Entrainment Rates and Eddy Exchange Coefficients From Reanalysis Sea Surface Salinity Data

Abstract Simple analytic models developed in this study are applied to long‐term averages of reanalysis surface salinity data to quantify two fundamental properties of ocean currents. The first model is based on the new Freshening Length schema and its application to the Irminger Current yields a ra...

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Bibliographic Details
Published in:Journal of Advances in Modeling Earth Systems
Main Authors: Nathan Paldor, Ofer Shamir, Itamar Yacoby
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2023
Subjects:
Knudsen relation
Irminger Current
Adriatic sea
eddy transport
Physical geography
GB3-5030
Oceanography
GC1-1581
Greenland
Knudsen
Online Access:https://doi.org/10.1029/2022MS003512
https://doaj.org/article/94a84f0bee7c445ba34f8f6cc48c659a
Description
Summary:Abstract Simple analytic models developed in this study are applied to long‐term averages of reanalysis surface salinity data to quantify two fundamental properties of ocean currents. The first model is based on the new Freshening Length schema and its application to the Irminger Current yields a ratio of about 5 between the turbulent entrainment rates of surrounding fresher surface waters west and east of Greenland. The second model is based on the steady solution of the advection‐diffusion equation subject to suitable boundary conditions. The application of this model to the spreading of fresh, snow‐melt, water from the delta of the Po river in the northwest Adriatic Sea into the rest of the Sea yields a ratio of 8 × 104 m between the eddy exchange coefficient and the speed of advection in the Sea.

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