Preprints
https://doi.org/10.5194/egusphere-2026-6294
https://doi.org/10.5194/egusphere-2026-6294
22 Oct 2026
 | 22 Oct 2026
Status: this preprint is open for discussion and under review for Ocean Science (OS).

Argo Trajectories Reveal Changing Core-Peripheral Partitioning of Gulf Stream Transport

Tianle Luo, Yi Cai, Songtao Ai, Fangjie Liu, and Michal Pętlicki

Abstract. Long-term Gulf Stream transport estimates diverge, partly because existing observing systems sample different locations and cross-stream extents. Most studies assess transport at fixed sections, leaving changes in the core and surrounding flow unresolved. Here, we develop a Core-Peripheral Transport Decomposition Method using Argo float trajectories from 2003 to 2024. We identify the mean core band from velocity gradients and quantify core-band and peripheral transport from annual mean time series. Core-band transport shows no significant trend, while peripheral transport declines at −4.99 Sv yr-1 before 2017 and recovers at +20.01 Sv yr-1 afterward. The core fraction of the fixed-latitude total rises from approximately 33 % to more than 100 % in 2015 and 2019, before decreasing to 26 % at the end of the record. Validation against shipboard ADCP observations yields significant interannual correlation (R = 0.667). These results reveal changing cross-stream transport partitioning and provide an observational basis for interpreting divergent Gulf Stream transport estimates across observing systems.

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Tianle Luo, Yi Cai, Songtao Ai, Fangjie Liu, and Michal Pętlicki

Status: open (until 17 Dec 2026)

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Tianle Luo, Yi Cai, Songtao Ai, Fangjie Liu, and Michal Pętlicki
Tianle Luo, Yi Cai, Songtao Ai, Fangjie Liu, and Michal Pętlicki
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Short summary
The Gulf Stream carries warm water northward and affects climate. Scientists disagree about whether it is weakening. Using Argo floats from 2003 to 2024, we separated the fast core from the slower surrounding water across the current's width. The core remained stable, while the surrounding water weakened before 2017 and recovered afterward, changing the core's share of transport. This shows the current is not changing uniformly, explaining why studies report different trends.
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