Stepwise Subduction Observed at a Front in the Marginal Ice Zone in Fram Strait

At high latitudes, submesoscale dynamics act on scales of O $\mathcal{O}$(100 m–1 km) and are associated with the breakdown of geostrophic balance, vertical velocities, and energy cascading to small scales. Submesoscale features such as fronts, filaments, and eddies are ubiquitous in marginal ice zo...

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Veröffentlicht in:	Journal of geophysical research. Oceans 2024-05, Vol.129 (5), p.n/a
Hauptverfasser:	Hofmann, Zerlina, Appen, Wilken‐Jon, Kanzow, Torsten, Becker, Hauke, Hagemann, Jonas, Hufnagel, Lili, Iversen, Morten H.
Format:	Artikel
Sprache:	eng
Schlagworte:	Arctic Biological materials Carbon cycle Chlorophyll Chlorophylls Density gradients Eddies Filaments Fluorescence front Fronts high‐resolution Ice cover Ice edge Isopycnals marginal ice zones Meltwater ocean Oceans Polar waters Sea ice Sea surface Straits Subduction submesoscale Summer Vertical advection Vertical velocities Water depth
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