Articles | Volume 8, issue 2
https://doi.org/10.5194/esd-8-323-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esd-8-323-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| Highlight paper
| 
18 May 2017
Research article | Highlight paper |
| 18 May 2017
The polar amplification asymmetry: role of Antarctic surface height
Marc Salzmann
CORRESPONDING AUTHOR
Institute for Meteorology, Universität Leipzig, Vor dem
Hospitaltore 1, 04103 Leipzig, Germany
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Total article views: 7,431 (including HTML, PDF, and XML)
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Cited
31 citations as recorded by crossref.
- Arctic Ocean Surface Energy Flux and the Cold Halocline in Future Climate Projections E. Metzner et al. 10.1029/2019JC015554
- Low Antarctic continental climate sensitivity due to high ice sheet orography H. Singh & L. Polvani 10.1038/s41612-020-00143-w
- Antarctic Elevation Drives Hemispheric Asymmetry in Polar Lapse Rate Climatology and Feedback L. Hahn et al. 10.1029/2020GL088965
- Hemispheric Asymmetry of Tropical Expansion Under CO2 Forcing O. Watt‐Meyer et al. 10.1029/2019GL083695
- Process Drivers, Inter-Model Spread, and the Path Forward: A Review of Amplified Arctic Warming P. Taylor et al. 10.3389/feart.2021.758361
- Equilibrium Climate Sensitivity Estimated by Equilibrating Climate Models M. Rugenstein et al. 10.1029/2019GL083898
- Polar Amplification in the Earth’s Three Poles Based on MODIS Land Surface Temperatures A. Xie et al. 10.3390/rs15235566
- 21st Century Global and Regional Surface Temperature Projections N. Ma et al. 10.1029/2022EA002662
- Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models K. Hajjar & M. Salzmann 10.1002/qj.4496
- Does polar amplification exist in Antarctic surface during the recent four decades? S. Wang et al. 10.1007/s11629-021-6912-2
- Divergent global-scale temperature effects from identical aerosols emitted in different regions G. Persad & K. Caldeira 10.1038/s41467-018-05838-6
- Climate response to interhemispheric differences in radiative forcing governed by shortwave cloud feedbacks H. Kaur et al. 10.1088/2752-5295/ad8df6
- Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models F. Casagrande et al. 10.3390/atmos12111494
- Connecting Hemispheric Asymmetries of Planetary Albedo and Surface Temperature M. Rugenstein & M. Hakuba 10.1029/2022GL101802
- Polar Amplification: A Fractional Integration Analysis G. Caporale et al. 10.2139/ssrn.4803860
- Prediction of Ice‐Free Conditions for a Perennially Ice‐Covered Antarctic Lake M. Obryk et al. 10.1029/2018JF004756
- Contributions to regional precipitation change and its polar-amplified pattern under warming D. Bonan et al. 10.1088/2752-5295/ace27a
- The power spectrum of climate change A. Sneppen 10.1140/epjp/s13360-022-02773-w
- Hemispherically symmetric strategies for stratospheric aerosol injection Y. Zhang et al. 10.5194/esd-15-191-2024
- Changes in polar amplification in response to increasing warming in CMIP6 S. Cai et al. 10.1016/j.aosl.2021.100043
- Water vapor and lapse rate feedbacks in the climate system R. Colman & B. Soden 10.1103/RevModPhys.93.045002
- The quandary of detecting the signature of climate change in Antarctica M. Casado et al. 10.1038/s41558-023-01791-5
- How Asymmetries Between Arctic and Antarctic Climate Sensitivity Are Modified by the Ocean H. Singh et al. 10.1029/2018GL079023
- An inter-hemispheric seasonal comparison of polar amplification using radiative forcing of a quadrupling CO<sub>2</sub> experiment F. Casagrande et al. 10.5194/angeo-38-1123-2020
- Meridional Heat Transport in the DeepMIP Eocene Ensemble: Non‐CO2 and CO2 Effects F. Kelemen et al. 10.1029/2022PA004607
- Twenty first century changes in Antarctic and Southern Ocean surface climate in CMIP6 T. Bracegirdle et al. 10.1002/asl.984
- Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature J. Zhu et al. 10.3390/atmos14020218
- Arctic Amplification of Precipitation Changes—The Energy Hypothesis F. Pithan & T. Jung 10.1029/2021GL094977
- A Laboratory Model for a Meandering Zonal Jet K. Stewart & F. Macleod 10.1029/2021MS002943
- Polar climate change: a multidisciplinary assessment F. Casagrande et al. 10.26848/rbgf.v16.6.p3204-3224
- Contributions to Polar Amplification in CMIP5 and CMIP6 Models L. Hahn et al. 10.3389/feart.2021.710036
31 citations as recorded by crossref.
- Arctic Ocean Surface Energy Flux and the Cold Halocline in Future Climate Projections E. Metzner et al. 10.1029/2019JC015554
- Low Antarctic continental climate sensitivity due to high ice sheet orography H. Singh & L. Polvani 10.1038/s41612-020-00143-w
- Antarctic Elevation Drives Hemispheric Asymmetry in Polar Lapse Rate Climatology and Feedback L. Hahn et al. 10.1029/2020GL088965
- Hemispheric Asymmetry of Tropical Expansion Under CO2 Forcing O. Watt‐Meyer et al. 10.1029/2019GL083695
- Process Drivers, Inter-Model Spread, and the Path Forward: A Review of Amplified Arctic Warming P. Taylor et al. 10.3389/feart.2021.758361
- Equilibrium Climate Sensitivity Estimated by Equilibrating Climate Models M. Rugenstein et al. 10.1029/2019GL083898
- Polar Amplification in the Earth’s Three Poles Based on MODIS Land Surface Temperatures A. Xie et al. 10.3390/rs15235566
- 21st Century Global and Regional Surface Temperature Projections N. Ma et al. 10.1029/2022EA002662
- Relative contributions of local heat storage and ocean heat transport to cold‐season Arctic Ocean surface energy fluxes in CMIP6 models K. Hajjar & M. Salzmann 10.1002/qj.4496
- Does polar amplification exist in Antarctic surface during the recent four decades? S. Wang et al. 10.1007/s11629-021-6912-2
- Divergent global-scale temperature effects from identical aerosols emitted in different regions G. Persad & K. Caldeira 10.1038/s41467-018-05838-6
- Climate response to interhemispheric differences in radiative forcing governed by shortwave cloud feedbacks H. Kaur et al. 10.1088/2752-5295/ad8df6
- Polar Amplification and Ice Free Conditions under 1.5, 2 and 3 °C of Global Warming as Simulated by CMIP5 and CMIP6 Models F. Casagrande et al. 10.3390/atmos12111494
- Connecting Hemispheric Asymmetries of Planetary Albedo and Surface Temperature M. Rugenstein & M. Hakuba 10.1029/2022GL101802
- Polar Amplification: A Fractional Integration Analysis G. Caporale et al. 10.2139/ssrn.4803860
- Prediction of Ice‐Free Conditions for a Perennially Ice‐Covered Antarctic Lake M. Obryk et al. 10.1029/2018JF004756
- Contributions to regional precipitation change and its polar-amplified pattern under warming D. Bonan et al. 10.1088/2752-5295/ace27a
- The power spectrum of climate change A. Sneppen 10.1140/epjp/s13360-022-02773-w
- Hemispherically symmetric strategies for stratospheric aerosol injection Y. Zhang et al. 10.5194/esd-15-191-2024
- Changes in polar amplification in response to increasing warming in CMIP6 S. Cai et al. 10.1016/j.aosl.2021.100043
- Water vapor and lapse rate feedbacks in the climate system R. Colman & B. Soden 10.1103/RevModPhys.93.045002
- The quandary of detecting the signature of climate change in Antarctica M. Casado et al. 10.1038/s41558-023-01791-5
- How Asymmetries Between Arctic and Antarctic Climate Sensitivity Are Modified by the Ocean H. Singh et al. 10.1029/2018GL079023
- An inter-hemispheric seasonal comparison of polar amplification using radiative forcing of a quadrupling CO<sub>2</sub> experiment F. Casagrande et al. 10.5194/angeo-38-1123-2020
- Meridional Heat Transport in the DeepMIP Eocene Ensemble: Non‐CO2 and CO2 Effects F. Kelemen et al. 10.1029/2022PA004607
- Twenty first century changes in Antarctic and Southern Ocean surface climate in CMIP6 T. Bracegirdle et al. 10.1002/asl.984
- Assessment of Antarctic Amplification Based on a Reconstruction of Near-Surface Air Temperature J. Zhu et al. 10.3390/atmos14020218
- Arctic Amplification of Precipitation Changes—The Energy Hypothesis F. Pithan & T. Jung 10.1029/2021GL094977
- A Laboratory Model for a Meandering Zonal Jet K. Stewart & F. Macleod 10.1029/2021MS002943
- Polar climate change: a multidisciplinary assessment F. Casagrande et al. 10.26848/rbgf.v16.6.p3204-3224
- Contributions to Polar Amplification in CMIP5 and CMIP6 Models L. Hahn et al. 10.3389/feart.2021.710036
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
The Arctic has been warming much faster than the rest of the globe, including Antarctica. Here it was shown that one of the important mechanisms that sets Antarctica apart from the Arctic is heat transport from lower latitudes, and it was argued that a decrease in land height due to Antarctic melting would be favorable for increased atmospheric heat transport from midlatitudes. Other factors related to the larger Antarctic land height were also investigated.
The Arctic has been warming much faster than the rest of the globe, including Antarctica. Here...
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