4.7 Article

Total Surface Current Vector and Shear From a Sequence of Satellite Images: Effect of Waves in Opposite Directions

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
Volume 126, Issue 7, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021JC017342

Keywords

surface current; remote sensing; vertical shear; Sentinel-2

Categories

Funding

  1. CNES, SKIM preparation program
  2. ANR [ANR-17-EURE-0015, ANR-14-CE01-0012]
  3. European Space Agency, through the IASCO contract [4000129945/19/NL/FF/gp]
  4. European Space Agency, through the SARONG contract [4000117644/16/NL/FF/gp]
  5. Ministry of Science and Education of the Russian Federation [0555-2021-0004]
  6. Russian Science Foundation [21-47-00038]
  7. Russian Science Foundation [21-47-00038] Funding Source: Russian Science Foundation

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The study proposes a method based on Sentinel-2 data and numerical simulation to estimate near-surface shear in the ocean. The research shows that paying special attention to opposing waves and using least squares fit can better estimate current velocity. Furthermore, increasing time lags, resolution, and exposure time of acquisition can improve the retrieval of TSCV and shear.
The total surface current velocity (TSCV)-the horizontal vector quantity that advects seawater-is an essential climate variable, with few observations available today. The TSCV can be derived from the phase speed of surface gravity waves, and the estimates of the phase speeds of different wavelengths could give a measure of the vertical shear. Here, we combine 10-m resolution Level-1C of the Sentinel-2 Multispectral Instrument, acquired with time lags up to 1 s, and numerical simulation of these images. Retrieving the near-surface shear requires a specific attention to waves in opposing directions when estimating a single-phase speed from the phase difference in an image pair. Opposing waves lead to errors in phase speeds that are most frequent for shorter wavelengths. We propose an alternative method using a least squares fit of the current speed and amplitudes of waves in opposing directions to the observed complex amplitudes of a sequence of three images. When applied to Sentinel-2, this method generally provides more noisy estimate of the current. A byproduct of this analysis is the opposition spectrum which is a key quantity in the sources of microseisms and microbaroms. For future possible sensors, the retrieval of TSCV and shear can benefit from increased time lags, resolution, and exposure time of acquisition. These findings should allow new investigations of near-surface ocean processes including regions of freshwater influence or internal waves, using existing satellite missions such as Sentinel-2, and provide a basis for the design of future optical instruments.

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