1. Sea Ice‐Driven Iceberg Drift in Baffin Bay.
- Author
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Marson, J. M., Myers, P. G., Garbo, A., Copland, L., and Mueller, D.
- Subjects
SEA ice ,ICEBERGS ,MARITIME shipping ,DRAG force ,ICE calving ,OCEAN currents - Abstract
Baffin Bay is the travel destination of most icebergs calving from west Greenland. They commonly follow the bay's cyclonic circulation and might end up far south along the coast of Newfoundland and Labrador, where many shipping routes converge. Given the hazard that icebergs pose to marine transportation, understanding their distribution is fundamental. One of the forces driving iceberg drift arises from the presence of sea ice. Observations in the Southern Ocean indicate that icebergs get locked in thick and concentrated sea ice. We present observations that support the occurrence of this sea ice locking mechanism (SIL) in Baffin Bay as well. Most iceberg models, however, represent the sea ice force over an iceberg as a simple drag force. Here, we implement a new parameterization in the iceberg module of the Nucleus for European Modeling of the Ocean (NEMO‐ICB) to represent SIL. We show that, by using this new parameterization, icebergs are more likely to travel outside of the Baffin Island Current during winter, which is supported by satellite observations. There is a slight improvement in the representation of iceberg severity along the coast of Newfoundland and Labrador and a slight shift of iceberg melt toward this region and Lancaster Sound/Hudson Strait. Although the impacts of icebergs on sea ice are still not represented, and targeted observations are needed for model calibration regarding sea ice concentration thresholds from which icebergs get locked, we are confident that this model improvement takes iceberg modeling one step forward toward reality. Plain Language Summary: After they break off Greenland's glaciers, icebergs drift in the ocean in somewhat predictable patterns across Baffin Bay. What makes them predictable is that we know the main natural forces that cause icebergs to move: the winds, the ocean currents, and the sea ice cover. Because it is impossible to monitor all the icebergs coming from Greenland, we use computer models to understand their typical trajectories. In these models, each one of the forces responsible for iceberg drift can be represented mathematically, usually in a very simplistic way. The sea ice force, for example, is proportional to how much friction there is between the iceberg and sea ice. However, observations in nature show that the iceberg‐sea ice interaction is more complicated than that: if the sea ice cover is thick and compact, it is able to trap icebergs, and both will move as one solid block. In this study, we improve a model's representation of the sea ice force by including this trapping mechanism. Results show that iceberg trajectory can be slightly different during winter due to sea ice trapping and that this mechanism potentially improves our ability to predict when icebergs reach the transatlantic shipping routes east of Canada. Key Points: A new sea ice‐iceberg locking parameterization was implemented in Nucleus for European Modeling of the Ocean and tested in a 1/4° resolution regional configurationIcebergs locked in sea ice in Baffin Bay are more likely to travel outside of the Baffin Island Current than "unlocked" onesThe existence of a sea ice locking mechanism in Baffin Bay is supported by observations of co‐varying iceberg and sea ice speeds [ABSTRACT FROM AUTHOR]
- Published
- 2024
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