Supplementary material to "How polar-to-midlatitude atmospheric teleconnections depend on regional sea ice fraction and global warming level"
CESM2 NH Barents-Kara Okhotsk Labrador Greenland Chukchi-Bering Antarctic NH 1.00 0.75 0.30 0.18 0.58 0.37 0.06 Barents-Kara 0.75 1.00 0.06 -0.11 0.32 -0.04 0.01 Okhotsk 0.30 0.06 1.00 -0.06 -0.09 -0.07 0.04 Labrador 0.18 -0.11 -0.06 1.00 0.20 -0.04 0.06 Greenland 0.58 0.32 -0.09 0.20 1.00
Authors
- B. H. Samset (ORCID: https://orcid.org/0000-0001-8013-1833)
- Marianne T. Lund (ORCID: https://orcid.org/0000-0001-9911-4160)
- Carley Iles (ORCID: https://orcid.org/0000-0003-3504-2107)
Publication Details
- Published
- 2025-08-29
- DOI
- https://doi.org/10.5194/egusphere-2025-4115-supplement
- Primary Topic
- Arctic and Antarctic ice dynamics
- Type
- article
- Field-Weighted Citation Impact
- 0.00