Obukhov Length Estimation From Spaceborne Radars

Journal Article (2023)
Author(s)

Owen O’Driscoll (Technopôle Brest-Iroise)

Alexis Mouche (Technopôle Brest-Iroise)

Bertrand Chapron (Technopôle Brest-Iroise)

Marcel Kleinherenbrink (TU Delft - Mathematical Geodesy and Positioning)

Francisco Dekker (TU Delft - Mathematical Geodesy and Positioning)

Research Group
Mathematical Geodesy and Positioning
Copyright
© 2023 Owen O’Driscoll, Alexis Mouche, Bertrand Chapron, M. Kleinherenbrink, F.J. Lopez Dekker
DOI related publication
https://doi.org/10.1029/2023GL104228
More Info
expand_more
Publication Year
2023
Language
English
Copyright
© 2023 Owen O’Driscoll, Alexis Mouche, Bertrand Chapron, M. Kleinherenbrink, F.J. Lopez Dekker
Research Group
Mathematical Geodesy and Positioning
Issue number
15
Volume number
50
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

Two air-sea interaction quantification methods are employed on synthetic aperture radar (SAR) scenes containing atmospheric-turbulence signatures. Quantification performance is assessed on Obukhov length L, an atmospheric surface-layer stability metric. The first method correlates spectral energy at specific turbulence-spectrum wavelengths directly to L. Improved results are obtained from the second method, which relies on a machine-learning algorithm trained on a wider array of SAR-derived parameters. When applied on scenes containing convective signatures, the second method is able to predict approximately 80% of observed variance with respect to validation. Estimated wind speed provides the bulk of predictive power while parameters related to the kilometer-scale distribution of spectral energy contribute to a significant reduction in prediction errors, enabling the methodology to be applied on a scene-by-scene basis. Differences between these physically based estimates and parameterized numerical models may guide the latter's improvement.