1. Impact of Tibetan lake outburst floods on erosion, morphology, and sedimentary record of the eastern Himalaya from source to sink
- Author
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Huntington, Katharine W., Morey, Susannah, Turzewski, Michael, Lang, Karl, Mueller, Megan, Montgomery, David R., Licht, Alexis, Goodbred, Steven, L., Pickering, Jennifer, Diamond, Michael S., Shobe, Charles, Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), and Licht, Alexis
- Subjects
[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology ,[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology - Abstract
International audience; The Tsangpo Gorge region of eastern Tibet is an exceptionally dynamic landscape, where the Yarlung-Siang-Brahmaputra River cuts through the high Himalaya in a zone of extremely localized rapid erosion and rock uplift. Quaternary megafloods (≥106 m3/s) sourced from valley blocking glaciers may have played an important role in the geomorphic evolution of the Gorge and Tibetan plateau margin. We investigate the sedimentary record and hydraulics of outburst floods through the Gorge, with implications for erosion and deposition in the largest source-to-sink sedimentary system on Earth.Within the Himalaya downstream of the Gorge, detrital zircon U-Pb and feldspar luminescence data from slackwater flood deposits suggest megaflood sands came from impoundments of the Yarlung River drainage immediately upstream or west of the Gorge. Megaflood deposits contain a disproportionately large number of zircons eroded from the Gorge compared to active bedload and historical landslide-dam-burst flood deposits from the same drainage. This observation cannot be explained by sediment recycling. Rather, it reflects preferential erosion of the Gorge during megafloods, supporting the hypothesis that megafloods are a primary contributor to rapid exhumation of the region.A numerically simulated flood sourced from a reconstructed 81 km3 glacial lake impoundment immediately upstream of the Gorge reaches peak discharge of 2.6x106 m3/s and flow speeds up to 70 m/s, inundating hillslopes up to 250 m above the modern channel. Tributaries experience 8-60 km of backflow inundation. Simulated megaflood power and energy expenditure is over an order of magnitude higher than that of the modern river, showing the high erosive potential of megafloods in the Gorge. Hydraulic simulations, field observations, and process-based numerical models suggest a lasting impact of megaflood deposits on channel/valley form and processes.Downstream observations show that megafloods have significantly altered landscapes in the sedimentary transfer zone between the headwaters and deepwater Bengal Fan and deposited material >2000 km offshore. Our findings show the profound legacy of these episodic, large magnitude floods on mountain valley processes and on the transmission and preservation of tectonic and climatic signals in the sedimentary record.
- Published
- 2021