Preview

Fundamental and Applied Hydrophysics

Advanced search

Determination of the Sea Surface Current by a Doppler X-Band Radar

https://doi.org/10.7868/S2073667320030089

Abstract

The paper proposes a methodology for determining the speed and direction of the sea surface current from measurements of Doppler radar panoramas with an X-band Doppler radar. Numerical simulation of the Doppler velocity of the Bragg waves in the field of wind waves and currents were carried out. The range of distance was selected for measuring the velocity of the surface current at which the effect of shading of the sea surface sections by wave crests can be ignored. Long field experiments were conducted, during which the proposed method was tested. The velocity and direction of the surface current were calculated as the vectorial sum of the velocity of the water column and 3% of the wind speed, while at the same time Doppler radar panoramas of the sea surface were measured. It was shown that, for upwind/upwave radar sensing, the average Doppler velocity of the scattering microwave waves of sea surface elements are significantly higher than the predictions of the two-scale scattering model. To restore the velocity of the surface current the registration was carried out empirically. For downwind/downwaves radar sensing, good agreement with the simulation results was observed. A correlation analysis of the surface current, calculated through hydro meteorological parameters and Doppler radar panoramas, showed a maximum correlation coefficient for a velocity value is about 0.88 with a root mean square error of 8 cm/s, and for a direction is about 0.98 with a root mean square error of 14 degrees. It is noted that film slicks on the sea surface lead to a significant decrease in the average Doppler velocity, which may serve as an additional criterion for the remote detection of oil spills.

About the Authors

A. V. Ermoshkin
Institute of Applied Physics RAS
Russian Federation

603950, Ulyanova Str., 46, Nizhny Novgorod



I. A. Kapustin
Institute of Applied Physics RAS
Russian Federation

603950, Ulyanova Str., 46, Nizhny Novgorod



A. A. Molkov
Institute of Applied Physics RAS
Russian Federation

603950, Ulyanova Str., 46, Nizhny Novgorod



N. A. Bogatov
Institute of Applied Physics RAS
Russian Federation

603950, Ulyanova Str., 46, Nizhny Novgorod



References

1. Stehnovskiy D.I., Zubkov A.E. Navigation and hydrometeorology. Moscow, Transport, 1977. 264 p. (in Russian).

2. Budyanskiy M.V. et al. Lagrange analysis of the Kuril vortices. Vestnik DVO RAN. 2017, 4, 81–88 (in Russian).

3. Zatsepin A.G. et al. Comparison of coastal currents measured by HF and X-band radars with ADCP and drifter data at the IO RAS hydrophysical test site in the Black Sea. Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa. 2017, 14, 7, 250–266 (in Russian).

4. Bulatov M.G. et al. Physical mechanisms for the formation of aerospace radar images of the ocean. UFN. 2003, 173 (1), 69–87 (in Russian).

5. Pereslegin S.V. et al. The forming of sea surface velocity images from stationary, airborne and spaceborne platforms. Fundamentalnaya i Prikladnaya Gidrofizika. 2019, 12, 1, 21–29 (in Russian).

6. Braun N., Ziemer F., Bezuglov A., Cysewski M., Schymura G. Sea-surface current features observed by Doppler Radar. IEEE Transactions on Geoscience and Remote Sensing. 2008, 46, 4, 1125–1133. doi: 10.1109/TGRS.2007.910221

7. Nyman L., Lund B., Romeiser R., Graber H., Horstmann J. A new approach to detect surface currents of complex flow using Doppler marine radar. IGARSS2018–2018 IEEE International Geoscience and Remote Sensing Symposium, Valencia, 2018, 1493–1496. doi: 10.1109/IGARSS.2018.8519168

8. Moiseev A. et al. Evaluation of radial ocean surface currents derived from Sentinel-1 IW Doppler shift using coastal radar and Lagrangian surface drifter observations. Journal of Geophysical Research: Oceans. 2020, 125, e2019JC015743. doi: https://doi.org/10.1029/2019JC015743

9. Mouche A.A. et al. On the use of Doppler shift for sea surface wind retrieval from SAR. IEEE Transactions on Geoscience and Remote Sensing. 2012, 50(7), 2901–2909. doi: https://doi.org/10.1109/TGRS.2011.2174998

10. Lund B. et al. Marine X-band radar currents and bathymetry: An argument for a wave number-dependent retrieval method. Journal of Geophysical Research: Oceans. 2020, 125, e2019JC015618. doi: https://doi.org/10.1029/2019JC015618

11. Ivonin D.V. et al. Monitoring system of surface currents on the base of low-cost X-band radar. First application on the Black Sea. Russian Journal of Earth Sciences. 2011, 13, ESES1001000.

12. Dankert H. Retrieval of surface-current fields and bathymetries using radar-image sequences. Proc. IGARSS. 2003. doi: 10.2205/2009ES000245

13. Ermoshkin A.V., Kapustin I.A. Estimation of the wind-driven wave spectrum using a high spatial resolution coherent radar. Russian Journal of Earth Sciences. 2019, 19, 3, ES1005 1–9.

14. Ermoshkin A.V. et al. On the features of Doppler velocities estimation with coherent radar of high spatial resolution. Proc. SPIE. 2019, 111501I.

15. Valenzuela G.R. Theories for the interaction of electromagnetic and oceanic waves — a review. Boundary-Layer Meteorology. 1978, 13, 61–85.

16. Johnson J.T., Chuang C.W. Quantitative Evaluation of Ocean Surface Spectral Model Influence on Sea Surface Backscattering. Technical Report 738927–1. Office of Naval Research. 2000. 47 p.

17. Salcedo-Sanz S. et al. Significant Wave Height Estimation using SVR Algorithms and Shadowing Information from Simulated and Real measured X-band radar images of the sea surface. Ocean Engineering. 2015, 101, 244–253. doi: https://doi.org/10.1016/j.oceaneng.2015.04.041

18. Hwang P.A., Sletten M.A., Toporkov J.V. Breaking wave contribution to low grazing angle radar backscatter from the ocean surface. Journal of Geophysical Research. 2008, 113, C09017.

19. Wu J. Sea-surface drift currents induced by wind and waves. Journal of Geophysical Research. 1983, 13(8), 1441–1451. doi:10.1029/2008JC004752

20. Kapustin I.A. et al. On the estimation of the contribution of near-surface wind to the kinematics of slicks on the sea surface under conditions of finite wave fetch. Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa. 2019, 16, 2, 163–172 (in Russian).

21. Ermoshkin A.V. et al. Statistical characteristics of Doppler velocity shift in artificial slick on sea surface. Proc. SPIE. 2019, 111501L.


Review

For citations:


Ermoshkin A.V., Kapustin I.A., Molkov A.A., Bogatov N.A. Determination of the Sea Surface Current by a Doppler X-Band Radar. Fundamental and Applied Hydrophysics. 2020;13(3):93-103. (In Russ.) https://doi.org/10.7868/S2073667320030089

Views: 128


Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.


ISSN 2073-6673 (Print)
ISSN 2782-5221 (Online)