On 28th November OxTalks will move to the new Halo platform and will become 'Oxford Events' (full details are available on the Staff Gateway).
There will be an OxTalks freeze beginning on Friday 14th November. This means you will need to publish any of your known events to OxTalks by then as there will be no facility to publish or edit events in that fortnight. During the freeze, all events will be migrated to the new Oxford Events site. It will still be possible to view events on OxTalks during this time.
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Rivers originating in High Mountain Asia (HMA) are crucial lifelines for approximately one-third of the world’s population. These fragile headwater rivers are now experiencing amplified climate change, glacier melt, and permafrost thaw. The rapid climate change and melting and thawing of the cryosphere are not only affecting the water cycle but also influencing the sediment erosion and transport. In this talk, I will give an overview of how modern climate change drives the substantial increases in the fluvial sediment loads in the glacier and permafrost landscapes of HMA. I will also discuss the implications of the increasing fluvial sediment loads for water quality, hydropower, floods, carbon cycling and thus securities of energy-food-environment in the region and beyond.
