Monitoring intense oceanic fronts using sea surface roughness: Satellite, airplane and in‐situ comparison

Type Article
Date 2020-08
Language English
Author(s) Rascle NicolasORCID1, 6, Chapron BertrandORCID2, Molemaker Jeroen2, 3, Nouguier FredericORCID2, Ocampo‐torres Francisco J.1, Osuna Cañedo J. Pedro1, Marié Louis2, Lund Björn4, Horstmann Jochen5
Affiliation(s) 1 : Departamento de Oceanografía Física Centro de Investigación Científica y de Educación Superior de Ensenada Baja California ,México
2 : Univ. Brest, CNRS, IRD, Ifremer, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM Brest ,France
3 : University of California Los Angeles Los Angeles California ,USA
4 : Department of Ocean Sciences Rosenstiel School of Marine and Atmospheric Science, University of Miami Miami Florida,USA
5 : Department of Radar Hydrography Helmholtz‐Zentrum Geesthacht Geesthacht,Germany
6 : Univ. Brest, CNRS, IRD, Ifremer, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM Brest ,France
Source Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2020-08 , Vol. 125 , N. 8 , P. e2019JC015704 (22p.)
DOI 10.1029/2019JC015704
WOS© Times Cited 12
Keyword(s) sea surface roughness, submesoscale current, fine-scale current, synthetic aperture radar (SAR), sunglint Sun glitter, ocean front

Sea surface roughness is affected by surface current gradients, which provides a means of monitoring from satellite sharp oceanic fronts. This paper is the second report of an experiment designed to compare observations of sea surface roughness and surface currents at an unprecedented accuracy, owing to the conjunction of numerous deployed drifters and roughness instruments. About 200 drifters sampled a thin 10~km elongated submesoscale front, also monitored by a high density of roughness instruments: satellite Synthetic Aperture Radar, satellite and airborne multi‐angle sunglint radiometers. The first paper focused on the retrieval of the current gradient direction (convergence and cyclonic vorticity) at the front, using roughness observations at multiple angle from airplane. This second paper focuses on the retrieval of the current gradient magnitude and scale, using roughness observations at different scales, from airplane and from satellite. Two main results are obtained: (i) Trajectories of selected drifters show that the front is only 50~m wide and unambiguously exhibits convergence and cyclonic vorticity up to 100~f (with f the Coriolis frequency). This far exceeds previously documented values for submesoscale deep ocean fronts. (ii) Correct estimation of such extreme current gradients using surface roughness hinges on instruments with sufficiently high spatial resolution. Lower resolution roughness sensors can still detect the front, as demonstrated from observations and a simplified model, but cannot properly estimate the current gradient magnitude and the frontal width. Those results provide guidelines for monitoring intense current gradients from space using sea surface roughness.


Ocean surface currents are not uniform horizontally, but involve structures of many different sizes. After focusing on large scale currents (about 1000~km) and eddies (about 100~km), attention is nowadays turning towards fine scale (about 1~km) fronts and filaments. Those fine structures are indeed particularly important for the exchanges between ocean surface and deeper ocean, for the accumulation of drifting pollution and for the concentration of biological production and marine predators. Fishermen well know that oceanic fronts can be revealed by visual inspection of the ocean surface roughness. Exploring this idea, this paper investigates how oceanic fronts can be monitored using images of sea surface roughness. Images from satellites and airplanes were taken during an experiment where hundreds of surface drifters were released and got caught within an intense front. Two new lessons are learned from those observations: (1) The front was only 50~m wide, which is much sharper than commonly assumed for fronts of this type. (2) The front is thus associated with extreme current shear, which can only be detected by roughness sensors with sufficiently high spatial resolution. Those are important findings to improve monitoring of intense oceanic fronts from satellite.

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Rascle Nicolas, Chapron Bertrand, Molemaker Jeroen, Nouguier Frederic, Ocampo‐torres Francisco J., Osuna Cañedo J. Pedro, Marié Louis, Lund Björn, Horstmann Jochen (2020). Monitoring intense oceanic fronts using sea surface roughness: Satellite, airplane and in‐situ comparison. Journal Of Geophysical Research-oceans, 125(8), e2019JC015704 (22p.). Publisher's official version : , Open Access version :