Articles | Volume 6, issue 2
https://doi.org/10.5194/esurf-6-271-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-6-271-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Estimates of late Cenozoic climate change relevant to Earth surface processes in tectonically active orogens
Sebastian G. Mutz
CORRESPONDING AUTHOR
Department of Geosciences, University Tübingen, 72074
Tübingen, Germany
Todd A. Ehlers
Department of Geosciences, University Tübingen, 72074
Tübingen, Germany
Martin Werner
Department of Paleoclimate Dynamics, Alfred Wegener Institute,
Helmholtz Centre for Polar and Marine Research, 27570 Bremerhaven, Germany
Gerrit Lohmann
Department of Paleoclimate Dynamics, Alfred Wegener Institute,
Helmholtz Centre for Polar and Marine Research, 27570 Bremerhaven, Germany
Christian Stepanek
Department of Paleoclimate Dynamics, Alfred Wegener Institute,
Helmholtz Centre for Polar and Marine Research, 27570 Bremerhaven, Germany
Jingmin Li
Department of Geosciences, University Tübingen, 72074
Tübingen, Germany
now at: Institute for Geography and Geology, University of
Würzburg, Würzburg, 97074 Germany
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31 citations as recorded by crossref.
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- Comparison of climate change from Cenozoic surface uplift and glacial-interglacial episodes in the Himalaya-Tibet region: Insights from a regional climate model and proxy data H. Paeth et al. 10.1016/j.gloplacha.2019.03.005
- Coupled surface to deep Earth processes: Perspectives from TOPO-EUROPE with an emphasis on climate- and energy-related societal challenges S. Cloetingh et al. 10.1016/j.gloplacha.2023.104140
- Bias and error in modelling thermochronometric data: resolving a potential increase in Plio-Pleistocene erosion rate S. Willett et al. 10.5194/esurf-9-1153-2021
- Tectonic and climatic forcing of chemical weathering intensity in the northeastern Tibetan Plateau since the middle Miocene H. Fu et al. 10.1016/j.catena.2021.105785
- Miocene high elevation in the Central Alps E. Krsnik et al. 10.5194/se-12-2615-2021
- Differential depression of the glacier equilibrium-line altitudes in the Yarlung Zangbo Downstream Basin in the Last Glacial Maximum compared to the pre-industrial era H. Li et al. 10.1007/s11442-024-2243-x
- Milankovitch-paced erosion in the southern Central Andes G. Fisher et al. 10.1038/s41467-023-36022-0
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- Constraining the exhumation history of the Greater Himalayan Sequence, Kali Gandaki, Central Nepal A. Pye et al. 10.1144/jgs2023-100
- Pedogenic and microbial interrelations to regional climate and local topography: New insights from a climate gradient (arid to humid) along the Coastal Cordillera of Chile N. Bernhard et al. 10.1016/j.catena.2018.06.018
- How steady are steady-state mountain belts? A reexamination of the Olympic Mountains (Washington state, USA) L. Michel et al. 10.5194/esurf-7-275-2019
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- Niches and radiations: a case study on the Andean sapphire‐vented puffleg Eriocnemis luciani and coppery‐naped puffleg E. sapphiropygia (Aves, Trochilidae) P. Ramoni‐Perazzi et al. 10.1111/jav.02242
- Past, present, and future geo-biosphere interactions on the Tibetan Plateau and implications for permafrost T. Ehlers et al. 10.1016/j.earscirev.2022.104197
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Discussed (final revised paper)
Discussed (preprint)
Latest update: 14 Dec 2024
Short summary
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...