ERC Advanced Grant · 2018
Climatic Controls on Erosion Rates and Relief of Mountain Belts
Quantifying the feedbacks between tectonic processes in the lithosphere and climatic processes in the atmosphere is an overarching goal in Earth-Systems research, as it underpins our ability to differentiate natural from anthropogenic climate forcing. Long-term cooling during the Cenozoic has been linked to the growth of mountain belts, which enhanced erosion, chemical weathering, organic-carbon burial and drawdown of atmospheric CO2. Conversely, it has been proposed that the cooler and more variable climate of the late Cenozoic led to increased topographic relief and erosion. This latter coupling, however, has not been decisively demonstrated and remains highly controversial. Advancing our…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.