Skip to Main content Skip to Navigation
New interface
Journal articles

Influence of Climate‐Forcing Frequency on Hillslope Response

Abstract : Assessing rivers' and hillslopes' sensitivity to external forcing is paramount to understand landscape evolution, in particular as a response to Quaternary climate changes. River networks are usually considered to be the main conveyors of environmental signals, such as changes in precipitation, temperature, or baselevel. Yet because hillslopes provide the source of sediment for river networks, their response to environmental change also modulates landscape dynamics. In order to characterize such behavior, we analyze the response times of a transport-limited hillslope. We use simple numerical models of denudation to study hillslope responses to oscillatory forcing and understand their filtering effects on environmental signals. Modifications in the frequency of climate oscillation, such as the change that occurred at the Mid-Pleistocene Transition, can significantly modulate hillslope sediment-flux response. We infer a wide range of hillslope responses, ranging from negligible change over the full range of climate-forcing frequencies, to a significant filtering of long-period signals.
Complete list of metadata
Contributor : Vincent Godard Connect in order to contact the contributor
Submitted on : Friday, September 17, 2021 - 9:02:48 AM
Last modification on : Friday, April 1, 2022 - 3:47:09 AM
Long-term archiving on: : Saturday, December 18, 2021 - 6:17:24 PM


Files produced by the author(s)




V. Godard, G. Tucker. Influence of Climate‐Forcing Frequency on Hillslope Response. Geophysical Research Letters, 2021, 48 (18), ⟨10.1029/2021GL094305⟩. ⟨hal-03347189⟩



Record views


Files downloads