The Iceland Faroe Slope Jet is a deep, dense-water current that flows south and east through the Faroe Bank Channel and feeds into the lower limb of the Atlantic meridional overturning circulation (AMOC).
Notes on verification
Confirmed by peer-reviewed Nature Communications study (Semper et al. 2020) that first identified the IFSJ, and independently reaffirmed by a 2026 JGR: Oceans paper describing the same current and its role in feeding the AMOC's lower limb. [tier=silver indep_score=1.0 clusters=2 claim_tier=notable]
Sources
- Solving this oceanic mystery could help predict our future on Earth (seed:science_and_space)
- https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585422/ (corroboration)
- https://pmc.ncbi.nlm.nih.gov/articles/PMC7585422/ (corroboration)
- https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2026JC024510 (corroboration)