Sea-Ice Melt Driven by Ice-Ocean Stresses on the Mesoscale

Mukund Gupta, John Marshall, Hajoon Song, Jean Michel Campin, Gianluca Meneghello

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1 Citation (Scopus)

Abstract

The seasonal ice zone around both the Arctic and the Antarctic coasts is typically characterized by warm and salty waters underlying a cold and fresh layer that insulates sea-ice floating at the surface from vertical heat fluxes. Here, we explore how a mesoscale eddy field rubbing against ice at the surface can, through Ekman-induced vertical motion, bring warm waters up to the surface and partially melt the ice. We dub this the “Eddy-Ice-Pumping” (EIP) mechanism. When sea-ice is relatively motionless, underlying mesoscale eddies experience a surface drag that generates Ekman upwelling in anticyclones and downwelling in cyclones. An eddy composite analysis of a Southern Ocean eddying channel model, capturing the interaction of the mesoscale with sea-ice, shows that within the compact ice zone, the mixed layer depth (MLD) is shallow in anticyclones (∼20 m) due to sea-ice melt and deep in cyclones (∼50–200m) due to brine rejection. “EIP” warms the core of anticyclones without significantly affecting the temperature of cyclones, producing a net upward vertical heat flux that reduces the mean sea-ice thickness by 10% and shoals the MLD by 60% over the course of winter and spring. In the following months, the sea-ice thickness recovers with an overshoot, due to strong negative feedbacks associated with atmospheric cooling and salt stratification. Consequently, the effect of “EIP” does not accumulate over the years, but modulates the seasonal cycle of ice within the compact ice zone.

Original languageEnglish
Article numbere2020JC016404
JournalJournal of Geophysical Research: Oceans
Volume125
Issue number11
DOIs
Publication statusPublished - 2020 Nov

Bibliographical note

Funding Information:
Mukund Gupta and John Marshall acknowledge support from the NSF Antarctic Program, Hajoon Song acknowledges the support of the National Research Foundation of Korea (NRF) grant funded by the Korean government (MSIT; NRF‐2019R1C1C1003663) and the Yonsei University Research Fund of 2020‐22‐0114, Jean‐Michel Campin acknowledges support from the MIT‐GISS collaborative agreement, and Gianluca Meneghello acknowledges support from the NSF program on Arctic Research (1603557). We are grateful for the insightful reviews provided by Georgy Manucharyan and Chris Horvat that helped improved the manuscript.

Publisher Copyright:
© 2020. American Geophysical Union. All Rights Reserved.

All Science Journal Classification (ASJC) codes

  • Geochemistry and Petrology
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Oceanography

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