Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2020, Vol. 17, No. 1, pp. 211-219
Distribution of variance of sea surface slopes by spatial wave range
1 Marine Hydrophysical Institute RAS, Sevastopol, Russia
Accepted: 24.12.2019
DOI: 10.21046/2070-7401-2020-17-1-211-219
The contribution to the variance of sea surface slopes created by waves of different lengths is analyzed. Remote sensing data (radar, radiometric and optical measurements), as well as in situ> measurements (measurements by laser slope meters, wave gauge sensors, special construction buoys) are used. The analysis took into account the following physical effects: the magnitude of the variance of the slopes, determined from remote sensing data, depends on the length of the probing radio wave; measured in situ> variance of slopes is determined by the design characteristics of the measuring equipment. For wind speeds above 7–8 m/s, the dependence of the change in the variance of slopes in the range from the length of the main energy-carrying waves to the specified length Λ0 is obtained. It is shown that the dependence of the variance of slopes on the length of the probing wave currently used in radiometric measurements significantly overestimates the variance values in the region where surface waves with a length Λ0 < 0,1 contribute to the mirror reflection of radio waves. It is also shown that the contribution to the variance of slopes, which is given by waves longer than 10 m, is less than 20 %.
Keywords: remote sensing, sea surface, slopes, long waves
Full textReferences:
- Bass F. G., Fuks I. M., Rasseyanie voln na statisticheski nerovnoi poverkhnosti (Wave scattering from statistically rough surface), Moscow: Nauka, 1972, 424 p.
- Danilychev M. V., Nikolaev A. N., Kutuza B. G., Application of the kirchhoff method for practical calculations in microwave radiometry of wavy sea surface, J. Communications Technology and Electronics, 2009, Vol. 54, No. 8, pp. 869–878.
- Zapevalov A. S., Statistical characteristics of the moduli of slopes of the sea surface, Physical Oceanography, 2002, Vol. 12, Issue 1, pp. 24–31.
- Zapevalov A. S., Bragg scattering of centimeter electromagnetic radiation from the sea surface: The effect of waves longer than Bragg components, Izvestiya — Atmospheric and Ocean Physics, 2009, Vol. 45, Issue 2, pp. 253–261.
- Zapevalov A. S., Bolshakov A. N., Smolov V. E., Studying the sea surface slopes using an array of wave gauge sensors, Oceanology, 2009, Vol. 49, No. 1, pp. 31–38.
- Kalinin S. A., Leikin I., Izmerenie uklonov vetrovykh voln v Kaspiiskom more (Measurement of the slopes of wind waves in the Caspian Sea), Izvestiya akademii nauk SSSR. Fizika atmosfery i okeana, 1988, Vol. 24, No. 11, pp. 1210–1217.
- Karaev V. Yu., Panfilova M. A., Balandina G. N., Chu X., Vosstanovlenie dispersii naklonov krupnomasshtabnykh voln po radiolokatsionnym izmereniyam v SVCh-diapazone (Retrieval of the slope variance by microwave measurements), Issledovanie Zemli iz kosmosa, 2012, No. 4, pp. 62–77.
- Khristoforov G. N., Zapevalov A. S., Babii M., Statisticheskie kharakteristiki uklonov morskoi poverkhnosti pri raznykh skorostyakh vetra (Statistics of sea-surface slope for different wind speeds), Okeanologiya, 1992, Vol. 32, No. 3, pp. 452–459.
- Apel J. R., An improved model of the ocean surface wave vector spectrum and its effects on radar backscatter, J. Geophysical Research, 1994, Vol. 99, No. C8, pp. 16269–16291.
- Chen P., Yin Q., Huang P., Effect of non-Gaussian properties of the sea surface on the low-incidence radar backscatter and its inversion in terms of wave spectra by an ocean wave, Chinese J. Oceanology and Limnology, 2015, Vol. 33, No. 5, pp. 1142–1156.
- Cheng Y., Liu Y., Xu Q., A new wind-wave spectrum model for deep water, Indian J. Marine Sciences, 2006, Vol. 35, No. 3, pp. 181–194.
- Cox C., Munk W., Measurements of the roughness of the sea surface from photographs of the sun glitter, J. Optical Society of America, 1954, Vol. 44, No. 11, pp. 838–850.
- Elfouhaily T., Chapron B., Katsaros K., Vandemark D., A unified directional spectrum for long and short wind-driven waves, J. Geophysical Research, 1997, Vol. 102, No. C7, pp. 15781–15796.
- Hollinger J. P., Passive microwave measurements of sea surface roughness, IEEE Trans. Geoscience Electronics, 1971, Vol. GE-9, No. 3, pp. 165–169.
- Hughes B. A., Grant H. L., Chappell R. W. A., A fast response surface-wave slope meter and measured wind-wave components, Deep-Sea Research, 1977, Vol. 24, No. 12, pp. 1211–1223.
- Kudryavtsev V. N., Markin V. K. Chapron B., Coupled sea surface-atmosphere model 2, spectrum of short wind waves, J. Geophysical Research, 1999, Vol. 104, pp. 7625–7639.
- Longuett-Higgins M. S., Cartwrighte D. E., Smith N. D., Observation of the directional spectrum of sea waves using the motions of the floating buoy, Proc. Conf. Ocean Wave Spectra, Englewood Cliffs, New Jersey: Prentice Hall, 1963, pp. 111–132.
- Plant W. J., A stochastic, multiscale model of microwave backscatter from the ocean, J. Geophysical Research, 2002, Vol. 107, No. C9, 3120, DOI: 10.1029/2001JC000909.
- Wilheit T. T., A model for the microwave emissivity of the ocean’s surface as a function of wind speed, IEEE Trans. Geoscience Electronics, 1979, Vol. GE-17, No. 4, pp. 244–249.