Articles | Volume 19, issue 3
https://doi.org/10.5194/os-19-887-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-19-887-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
22 Jun 2023
Research article |
| 22 Jun 2023
| 22 Jun 2023
Improving the thermocline calculation over the global ocean
Emmanuel Romero
Departamento de Oceanología, Instituto Politécnico Nacional–Centro Interdisciplinario de Ciencias Marinas (IPN–CICIMAR), Av. IPN s/n, La Paz, B.C.S., 23096, Mexico
Leonardo Tenorio-Fernandez
CORRESPONDING AUTHOR
Departamento de Oceanología, Instituto Politécnico Nacional–Centro Interdisciplinario de Ciencias Marinas (IPN–CICIMAR), Av. IPN s/n, La Paz, B.C.S., 23096, Mexico
CONAHCyT, Consejo Nacional de Humanidades Ciencia y Tecnología, Av. Insurgentes Sur 1582, Col. Crédito Constructor, Alcaldía Benito Juárez, C.P. 03940, Mexico City, Mexico
Esther Portela
School of Environmental Sciences, University of East Anglia, Norwich, UK
Univ. Brest, Laboratoire d'Océanographie Physique et Spatiale, CNRS, IRD, Ifremer, Plouzané, France
Institute for Marine and Antarctic Studies, University of Tasmania, Hobart 7001, Australia
Jorge Montes-Aréchiga
Departamento de Física, Universidad de Guadalajara, Gral. Marcelino García Barragán 1421, Olímpica, 44430 Guadalajara, Jal, Mexico
Laura Sánchez-Velasco
Departamento de Oceanología, Instituto Politécnico Nacional–Centro Interdisciplinario de Ciencias Marinas (IPN–CICIMAR), Av. IPN s/n, La Paz, B.C.S., 23096, Mexico
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Short summary
In this study, we present a methodology to locate the minimum and maximum depths of the strongest thermocline, its thickness, and its strength by adjusting the sigmoid function to the temperature profiles in the global ocean. The results of the methodology are compared with the results of other methods found in the literature, and an assessment of the ocean regions where the adjustment is valid is provided. The method proposed here has shown to be robust and easy to apply.
In this study, we present a methodology to locate the minimum and maximum depths of the...
