Print Email Facebook Twitter Eddy-Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone Title Eddy-Induced Dispersion of Sea Ice Floes at the Marginal Ice Zone Author Gupta, M. (TU Delft Physical and Space Geodesy; California Institute of Technology) Gürcan, Emma (California Institute of Technology) Thompson, Andrew F. (California Institute of Technology) Date 2024 Abstract Ocean heat exchanges at the marginal ice zone (MIZ) play an important role in melting sea ice. Mixed-layer eddies transport heat and ice floes across the MIZ, facilitating the pack's access to warm waters. This study explores these frontal dynamics using disk-shaped floes coupled to an upper-ocean model simulating the sea ice edge. Numerical experiments reveal that small floes respond more strongly to fine-scale ocean currents, which favors higher dispersion rates and weakens sea ice drag onto the underlying ocean. Floes with radii smaller than resolved turbulent filaments (∼2–4 km) result in a wider and more energetic MIZ, by a factor of 70% each, compared to larger floes. We hypothesize that this floe size dependency may affect sea ice break-up by controlling oceanic energy propagation into the MIZ and modulate the sea ice pack's melt rate by regulating lateral heat transport toward the sea ice cover. Subject eddiesheat transportoceanographypolar climatesea icesubmesoscale To reference this document use: http://resolver.tudelft.nl/uuid:95ef7374-1908-4ebd-81fe-c042d7f3b2d3 DOI https://doi.org/10.1029/2023GL105656 ISSN 0094-8276 Source Geophysical Research Letters, 51 (2) Part of collection Institutional Repository Document type journal article Rights © 2024 M. Gupta, Emma Gürcan, Andrew F. Thompson Files PDF Geophysical_Research_Lett ... e_Zone.pdf 1.19 MB Close viewer /islandora/object/uuid:95ef7374-1908-4ebd-81fe-c042d7f3b2d3/datastream/OBJ/view