplemented by simple numerical experiments. Our analysis shows that globally averaged glacial erosion rates surpass fluvial erosion rates by an order of magnitude (0.51 mm/year vs. 0.067 mm/year), a difference that cannot be attributed to the Sadler effect. We further demonstrate that the Sadler effect arises from three distinct biases: a measurement thickness bias (primarily related to the average penetration depth of cosmic rays into rocks), an erosion-redeposition bias (reflecting the bidirectional nature of certain geological processes whereby previous progress may be undone), and a non-observation bias (resulting from unobserved erosionally or depositionally quiescent intervals). Collectively, these findings support the notion that erosion rates increased with Cenozoic cooling and glaciation, highlighting the global importance of glacial erosion across diverse timescales.
Zoom link: https://gfz-de.zoom-x.de/meeting/register/0ELr2ojrSOW3thSRgSm3bw
Joel's Google Scholar: https://scholar.google.com/citations?user=zfRosDIAAAAJ&hl=en
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Andrew's website: https://research.monash.edu/en/persons/andrew-gunn
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Zhiwei's website: https://scholar.google.com/citations?user=kZLbPDEAAAAJ&hl=en
Now on LL's Youtube page: https://www.lboro.ac.uk/subjects/geography-environment/staff/dan-parsons/
Now on LL's Youtube page: https://www.youtube.com/watch?v=lfQbh_p3G2c
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Presentation now on LL's Youtube page: https://www.youtube.com/watch?v=1xGKVL-2HMc
Presentation now on LL's Youtube page: https://youtu.be/4-3VU0iVf6s
Talk is now on LL's Youtube channel: https://youtu.be/6uOiu98vCjM
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Resolving the impacts of earthquakes, storms, and prolonged rainfall on shallow landsliding
Talk is now on LL's YouTube channel: https://www.youtube.com/watch?v=72yxOMXzfNs
Talk is now on LL's YouTube channel: https://www.youtube.com/watch?v=uKF473Pv1No
Talk is now on LL's YouTube channel: https://www.youtube.com/watch?v=SQQFXh5aYIw
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Talk is now on LL's YouTube channel: https://www.youtube.com/watch?v=38oT5MwHgX4
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