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
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Cited
18 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
- 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
- Hemispheric Asymmetry of Tropical Expansion Under CO 2 Forcing O. Watt‐Meyer et al. 10.1029/2019GL083695
- 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
- 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
- LongRunMIP: Motivation and Design for a Large Collection of Millennial-Length AOGCM Simulations M. Rugenstein et al. 10.1175/BAMS-D-19-0068.1
- Twenty first century changes in Antarctic and Southern Ocean surface climate in CMIP6 T. Bracegirdle et al. 10.1002/asl.984
- Does polar amplification exist in Antarctic surface during the recent four decades? S. Wang et al. 10.1007/s11629-021-6912-2
- Arctic Amplification of Precipitation Changes—The Energy Hypothesis F. Pithan & T. Jung 10.1029/2021GL094977
- Divergent global-scale temperature effects from identical aerosols emitted in different regions G. Persad & K. Caldeira 10.1038/s41467-018-05838-6
- 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
- Contributions to Polar Amplification in CMIP5 and CMIP6 Models L. Hahn et al. 10.3389/feart.2021.710036
- Prediction of Ice‐Free Conditions for a Perennially Ice‐Covered Antarctic Lake M. Obryk et al. 10.1029/2018JF004756
18 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
- 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
- Hemispheric Asymmetry of Tropical Expansion Under CO 2 Forcing O. Watt‐Meyer et al. 10.1029/2019GL083695
- 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
- 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
- LongRunMIP: Motivation and Design for a Large Collection of Millennial-Length AOGCM Simulations M. Rugenstein et al. 10.1175/BAMS-D-19-0068.1
- Twenty first century changes in Antarctic and Southern Ocean surface climate in CMIP6 T. Bracegirdle et al. 10.1002/asl.984
- Does polar amplification exist in Antarctic surface during the recent four decades? S. Wang et al. 10.1007/s11629-021-6912-2
- Arctic Amplification of Precipitation Changes—The Energy Hypothesis F. Pithan & T. Jung 10.1029/2021GL094977
- Divergent global-scale temperature effects from identical aerosols emitted in different regions G. Persad & K. Caldeira 10.1038/s41467-018-05838-6
- 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
- Contributions to Polar Amplification in CMIP5 and CMIP6 Models L. Hahn et al. 10.3389/feart.2021.710036
- Prediction of Ice‐Free Conditions for a Perennially Ice‐Covered Antarctic Lake M. Obryk et al. 10.1029/2018JF004756
Discussed (final revised paper)
Latest update: 28 Jun 2022
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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Final-revised paper
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