Articles | Volume 12, issue 6
https://doi.org/10.5194/cp-12-1401-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1401-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impacts of Tibetan Plateau uplift on atmospheric dynamics and associated precipitation δ18O
Svetlana Botsyun
CORRESPONDING AUTHOR
Laboratoire des Sciences du Climat et de l'Environnement,
LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette,
France
Pierre Sepulchre
Laboratoire des Sciences du Climat et de l'Environnement,
LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette,
France
Camille Risi
Laboratoire de Météorologie Dynamique, LMD/IPSL,
UPMC, CNRS, Paris, France
Yannick Donnadieu
Laboratoire des Sciences du Climat et de l'Environnement,
LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette,
France
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Cited
35 citations as recorded by crossref.
- The evolution of hydroclimate in Asia over the Cenozoic: A stable-isotope perspective J. Caves Rugenstein & C. Chamberlain 10.1016/j.earscirev.2018.09.003
- Timing and mechanisms of Tibetan Plateau uplift L. Ding et al. 10.1038/s43017-022-00318-4
- Spatial distribution and controlling factors of stable isotopes in meteoric waters on the Tibetan Plateau: Implications for paleoelevation reconstruction L. Li & C. Garzione 10.1016/j.epsl.2016.11.046
- Lower-altitude of the Himalayas before the mid-Pliocene as constrained by hydrological and thermal conditions C. Chen et al. 10.1016/j.epsl.2020.116422
- Temperature–topographic elevation relationship for high mountain terrain: an example from the southeastern Tibetan Plateau D. Kattel & T. Yao 10.1002/joc.5418
- Some Illustrations of Large Tectonically Driven Climate Changes in Earth History G. Ramstein et al. 10.1029/2019TC005569
- Changes in Tibetan Plateau latitude as an important factor for understanding East Asian climate since the Eocene: A modeling study R. Zhang et al. 10.1016/j.epsl.2017.12.034
- How Can Climate Models Be Used in Paleoelevation Reconstructions? S. Botsyun & T. Ehlers 10.3389/feart.2021.624542
- High-resolution simulation of Asian monsoon response to regional uplift of the Tibetan Plateau with regional climate model nested with global climate model E. Yu et al. 10.1016/j.gloplacha.2018.07.002
- Precipitation <i>δ</i><sup>18</sup>O on the Himalaya–Tibet orogeny and its relationship to surface elevation H. Shen & C. Poulsen 10.5194/cp-15-169-2019
- Interpreting precipitation δ18O over eastern China for the Asian summer monsoon: Results from the last millennium simulations Y. Liu et al. 10.1002/joc.8171
- Miocene high elevation in the Central Alps E. Krsnik et al. 10.5194/se-12-2615-2021
- Topographic growth of the Jishi Shan and its impact on basin and hydrology evolution, NE Tibetan Plateau J. Saylor et al. 10.1111/bre.12264
- Asian monsoons and aridification response to Paleogene sea retreat and Neogene westerly shielding indicated by seasonality in Paratethys oysters L. Bougeois et al. 10.1016/j.epsl.2017.12.036
- Revised paleoaltimetry data show low Tibetan Plateau elevation during the Eocene S. Botsyun et al. 10.1126/science.aaq1436
- Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma F. Poblete et al. 10.1016/j.earscirev.2021.103508
- Impact of topography, climate and moisture sources on isotopic composition (δ18O & δD) of rivers in the Pyrenees: Implications for topographic reconstructions in small orogens D. Huyghe et al. 10.1016/j.epsl.2017.12.035
- Influence of Large‐Scale Atmospheric Dynamics on Precipitation Seasonality of the Tibetan Plateau and Central Asia in Cold and Warm Climates During the Late Cenozoic S. Botsyun et al. 10.1029/2021JD035810
- 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
- Stable Isotopes Reveal the Effect of Canopy and Litter Layer Interception on Water Recharge in a Subtropical Manmade Forest of Southwest China C. Xia et al. 10.3390/f14010129
- How high were these mountains? D. van Hinsbergen & L. Boschman 10.1126/science.aaw7705
- Organic Molecular Paleohypsometry: A New Approach to Quantifying Paleotopography and Paleorelief M. Hren & W. Ouimet 10.3389/feart.2021.665324
- Reconstructing early Eocene (∼55 Ma) paleogeographic boundary conditions for use in paleoclimate modelling Z. He et al. 10.1007/s11430-019-9366-2
- Difference between the North Atlantic and Pacific meridional overturning circulation in response to the uplift of the Tibetan Plateau B. Su et al. 10.5194/cp-14-751-2018
- Responses of sedimentary δ2Halk values to environmental changes as revealed by different plant responses to altitude and altitude-related temperatures Y. Bai et al. 10.1016/j.scitotenv.2020.138087
- Paleoelevation reconstruction of the Paleocene-Eocene Gonjo basin, SE-central Tibet M. Tang et al. 10.1016/j.tecto.2017.05.018
- The influence of ice sheets on temperature during the past 38 million years inferred from a one-dimensional ice sheet–climate model L. Stap et al. 10.5194/cp-13-1243-2017
- Where did the Arizona‐Plano Go? Protracted Thinning Via Upper‐ to Lower‐Crustal Processes G. Jepson et al. 10.1029/2021JB023850
- Middle Miocene Climate and Stable Oxygen Isotopes in Europe Based on Numerical Modeling S. Botsyun et al. 10.1029/2022PA004442
- Variability of Isotope Composition of Precipitation in the Southeastern Tibetan Plateau from the Synoptic to Seasonal Time Scale X. Shi et al. 10.1029/2019JD031751
- The role of paleogeography in Asian monsoon evolution: a review and new insights from climate modelling D. Tardif et al. 10.1016/j.earscirev.2023.104464
- Climate heterogeneity shapes phylogeographic pattern of Hippophae gyantsensis (Elaeagnaceae) in the east Himalaya‐Hengduan Mountains T. Xu et al. 10.1002/ece3.10182
- Post-glacial climate forcing of surface processes in the Ganges–Brahmaputra river basin and implications for carbon sequestration C. Hein et al. 10.1016/j.epsl.2017.08.013
- Effects of the uplifts of the main and marginal Tibetan Plateau on the Asian climate under modern and ~30 Ma boundary conditions R. Zhang et al. 10.1016/j.palaeo.2017.12.022
- Limits of oxygen isotope palaeoaltimetry in Tibet A. Farnsworth et al. 10.1016/j.epsl.2023.118040
35 citations as recorded by crossref.
- The evolution of hydroclimate in Asia over the Cenozoic: A stable-isotope perspective J. Caves Rugenstein & C. Chamberlain 10.1016/j.earscirev.2018.09.003
- Timing and mechanisms of Tibetan Plateau uplift L. Ding et al. 10.1038/s43017-022-00318-4
- Spatial distribution and controlling factors of stable isotopes in meteoric waters on the Tibetan Plateau: Implications for paleoelevation reconstruction L. Li & C. Garzione 10.1016/j.epsl.2016.11.046
- Lower-altitude of the Himalayas before the mid-Pliocene as constrained by hydrological and thermal conditions C. Chen et al. 10.1016/j.epsl.2020.116422
- Temperature–topographic elevation relationship for high mountain terrain: an example from the southeastern Tibetan Plateau D. Kattel & T. Yao 10.1002/joc.5418
- Some Illustrations of Large Tectonically Driven Climate Changes in Earth History G. Ramstein et al. 10.1029/2019TC005569
- Changes in Tibetan Plateau latitude as an important factor for understanding East Asian climate since the Eocene: A modeling study R. Zhang et al. 10.1016/j.epsl.2017.12.034
- How Can Climate Models Be Used in Paleoelevation Reconstructions? S. Botsyun & T. Ehlers 10.3389/feart.2021.624542
- High-resolution simulation of Asian monsoon response to regional uplift of the Tibetan Plateau with regional climate model nested with global climate model E. Yu et al. 10.1016/j.gloplacha.2018.07.002
- Precipitation <i>δ</i><sup>18</sup>O on the Himalaya–Tibet orogeny and its relationship to surface elevation H. Shen & C. Poulsen 10.5194/cp-15-169-2019
- Interpreting precipitation δ18O over eastern China for the Asian summer monsoon: Results from the last millennium simulations Y. Liu et al. 10.1002/joc.8171
- Miocene high elevation in the Central Alps E. Krsnik et al. 10.5194/se-12-2615-2021
- Topographic growth of the Jishi Shan and its impact on basin and hydrology evolution, NE Tibetan Plateau J. Saylor et al. 10.1111/bre.12264
- Asian monsoons and aridification response to Paleogene sea retreat and Neogene westerly shielding indicated by seasonality in Paratethys oysters L. Bougeois et al. 10.1016/j.epsl.2017.12.036
- Revised paleoaltimetry data show low Tibetan Plateau elevation during the Eocene S. Botsyun et al. 10.1126/science.aaq1436
- Towards interactive global paleogeographic maps, new reconstructions at 60, 40 and 20 Ma F. Poblete et al. 10.1016/j.earscirev.2021.103508
- Impact of topography, climate and moisture sources on isotopic composition (δ18O & δD) of rivers in the Pyrenees: Implications for topographic reconstructions in small orogens D. Huyghe et al. 10.1016/j.epsl.2017.12.035
- Influence of Large‐Scale Atmospheric Dynamics on Precipitation Seasonality of the Tibetan Plateau and Central Asia in Cold and Warm Climates During the Late Cenozoic S. Botsyun et al. 10.1029/2021JD035810
- 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
- Stable Isotopes Reveal the Effect of Canopy and Litter Layer Interception on Water Recharge in a Subtropical Manmade Forest of Southwest China C. Xia et al. 10.3390/f14010129
- How high were these mountains? D. van Hinsbergen & L. Boschman 10.1126/science.aaw7705
- Organic Molecular Paleohypsometry: A New Approach to Quantifying Paleotopography and Paleorelief M. Hren & W. Ouimet 10.3389/feart.2021.665324
- Reconstructing early Eocene (∼55 Ma) paleogeographic boundary conditions for use in paleoclimate modelling Z. He et al. 10.1007/s11430-019-9366-2
- Difference between the North Atlantic and Pacific meridional overturning circulation in response to the uplift of the Tibetan Plateau B. Su et al. 10.5194/cp-14-751-2018
- Responses of sedimentary δ2Halk values to environmental changes as revealed by different plant responses to altitude and altitude-related temperatures Y. Bai et al. 10.1016/j.scitotenv.2020.138087
- Paleoelevation reconstruction of the Paleocene-Eocene Gonjo basin, SE-central Tibet M. Tang et al. 10.1016/j.tecto.2017.05.018
- The influence of ice sheets on temperature during the past 38 million years inferred from a one-dimensional ice sheet–climate model L. Stap et al. 10.5194/cp-13-1243-2017
- Where did the Arizona‐Plano Go? Protracted Thinning Via Upper‐ to Lower‐Crustal Processes G. Jepson et al. 10.1029/2021JB023850
- Middle Miocene Climate and Stable Oxygen Isotopes in Europe Based on Numerical Modeling S. Botsyun et al. 10.1029/2022PA004442
- Variability of Isotope Composition of Precipitation in the Southeastern Tibetan Plateau from the Synoptic to Seasonal Time Scale X. Shi et al. 10.1029/2019JD031751
- The role of paleogeography in Asian monsoon evolution: a review and new insights from climate modelling D. Tardif et al. 10.1016/j.earscirev.2023.104464
- Climate heterogeneity shapes phylogeographic pattern of Hippophae gyantsensis (Elaeagnaceae) in the east Himalaya‐Hengduan Mountains T. Xu et al. 10.1002/ece3.10182
- Post-glacial climate forcing of surface processes in the Ganges–Brahmaputra river basin and implications for carbon sequestration C. Hein et al. 10.1016/j.epsl.2017.08.013
- Effects of the uplifts of the main and marginal Tibetan Plateau on the Asian climate under modern and ~30 Ma boundary conditions R. Zhang et al. 10.1016/j.palaeo.2017.12.022
- Limits of oxygen isotope palaeoaltimetry in Tibet A. Farnsworth et al. 10.1016/j.epsl.2023.118040
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Short summary
We use an isotope-equipped GCM and develop original theoretical expression for the precipitation composition to assess δ18O of paleo-precipitation changes with the Tibetan Plateau uplift. We show that δ18O of precipitation is very sensitive to climate changes related to the growth of mountains, notably changes in relative humidity and precipitation amount. Topography is shown to be not an exclusive controlling factor δ18O in precipitation that have crucial consequences for paleoelevation studies
We use an isotope-equipped GCM and develop original theoretical expression for the precipitation...