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Therefore, sea-ice floe size distribution (FSD), a key measurement of SIFs, actively influences sea-ice thermodynamics and dynamics (Alberello et al., 2019, Dumas-Lefebvre and Dumont, 2023). The decreasing thickness of sea ice has further underscored the crucial role of SIFs in the evolution of sea ice ( Horvat, 2022 , Sumata et al., 2023 ). More @Wikipedia
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- Integrating a data-driven classifier and shape ... - ScienceDirectTherefore, sea-ice floe size distribution (FSD), a key measurement of SIFs, actively influences sea-ice thermodynamics and dynamics (Alberello et al., 2019, Dumas-Lefebvre and Dumont, 2023). The decreasing thickness of sea ice has further underscored the crucial role of SIFs in the evolution of sea ice ( Horvat, 2022 , Sumata et al., 2023 ).
- Ship resistance when operating in floating ice floes: A combined CFD ...The movement of an ice floe can be considered as the combination of translation and rotation, which was solved with the rigid-body motion equations in the body-fixed system based on the mass centre of the floe G−x'y’z’: (7) F = m d V G → d t (8) T = [J] · d ω G → d t + ω G → × ([J] · ω G →) where F and T are the total force ...
- Ship resistance when operating in floating ice floes: Derivation ...Ice-floe resistance for varying ice thickness, obtained when Fr = 0.15; results of 1:52.667 KCS hull model. Download: Download high-res image (229KB) Download: Download full-size image; Fig. 12. Ice-floe resistance as a function of floe size, obtained when Fr = 0.15 and h = 0.02 m; results of 1:52.667
- Ice Floe - an overview | ScienceDirect Topics3D processes like floe rafting and overturning, however, will affect the out-of-plane thickening, which is the critical factor for deciding the horizontal strength of ice jam and ice floe field (Hopkins and Tuhkuri, 1999; McKenna et al., 1997). 3D DEM was also adopted in simulations of ship interacting with ice floes (Lau et al., 2011; Vroegrijk, 2012; Ji et al., 2013).
- Ice Floe Tracker: An algorithm to automatically retrieve Lagrangian ...The circled ice floe is identified continuously for nine days. The position of the ice floe is presented both (a) at the beginning (30.04.2017) and (b) at the end (08.05.2017) of the automatically retrieved trajectory. The contour of the ice floe is delineated with light-blue, and its area is filled in with gray.
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