Dual-tracer constraints on the inverse Gaussian transit time distribution improve the estimation of water mass ages and their temporal trends in the tropical thermocline

<p>Quantifying the mean state and temporal change of seawater age is crucial for understanding the role of ocean circulation and its change in the climate system. One commonly used technique to estimate the water age is the inverse Gaussian transit time distribution method (IG-TTD), which appl...

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Bibliographic Details
Main Authors: H. Guo, W. Koeve, A. Oschlies, Y.-C. He, T. P. Kemena, L. Gerke, I. Kriest
Format: Article
Language:English
Published: Copernicus Publications 2025-07-01
Series:Ocean Science
Online Access:https://os.copernicus.org/articles/21/1167/2025/os-21-1167-2025.pdf
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