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Volume 14, issue 5 | Copyright

Special issue: Coastal marine infrastructure in support of monitoring, science,...

Ocean Sci., 14, 1265-1281, 2018
https://doi.org/10.5194/os-14-1265-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 16 Oct 2018

Research article | 16 Oct 2018

Joint analysis of coastal altimetry and high-frequency (HF) radar data: observability of seasonal and mesoscale ocean dynamics in the Bay of Biscay

Ivan Manso-Narvarte1, Ainhoa Caballero1, Anna Rubio1, Claire Dufau2, and Florence Birol3 Ivan Manso-Narvarte et al.
  • 1AZTI-Marine Research, Herrera Kaia, Portualdea z/g, 20110 Pasaia, Spain
  • 2CLS Space Oceanography Division, 8–10 Rue Hermès, 31526 Ramonville-St.-Agne, France
  • 3LEGOS, 14 Ave. E. Belin, 31400 Toulouse, France

Abstract. Land-based coastal high-frequency (HF) radar systems provide operational measurements of coastal surface currents (within 1–3m depth) with high spatial (300m–10km) and temporal ( ≤ 1h) sampling resolutions, while the near-continuous altimetry missions provide information, from 1993 until today, on geostrophic currents in the global ocean with typical along-track and temporal sampling resolutions of  > 7km and  > 9 days, respectively. During the last years, the altimetry community has made a step forward in improving these data in the coastal area, where the data present lower quality than in the open ocean. The combination of HF radar and altimetry measurements arises as a promising strategy to improve the continuous monitoring of the coastal area (e.g. by expanding the measurements made by HF radars to adjacent areas covered by the altimetry or by validating/confirming improvements brought by specific coastal algorithms or new altimeter missions). A first step towards this combination is the comparison of both data sets in overlapping areas.

In this study, a HF radar system and two Jason-2 satellite altimetry products with different processing are compared over the period from 1 January 2009 to 24 July 2015. The results provide an evaluation of the performance of different coastal altimetry data sets within the study area and a better understanding of the ocean variability contained in the HF radar and altimetry data sets. Both observing systems detect the main mesoscale processes within the study area (the Iberian Poleward Current and mesoscale eddies), and the highest correlations between radar and altimetry (up to 0.64) occur in the slope where the Iberian Poleward Current represents a significant part of the variability in the circulation. Besides, the use of an Ekman model, to add the wind-induced current component to the altimetry-derived geostrophic currents, increases the agreement between both data sets (increasing the correlation by around 10%).

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Our main aim is to compare two different measuring systems of the surface ocean currents: land-based, high-frequency radar and satellite altimetry. Results show that the surface currents detected by both systems agree up to a 70 %, mostly in areas of persistent currents. This work is a first step in the combination of both technologies for an improved monitoring of the coastal surface ocean dynamics.
Our main aim is to compare two different measuring systems of the surface ocean currents:...
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