Articles | Volume 13, issue 4
Development and technical paper
22 Apr 2020
Development and technical paper |  | 22 Apr 2020

Tracking water masses using passive-tracer transport in NEMO v3.4 with NEMOTAM: application to North Atlantic Deep Water and North Atlantic Subtropical Mode Water

Dafydd Stephenson, Simon A. Müller, and Florian Sévellec


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Dafydd Stephenson on behalf of the Authors (12 Feb 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 Feb 2020) by Qiang Wang
RR by Anonymous Referee #2 (29 Feb 2020)
ED: Publish as is (02 Mar 2020) by Qiang Wang
Short summary
Different water types are created at the sea surface with a signature based on the local conditions of the atmosphere. They then take these conditions with them into the deeper ocean, and so their journey is an important climate process to understand. In this study, we modify and repurpose a specialised model which simulates the ocean forward and backward in time to determine where new ocean water goes, where at the surface existing water comes from, and how old it is, by tracking it as a dye.