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Ocean Surface Current Detection by Synthetic Aperture Radar

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Part of the book series: Marine Science ((MR,volume 13))

Abstract

Synthetic aperture radar Doppler histories have been used to obtain estimates of ocean surface currents. For currents in excess of 1 meter/second, airborne radar measurements agree with surface observations to within 25 percent. Satellite measurements, however, yield current speeds far in excess of surface estimates. The technique developed to obtain the Doppler information is described, and possible sources of error are discussed.

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References

  • Raney, R.K. and Shuchman, R.A., 1978, “SAR Mechanism for Imaging Waves,” Proc. of Fifth Canadian Symiposium on Remote Sensing, Victoria, B.C.

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© 1981 Plenum Press, New York

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Gonzalez, F.I., Rufenach, C.L., Shuchman, R.A. (1981). Ocean Surface Current Detection by Synthetic Aperture Radar. In: Gower, J.F.R. (eds) Oceanography from Space. Marine Science, vol 13. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-3315-9_59

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  • DOI: https://doi.org/10.1007/978-1-4613-3315-9_59

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4613-3317-3

  • Online ISBN: 978-1-4613-3315-9

  • eBook Packages: Springer Book Archive

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