Articles | Volume 19, issue 5
https://doi.org/10.5194/os-19-1453-2023
https://doi.org/10.5194/os-19-1453-2023
Technical note
 | 
18 Oct 2023
Technical note |  | 18 Oct 2023

Technical note: Determining Arctic Ocean halocline and cold halostad depths based on vertical stability

Enrico P. Metzner and Marc Salzmann

Data sets

Woods Hole Oceanographic Institution Ice-Tethered Profiler Program (2016), Ice-Tethered Profiler observations: Vertical profiles of temperature, salinity, oxygen, and ocean velocity from an Ice-Tethered Profiler buoy system J. M. Toole, R. Krishfield, J. K. O'Brien, A. E. Houk, and S. T. Cole https://doi.org/10.7289/v5mw2f7x

A comprehensive, quality-controlled and up-to-date data set of temperature and salinity data for the Arctic Mediterranean Sea (Version 1.0) A. Behrendt, H. Sumata, B. Rabe, and U. Schauer https://doi.org/10.1594/PANGAEA.872931

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Short summary
The Arctic Ocean cold halocline separates the cold surface mixed layer from the underlying warm Atlantic Water, and thus provides a precondition for sea ice formation. Here, we introduce a new method for detecting the halocline base and compare it to two existing methods. We show that the largest differences between the methods are found in the regions that are most prone to a halocline retreat in a warming climate, and we discuss the advantages and disadvantages of the three methods.