Articles | Volume 14, issue 8
https://doi.org/10.5194/tc-14-2673-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-2673-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Clouds damp the radiative impacts of polar sea ice loss
Ramdane Alkama
CORRESPONDING AUTHOR
European Commission – Joint Research Centre, Via Enrico Fermi, 2749,
21027 Ispra (VA), Italy
Patrick C. Taylor
CORRESPONDING AUTHOR
NASA Langley Research Center, Hampton, Virginia, USA
Lorea Garcia-San Martin
European Commission – Joint Research Centre, Via Enrico Fermi, 2749,
21027 Ispra (VA), Italy
Herve Douville
Centre National de Recherches Météorologiques, Météo-France/CNRS,
Toulouse, France
Gregory Duveiller
European Commission – Joint Research Centre, Via Enrico Fermi, 2749,
21027 Ispra (VA), Italy
Giovanni Forzieri
European Commission – Joint Research Centre, Via Enrico Fermi, 2749,
21027 Ispra (VA), Italy
Didier Swingedouw
EPOC, Université de Bordeaux, Allée Geoffroy Saint-Hilaire,
Pessac 33615, France
Alessandro Cescatti
European Commission – Joint Research Centre, Via Enrico Fermi, 2749,
21027 Ispra (VA), Italy
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Cited
21 citations as recorded by crossref.
- On the Association of the Summertime Shortwave Cloud Radiative Effect in Northern Russia With Atmospheric Circulation and Climate Over East Asia L. Liu et al. 10.1029/2021GL096606
- Oceanic Supply of Ice‐Nucleating Particles and Its Effect on Ice Cloud Formation: A Case Study in the Arctic Ocean During a Cold‐Air Outbreak in Early Winter J. Inoue et al. 10.1029/2021GL094646
- Arctic Cloud Response to a Perturbation in Sea Ice Concentration: The North Water Polynya E. Monroe et al. 10.1029/2020JD034409
- Arctic amplification of climate change: a review of underlying mechanisms M. Previdi et al. 10.1088/1748-9326/ac1c29
- Wind amplifies the polar sea ice retreat R. Alkama et al. 10.1088/1748-9326/abc379
- A Cloudier Picture of Ice-Albedo Feedback in CMIP6 Models A. Sledd & T. L’Ecuyer 10.3389/feart.2021.769844
- Understanding Sea Surface Temperature Cooling in the Central‐East Pacific Sector of the Southern Ocean During 1982–2020 X. Xu et al. 10.1029/2021GL097579
- The Representation of Sea Salt Aerosols and Their Role in Polar Climate Within CMIP6 R. Lapere et al. 10.1029/2022JD038235
- Evaluation of simulated cloud liquid water in low clouds over the Beaufort Sea in the Arctic System Reanalysis using ARISE airborne in situ observations J. Dodson et al. 10.5194/acp-21-11563-2021
- Assessment of CMIP6 Multi-Model Projections Worldwide: Which Regions Are Getting Warmer and Are Going through a Drought in Africa and Morocco? What Changes from CMIP5 to CMIP6? A. Bouramdane 10.3390/su15010690
- An Entropy Generation Rate Model for Tropospheric Behavior That Includes Cloud Evolution J. Sekhar 10.3390/e25121625
- Links between atmospheric aerosols and sea state in the Arctic Ocean A. Moallemi et al. 10.1016/j.atmosenv.2024.120844
- Changes in polar amplification in response to increasing warming in CMIP6 S. Cai et al. 10.1016/j.aosl.2021.100043
- Process Drivers, Inter-Model Spread, and the Path Forward: A Review of Amplified Arctic Warming P. Taylor et al. 10.3389/feart.2021.758361
- Isolating the Surface Type Influence on Arctic Low‐Clouds P. Taylor & E. Monroe 10.1029/2022JD038098
- Clouds Increasingly Influence Arctic Sea Surface Temperatures as CO2 Rises A. Sledd et al. 10.1029/2023GL102850
- Open Water in Sea Ice Causes High Bias in Polar Low‐Level Clouds in GFDL CM4 X. Li et al. 10.1029/2023GL106322
- A Quantitative Analysis of the Source of Inter‐Model Spread in Arctic Surface Warming Response to Increased CO2 Concentration X. Hu et al. 10.1029/2022GL100034
- Emerging Trends in Arctic Solar Absorption A. Sledd & T. L’Ecuyer 10.1029/2021GL095813
- Radiative effects of precipitation on the global energy budget and Arctic amplification T. Michibata 10.1038/s41612-024-00684-4
- Influence of spring Arctic sea ice melt on Eurasian surface air temperature X. Zhang et al. 10.1007/s00382-022-06267-4
20 citations as recorded by crossref.
- On the Association of the Summertime Shortwave Cloud Radiative Effect in Northern Russia With Atmospheric Circulation and Climate Over East Asia L. Liu et al. 10.1029/2021GL096606
- Oceanic Supply of Ice‐Nucleating Particles and Its Effect on Ice Cloud Formation: A Case Study in the Arctic Ocean During a Cold‐Air Outbreak in Early Winter J. Inoue et al. 10.1029/2021GL094646
- Arctic Cloud Response to a Perturbation in Sea Ice Concentration: The North Water Polynya E. Monroe et al. 10.1029/2020JD034409
- Arctic amplification of climate change: a review of underlying mechanisms M. Previdi et al. 10.1088/1748-9326/ac1c29
- Wind amplifies the polar sea ice retreat R. Alkama et al. 10.1088/1748-9326/abc379
- A Cloudier Picture of Ice-Albedo Feedback in CMIP6 Models A. Sledd & T. L’Ecuyer 10.3389/feart.2021.769844
- Understanding Sea Surface Temperature Cooling in the Central‐East Pacific Sector of the Southern Ocean During 1982–2020 X. Xu et al. 10.1029/2021GL097579
- The Representation of Sea Salt Aerosols and Their Role in Polar Climate Within CMIP6 R. Lapere et al. 10.1029/2022JD038235
- Evaluation of simulated cloud liquid water in low clouds over the Beaufort Sea in the Arctic System Reanalysis using ARISE airborne in situ observations J. Dodson et al. 10.5194/acp-21-11563-2021
- Assessment of CMIP6 Multi-Model Projections Worldwide: Which Regions Are Getting Warmer and Are Going through a Drought in Africa and Morocco? What Changes from CMIP5 to CMIP6? A. Bouramdane 10.3390/su15010690
- An Entropy Generation Rate Model for Tropospheric Behavior That Includes Cloud Evolution J. Sekhar 10.3390/e25121625
- Links between atmospheric aerosols and sea state in the Arctic Ocean A. Moallemi et al. 10.1016/j.atmosenv.2024.120844
- Changes in polar amplification in response to increasing warming in CMIP6 S. Cai et al. 10.1016/j.aosl.2021.100043
- Process Drivers, Inter-Model Spread, and the Path Forward: A Review of Amplified Arctic Warming P. Taylor et al. 10.3389/feart.2021.758361
- Isolating the Surface Type Influence on Arctic Low‐Clouds P. Taylor & E. Monroe 10.1029/2022JD038098
- Clouds Increasingly Influence Arctic Sea Surface Temperatures as CO2 Rises A. Sledd et al. 10.1029/2023GL102850
- Open Water in Sea Ice Causes High Bias in Polar Low‐Level Clouds in GFDL CM4 X. Li et al. 10.1029/2023GL106322
- A Quantitative Analysis of the Source of Inter‐Model Spread in Arctic Surface Warming Response to Increased CO2 Concentration X. Hu et al. 10.1029/2022GL100034
- Emerging Trends in Arctic Solar Absorption A. Sledd & T. L’Ecuyer 10.1029/2021GL095813
- Radiative effects of precipitation on the global energy budget and Arctic amplification T. Michibata 10.1038/s41612-024-00684-4
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
The amount of solar energy absorbed by Earth is believed to strongly depend on clouds. Here, we investigate this relationship using satellite data and 32 climate models, showing that this relationship holds everywhere except over polar seas, where an increased reflection by clouds corresponds to an increase in absorbed solar radiation at the surface. This interplay between clouds and sea ice reduces by half the increase of net radiation at the surface that follows the sea ice retreat.
The amount of solar energy absorbed by Earth is believed to strongly depend on clouds. Here, we...