Detail of a photo: Large angular boulder beside a shallow pebbly stream in a grassy mountain valley, below steep forested slopes and rocky peaks under a dramatic blue sky, in heavily processed colours.
EGU Blogs

Division blogs

GM

A conversation with Fiona Clubb, GM Division Outstanding Early Career Scientist Awardee

A conversation with Fiona Clubb, GM Division Outstanding Early Career Scientist Awardee

  Recently, EGU announced the 2024 medals and awards to be presented at the General Assembly in April, and the winner of the Geomorphology Division Outstanding Early Career Scientist Award is Fiona Clubb, Assistant Professor in Earth Surface Processes at Durham University. Fiona is geomorphologist interested in interactions between tectonics, climate, and surface process shape …[Read More]

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Can we predict floods accurately, fast and everywhere?

Can we predict floods accurately, fast and everywhere?

The impact of climate change has already and will continue to cause frequent flooding episodes all over the world, with devastating consequences not only for our society but for our natural habitat as well, should we not take immediate action. Therefore, have you ever wondered, what would happen if there was an effective flood modelling …[Read More]

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Rotational seismology in short

Rotational seismology in short

Always wanted to know the basics of rotational seismology? Follow us into this short blogpost written by our ECS team member Andreas Brotzer. Let’s spin it … or rather rotate it. Most of us enjoy a good spin on a carousel or rollercoaster. Well, we are actually doing this permanently since we live on a …[Read More]

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Calculating postglacial sea-level change within few seconds: a statistical emulator for GIA

Calculating postglacial sea-level change within few seconds: a statistical emulator for GIA

Sea-level change serves as a direct indicator of climate change with profound implications for coastal areas. Since 1900, the global mean sea level (GMSL) has risen over 20 cm, leading to beach erosion, delta inundation, and increased flooding worldwide. Over glacial cycles spanning tens of thousands of years, interactions between ocean and continental-scale ice sheets …[Read More]