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ESurf | Articles | Volume 6, issue 2
Earth Surf. Dynam., 6, 271–301, 2018
https://doi.org/10.5194/esurf-6-271-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Surf. Dynam., 6, 271–301, 2018
https://doi.org/10.5194/esurf-6-271-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 06 Apr 2018

Research article | 06 Apr 2018

Estimates of late Cenozoic climate change relevant to Earth surface processes in tectonically active orogens

Sebastian G. Mutz et al.
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Cited articles  
Abe-Ouchi, A., Saito, F., Kageyama, M., Braconnot, P., Harrison, S. P., Lambeck, K., Otto-Bliesner, B. L., Peltier, W. R., Tarasov, L., Peterschmitt, J.-Y., and Takahashi, K.: Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments, Geosci. Model Dev., 8, 3621–3637, https://doi.org/10.5194/gmd-8-3621-2015, 2015. 
Andersen, J. L., Egholm, D. L., Knudsen, M. F., Jansen, J. D., and Nielsen, S. B.: The periglacial engine of mountain erosion – Part 1: Rates of frost cracking and frost creep, Earth Surf. Dynam., 3, 447–462, https://doi.org/10.5194/esurf-3-447-2015, 2015. 
Arnold, L., Breon, F. M., and Brewer, S: The earth as an extrasolar planet: the vegetation spectral signature today and during the last Quaternary climatic extrema, Int. J. Astrobiol., 8, 81–94, https://doi.org/10.1017/S1473550409004406, 2009. 
Asahi, K.: Equilibrium-line altitudes of the present and Last Glacial Maximum in the eastern Nepal Himalayas and their implications for SW monsoon climate, Quatern. Int., 212, 26–34, https://doi.org/10.1016/j.quaint.2008.08.004, 2010. 
Bahrenberg, G., Giese, E., and Nipper, J.: Multivariate Statistik, Statistische Methoden in der Geographie 2, Stuttgart, 1992. 
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We use a climate model and statistics to provide an overview of regional climates from different times in the late Cenozoic. We focus on tectonically active mountain ranges in particular. Our results highlight significant changes in climates throughout the late Cenozoic, which should be taken into consideration when interpreting erosion rates. We also document the differences between model- and proxy-based estimates for late Cenozoic climate change in South America and Tibet.
We use a climate model and statistics to provide an overview of regional climates from different...
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