Articles | Volume 3, issue 1
https://doi.org/10.5194/esurf-3-1-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esurf-3-1-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
05 Jan 2015
Research article |
| 05 Jan 2015
Erosional response of an actively uplifting mountain belt to cyclic rainfall variations
ISTerre, Université Grenoble Alpes and CNRS BP 53, 38041 Grenoble CEDEX 9, France
C. Voisin
ISTerre, Université Grenoble Alpes and CNRS BP 53, 38041 Grenoble CEDEX 9, France
A. T. Gourlan
ISTerre, Université Grenoble Alpes and CNRS BP 53, 38041 Grenoble CEDEX 9, France
C. Chauvel
ISTerre, Université Grenoble Alpes and CNRS BP 53, 38041 Grenoble CEDEX 9, France
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30 citations as recorded by crossref.
- The Response Time of Glacial Erosion F. Herman et al. 10.1002/2017JF004586
- Late Quaternary Tectonics, Incision, and Landscape Evolution of the Calchaquí River Catchment, Eastern Cordillera, NW Argentina J. McCarthy et al. 10.1029/2019JF005091
- The degradation and detection of environmental signals in sediment transport systems C. Griffin et al. 10.1126/sciadv.adi8046
- Geomorphic response to active tectonics: Numerical and field‐based approaches A. Demoulin et al. 10.1002/esp.4397
- Modulation of the erosion rate of an uplifting landscape by long-term climate change: An experimental investigation B. Moussirou & S. Bonnet 10.1016/j.geomorph.2017.12.010
- Quaternary Rock Uplift Rates and Their Implications for the Western Flank of the North Anatolian Fault Restraining Bend; Inferences From Fluvial Terrace Ages K. McClain et al. 10.1029/2019TC005993
- High‐resolution sedimentary budget quantification – Example from the Cenozoic deposits in the Pelotas Basin, South Atlantic S. Rohais et al. 10.1111/bre.12556
- Numerical modelling of landscape and sediment flux response to precipitation rate change J. Armitage et al. 10.5194/esurf-6-77-2018
- Anthropogenic impacts on Holocene fluvial dynamics in the Chinese Loess Plateau, an evaluation based on landscape evolution modeling H. Chen et al. 10.1016/j.geomorph.2021.107935
- Autogenic versus allogenic controls on the evolution of a coupled fluvial megafan–mountainous catchment system: numerical modelling and comparison with the Lannemezan megafan system (northern Pyrenees, France) M. Mouchené et al. 10.5194/esurf-5-125-2017
- Thickness of Fluvial Deposits Records Climate Oscillations X. Yuan et al. 10.1029/2021JB023510
- The CAIRN method: automated, reproducible calculation of catchment-averaged denudation rates from cosmogenic nuclide concentrations S. Mudd et al. 10.5194/esurf-4-655-2016
- Grand Challenges (and Great Opportunities) in Sedimentology, Stratigraphy, and Diagenesis Research D. Hodgson et al. 10.3389/feart.2018.00173
- Detection of transience in eroding landscapes S. Mudd 10.1002/esp.3923
- The Importance of Hillslope Scale in Responses of Chemical Erosion Rate to Changes in Tectonics and Climate K. Ferrier & J. Perron 10.1029/2020JF005562
- Autogenic geomorphic processes determine the resolution and fidelity of terrestrial paleoclimate records B. Foreman & K. Straub 10.1126/sciadv.1700683
- Milankovitch-paced erosion in the southern Central Andes G. Fisher et al. 10.1038/s41467-023-36022-0
- Deciphering the origin of cyclical gravel front and shoreline progradation and retrogradation in the stratigraphic record J. Armitage et al. 10.1111/bre.12203
- Times Associated With Source-to-Sink Propagation of Environmental Signals During Landscape Transience S. Tofelde et al. 10.3389/feart.2021.628315
- The impact of extreme El Niño events on modern sediment transport along the western Peruvian Andes (1968–2012) S. Morera et al. 10.1038/s41598-017-12220-x
- Mass balance, grade, and adjustment timescales in bedrock channels J. Turowski 10.5194/esurf-8-103-2020
- Alluvial plains formation in response to 100-ka glacial–interglacial cycles since the Middle Pleistocene in the southern Tian Shan, NW China W. Huang et al. 10.1016/j.geomorph.2019.05.013
- Tectonic Accretion Controls Erosional Cyclicity in the Himalaya S. Mandal et al. 10.1029/2021AV000487
- Influence of Climate‐Forcing Frequency on Hillslope Response V. Godard & G. Tucker 10.1029/2021GL094305
- 100 kyr fluvial cut-and-fill terrace cycles since the Middle Pleistocene in the southern Central Andes, NW Argentina S. Tofelde et al. 10.1016/j.epsl.2017.06.001
- Changes in Indian Summer Monsoon Using Neodymium (Nd) Isotopes in the Andaman Sea During the Last 24,000 years H. Rashid et al. 10.1007/s41748-019-00105-0
- Effect of rock uplift and Milankovitch timescale variations in precipitation and vegetation cover on catchment erosion rates H. Sharma et al. 10.5194/esurf-9-1045-2021
- Late Pleistocene - Holocene development of the Tista megafan (West Bengal, India): 10Be cosmogenic and IRSL age constraints R. Abrahami et al. 10.1016/j.quascirev.2018.02.001
- Fluvial archives, a valuable record of vertical crustal deformation A. Demoulin et al. 10.1016/j.quascirev.2016.11.011
- Diverse Responses of Alluvial Rivers to Periodic Environmental Change F. MNab et al. 10.1029/2023GL103075
1 citations as recorded by crossref.
Saved (final revised paper)
Latest update: 13 Dec 2024
Short summary
We have derived a simple solution to the stream power law equation governing the erosion of rapidly uplifting tectonic areas assuming that rainfall varies as a periodic function of time. We show that the erosional response of this forcing is characterized by an amplification of the resulting erosional flux variations as well as a time lag. We show how this time lag can be important in interpreting several geological observations.
We have derived a simple solution to the stream power law equation governing the erosion of...
