An analytical model of iceberg drift
Till J.W. Wagner, Rebecca W. Dell, and Ian Eisenman

TL;DR
This paper presents an analytical model of iceberg drift that captures key physical processes, deriving a formula for iceberg movement and explaining the empirical drift rule, with applications to Arctic and Antarctic icebergs.
Contribution
An idealized analytical model of iceberg drift is developed, providing physical insights and a formula for iceberg trajectories based on wind and ocean currents.
Findings
Icebergs drift at about 2% of wind speed relative to ocean current in strong wind conditions.
In weak winds or with large icebergs, drift aligns with ocean surface currents.
Wind strength determines whether icebergs move with wind or ocean currents.
Abstract
Iceberg drift and decay and the associated freshwater release are increasingly seen as important processes in Earth's climate system, yet a detailed understanding of their dynamics has remained elusive. Here, an idealized model of iceberg drift is presented. The model is designed to include the most salient physical processes that determine iceberg motion while remaining sufficiently simple to facilitate physical insight into iceberg drift dynamics. We derive an analytical solution of the model, which helps build understanding and also enables the rapid computation of large numbers of iceberg trajectories. The long-standing empirical rule of thumb that icebergs drift at 2% of the wind velocity, relative to the ocean current, is derived here from physical first principles, and it is shown that this relation only holds in the limit of strong winds or small icebergs, which approximately…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
