Articles | Volume 19, issue 4
https://doi.org/10.5194/os-19-1225-2023
https://doi.org/10.5194/os-19-1225-2023
Research article
 | 
16 Aug 2023
Research article |  | 16 Aug 2023

The Iceland–Faroe warm-water flow towards the Arctic estimated from satellite altimetry and in situ observations

Bogi Hansen, Karin M. H. Larsen, Hjálmar Hátún, Steffen M. Olsen, Andrea M. U. Gierisch, Svein Østerhus, and Sólveig R. Ólafsdóttir

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Latest update: 17 Nov 2024
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Short summary
Based on in situ observations combined with sea level anomaly (SLA) data from satellite altimetry, volume as well as heat (relative to 0 °C) transport of the Iceland–Faroe warm-water inflow towards the Arctic (IF inflow) increased from 1993 to 2021. The reprocessed SLA data released in December 2021 represent observed variations accurately. The IF inflow crosses the Iceland–Faroe Ridge in two branches, with retroflection in between. The associated coupling to overflow reduces predictability.