Comparison of Travel-time statistics of Backscattered Pulses from Gaussian and Non-Gaussian Rough Surfaces

Similar documents
Thermal Emission from a Layered Medium Bounded by a Slightly Rough Interface

Ambiguity of optical coherence tomography measurements due to rough surface scattering

Three-scale Radar Backscattering Model of the Ocean Surface Based on Second-order Scattering

A study of the slope probability density function of the ocean waves from radar observations

IMPACT OF RAIN, SWELL, AND SEA SURFACE CURRENTS ON THE ELECTROMAGNETIC BIAS IN GNSS-REFLECTOMETRY

A Statistical Kirchhoff Model for EM Scattering from Gaussian Rough Surface

Active microwave systems (2) Satellite Altimetry * the movie * applications

INVERSION ASSUMING WEAK SCATTERING

MICROWAVE DOPPLER SPECTRA OF SEA ECHOES AT HIGH INCIDENCE ANGLES: INFLUENCES OF LARGE- SCALE WAVES

7.2.1 Seismic waves. Waves in a mass- spring system

ASCAT B OCEAN CALIBRATION AND WIND PRODUCT RESULTS

BROADBAND MIMO SONAR SYSTEM: A THEORETICAL AND EXPERIMENTAL APPROACH

Frequency and Spatial Features of Waves Scattering on Fractals

EFFECTS OF ALONG-TRACK INTEGRATION ON DOPPLER VELOCITY BIAS WITH A SPACEBORNE CLOUD-PROFILING RADAR

Using the MBES for classification of riverbed sediments

Akira Ishimaru, Sermsak Jaruwatanadilok and Yasuo Kuga

Two-Dimensional simulation of thermal blooming effects in ring pattern laser beam propagating into absorbing CO2 gas

Mandatory Assignment 2013 INF-GEO4310

P14R.11 INFERENCE OF MEAN RAINDROP SHAPES FROM DUAL-POLARIZATION DOPPLER SPECTRA OBSERVATIONS

WAVE PROPAGATION AND SCATTERING IN RANDOM MEDIA

VARIABLE GAP UNDULATOR FOR KEV FREE ELECTRON LASER AT LINAC COHERENT LIGHT SOURCE

Multiple Scattering of Sound by Internal Waves and Acoustic Characterization of Internal Wave Fields in Deep and Shallow Water

Emergence of the Green s Functions from Noise and Passive Acoustic Remote Sensing of Ocean Dynamics

Contents of this Document [ntc5]

Remote Sensing ISSN

Signal Loss. A1 A L[Neper] = ln or L[dB] = 20log 1. Proportional loss of signal amplitude with increasing propagation distance: = α d

CRAMÉR-RAO BOUNDS FOR RADAR ALTIMETER WAVEFORMS. Corinne Mailhes (1), Jean-Yves Tourneret (1), Jérôme Severini (1), and Pierre Thibaut (2)

Using Remote-sensed Sea Ice Thickness, Extent and Speed Observations to Optimise a Sea Ice Model

ESTIMATING INDEPENDENT-SCATTERER DENSITY FROM ACTIVE SONAR REVERBERATION

Introduction to Acoustic Remote Sensing and Seafloor Mapping (AE4-E13) May 19, 2010

Mutah University, P.O. Box 7, Mutah, Al-Karak, 61710, Jordan 2 Department of Electrical Engineering,

Comparison of DPSK and MSK bit error rates for K and Rayleigh-lognormal fading distributions

Long- and short-term average intensity for multi-gaussian beam with a common axis in turbulence

THE SCATTERING FROM AN ELLIPTIC CYLINDER IRRADIATED BY AN ELECTROMAGNETIC WAVE WITH ARBITRARY DIRECTION AND POLARIZATION

In these notes on roughness, I ll be paraphrasing two major references, along with including some other material. The two references are:

EXTENDED UHF RADAR OBSERVATIONS OF RIVER FLOW VELOCITY AND COMPARISONS WITH IN-SITU MEASUREMENTS

Shipborne polarimetric weather radar: Impact of ship movement on polarimetric variables

Chapter 9. Reflection, Refraction and Polarization

7.4 GPS-Based Measurements of Ocean Surface Roughness. Stephen J. Katzberg NASA Langley Research Center Hampton, VA 23681

Simulations and Observations of GNSS Ocean Surface Reflections

Vector diffraction theory of refraction of light by a spherical surface

2.3. Large Scale Channel Modeling Shadowing

PEMC PARABOLOIDAL REFLECTOR IN CHIRAL MEDIUM SUPPORTING POSITIVE PHASE VELOC- ITY AND NEGATIVE PHASE VELOCITY SIMULTANE- OUSLY

An analytical model for the illuminance distribution of a power LED

Propagation of longitudinal waves in a random binary rod

APPLICATION OF THE MAGNETIC FIELD INTEGRAL EQUATION TO DIFFRACTION AND REFLECTION BY A CONDUCTING SHEET

GLAS Team Member Quarterly Report

A PRACTICAL METHODOLOGY FOR ESTIMATING WAVE SPECTRA FROM THE SIR-B

Progress In Electromagnetics Research M, Vol. 21, 33 45, 2011

Offset Spheroidal Mirrors for Gaussian Beam Optics in ZEMAX

Doppler echocardiography & Magnetic Resonance Imaging. Doppler echocardiography. History: - Langevin developed sonar.

A Discussion on the Applicable Condition of Rayleigh Scattering

SCATTERING ANALYSIS FOR SHIP KELVIN WAKES ON TWO-DIMENSIONAL LINEAR AND NONLINEAR SEA SURFACES

Radioholographic analysis of radio occultation data in multipath zones

OPTIMAL SENSOR-TARGET GEOMETRIES FOR DOPPLER-SHIFT TARGET LOCALIZATION. Ngoc Hung Nguyen and Kutluyıl Doğançay

Characteristics of the Mirror Image of Precipitation Observed by the TRMM Precipitation Radar

I. Rayleigh Scattering. EE Lecture 4. II. Dipole interpretation

Full Wave Analysis of RF Signal Attenuation in a Lossy Rough Surface Cave Using a High Order Time Domain Vector Finite Element Method

THE USE OF COMPARISON CALIBRATION OF REFLECTIVITY FROM THE TRMM PRECIPITATION RADAR AND GROUND-BASED OPERATIONAL RADARS

DETERMINATION OF MODEL VALID PREDICTION PERIOD USING THE BACKWARD FOKKER-PLANCK EQUATION

Electromagnetic Scattering from an Anisotropic Uniaxial-coated Conducting Sphere

Optical and radar observations of steep and breaking waves of decimeter range ( mesowaves ) on the sea surface: electrodynamical and hydrophysical

Today: 5 July 2008 ٢

Sensing. 14. Electromagnetic Wave Theory and Remote Electromagnetic Waves. Electromagnetic Wave Theory & Remote Sensing

China France. Oceanography S A T. The CFOSAT project. e l l i t e. C. Tison (1), D. Hauser (2), A. Mouche (3) CNES, France (2)

04. Random Variables: Concepts

Lecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar

Reverberation time, mean free path and sound absorption in concert halls

ERAD Drop size distribution retrieval from polarimetric radar measurements. Proceedings of ERAD (2002): c Copernicus GmbH 2002

Physics Letters A 374 (2010) Contents lists available at ScienceDirect. Physics Letters A.

P7.5 STUDIES OF SEA SURFACE NORMALIZED RADAR CROSS SECTIONS OBSERVED BY CLOUDSAT

1 The satellite altimeter measurement

Sensor and Simulation Notes. A Modified Description of Early Time High-altitude Electromagnetic Pulse Waveform (E1)

K distribution: an appropriate substitute for Rayleigh-lognormal. distribution in fading-shadowing wireless channels

A STATE-SPACE APPROACH FOR THE ANALYSIS OF WAVE AND DIFFUSION FIELDS

Seismic Noise Correlations. - RL Weaver, U Illinois, Physics

Assessment of Precipitation Characters between Ocean and Coast area during Winter Monsoon in Taiwan

Random deformation of Gaussian fields with an application to Lagrange models for asymmetric ocean waves

Lecture #12: Background

Visualization of polarization state and its application in Optics classroom teaching

IN SPITE of more than one half-century of theoretical developments

arxiv:physics/ v1 [physics.gen-ph] 2 Apr 2001

Physical Basics of Remote-Sensing with Satellites

Polarimetric Calibration of the Ingara Bistatic SAR

UNIVERSITY OF SOUTHAMPTON. Answer all questions in Section A and two and only two questions in. Section B.

Analyses of characteristics of spatial lightning electromagnetic field at different horizontal distances and observation point heights

Synthetic Aperture Radar Ship Detection Using Modified Gamma Fisher Metric

Oceanographic Aspect of Tropical Cyclone Wind and Wave Remote Sensing

Modeling microlenses by use of vectorial field rays and diffraction integrals

AN INTEGRAL EQUATION METHOD FOR DUAL-WAVELENGTH RADAR DATA USING A WEAK CONSTRAINT

Physics 403 Probability Distributions II: More Properties of PDFs and PMFs

COMPARISON OF THE INFLUENCES OF INITIAL ERRORS AND MODEL PARAMETER ERRORS ON PREDICTABILITY OF NUMERICAL FORECAST

FUNDAMENTALS OF OCEAN ACOUSTICS

Space Telescope Science Institute statistics mini-course. October Inference I: Estimation, Confidence Intervals, and Tests of Hypotheses

Propagation of Lorentz Gaussian Beams in Strongly Nonlocal Nonlinear Media

Learning Objectives for Stat 225

Annual Report. LaMer, Ehime University. Principle Investigator: Include the report on the result of the project/meeting in a separate sheet.

Physical substantiation of Huygens principle and the reciprocity theorem

Cramer-Rao Lower Bound Computation Via the Characteristic Function

Math 180A. Lecture 16 Friday May 7 th. Expectation. Recall the three main probability density functions so far (1) Uniform (2) Exponential.

Transcription:

Comparison of Travel-time statistics of Backscattered Pulses from Gaussian and Non-Gaussian Rough Surfaces GAO Wei, SHE Huqing Yichang Testing Technology Research Institute No. 55 Box, Yichang, Hubei Province 4433 People s Republic of China wellgao3@63.com Abstract: - Travel-time statistics of backscattered pulses from Gaussian and non-gaussian (Rayleigh and Exponential surfaces are studied and compared in this paper. It is found that in both cases (the Gaussian and non-gaussian surfaces, the probability distributions of the first and the second travel times are all only determined by a dimensionless parameter. Moreover, this study also found that the proportional relations between the dimensionless parameter and the median values of the first and the second travel times are remarkably different for Gaussian and non-gaussian cases. Then the statistical parameters of the rough surface can be estimated from travel-time statistics of backscattered pulses above if the probability distributions of the surface elevation and slope (PDSES are known in advance. However, PDSES are often unknown in most of practical applications, and little work has been applied to the problem of specifying the statistical characteristic of the rough surface in advance (Gaussian or non-gaussian. To solve this problem, on the basis of the relations between the median values of travel times and the altitude of source, a new theoretical method is proposed to judge the rough surfaces with Gaussian, Rayleigh and Exponential distributions. It is believed that the method proposed in this paper will be helpful to improve the estimate accuracy the parameters of a rough surface. Key-Words: probability distribution, travel time, backscatter, random surface. Introduction Travel times of backscattered waves from a random rough surface, especially the first arrivals of the backscattered signals play an important pole in a variety of applications to infer information about surface roughness and properties of the propagation medium []. For example, geophysical applications that employ the first arrivals include airborne laser altimetry [], seismic and ocean acoustic tomography [3], satellite radar altimetry [4], etc. In general, if a rough surface is random, travel time of a backscattered short pulse from the surface must be random too. Therefore, the statistics properties of travel-time have been the object of theoretical analyses by various authors. Frolov [5,6] studied the travel-time statistics of the signal backscattered from a rough surface in the limiting cases of large-scale roughness. Elfouhaily [7][8] solved the problem of the travel-time statistics in small-scale limit. Godin and Fuks [9] extended the results above to the three-dimensional problem. Recently on the basis of the mathematical theory of excursions of random functions[,], Fuks, Godin, et. al [-4] obtained the probability distributions of travel times and intensity of the first and second arrivals of a short pulse backscattered by a rough surface with a Gaussian statistics, within the geometrical optics approximation. GAO and WANG [5] then investigated the corresponding inverse problem for the Gaussian case. In the present paper, the problem of the first and the second travel times of a pulse backscattered by non-gaussian rough surfaces (Rayleigh and Exponential distribution is first studied and compared to the Gaussian case. The probability distributions, the median values of the travel times of the first and the second arrivals and the time delay between the first and the second arrivals are investigated theoretically and numerically. And the comparison of the results between Gaussian and non-gaussian cases and many new, different conclusions are also shown in this article. Furthermore, to improve the estimation accuracy of the parameters of a rough surface, a new theoretical method based on travel-time statistics of backscattered pulses is presented to judge the rough surfaces with Gaussian, Rayleigh and Exponential distributions. Arrangement of the paper is as follows. In section, we briefly recall some fundamental ingredients of the theory of Fuks and Godin [] on probability distribution functions of the first and the second ISSN: 9-777 59 Issue 3, Volume, March

Fig.. Problem geometry and notation. A point source located at (, H. ( x, t and ( x, t are the first and the second points of contact between the wave front Z( x, t and the rough surface ξ ( x, respectively. travel times of backscattered pulses from a rough surface. In section 3., these equations are applied to the case of rough surfaces with non-gaussian (Rayleigh and Exponential statistics. In section 3., the median values of travel times of the first and the second arrivals are discussed. In section 3.3, we investigate the probability distributions of time delay between the first and the second arrivals. Our summaries are presented in section 4. Fundamental equations Let us consider two-dimensional problem of a backscattered short pulse from a random rough surface, and do not concern the propagation effects of the medium between the source and the surface. The random surface is characterized by the equation z= ξ (x, (see Figure. A point source is located in the Cartesian coordinates (, H and emits a short pulse at the moment of time t=. The wave front makes the first contact with the surface at some point ( x, t. The first point of the contact must be a specularly reflecting point, namely the tangent plane to the surface at ( x, t is perpendicular to the ray connecting the source and the reflecting point. According to [], within the interval x ( L, L the probability of the absence of crossings between the random surface and the wave front satisfied the equation: Ρ{ t > t} = exp[ λ ( x, t dx] L ( where Zɺ ( x L λ ( x = dɺ ξ[ ɺ ξ Zɺ ( x] ω[ Z( x, ɺ ξ ] (a Z ( x λ( x = [ ( ] [ (, ] ( dɺ ξ ɺ ξ Zɺ x ω Z x ɺ ξ Z ( x ω ξ dξ ɺ (b where Z(x denoting the equation of the wave front, ω( ξ, ɺ ξ is the joint probability density function (PDF of the surface elevation ξ (x and slopes ɺ ξ ( x = dξ ( x / dx. Namely, Equation ( represents the probability of the event (there is not a specularly reflecting point at the interval x ( L, L. It is noted that Equation (a is the approximation given by Fuks and Godin [] and ISSN: 9-777 6 Issue 3, Volume, March

Equation (b is another different approximation result obtained by Smith [6]. For the reader s convenience, we introduce the H R dimensionless travel time difference =, σ (where R= ct, c is the signal propagation speed, σ is the root of mean square (rms of the elevation, H is the distance between the source and the mean surface and investigate the statistical properties of. It is obvious that the relation between H and H satisfies the following form: H = H+ ζ (3 where, ζ is the mean of the elevation ξ of the surface. Then the probability distribution functions F ( of the normalized time of the first arrival and F ( of the second arrival satisfy: F ( = Ρ{ < } =Ρ{ t > t} (4 ɺ ξ ɺ ξ exp( ω( ɺ ξ = γ γ, ɺ ξ >, ɺ ξ It is noted that the variances of the elevations and slopes are σ and γ, respectively. And the means of ξ and ɺ π ξ equal to σ π and γ. For simplifying analysis, we consider the surface elevation and slope are independent statistically at the same point as considered by Fuks and Godin []. Then the cumulative PDF of the surface elevation and slope can be written: ω( ξ, ɺ ξ = ω( ξ ω( ɺ ξ (8 (7 F ( = Ρ{ < } = Ρ{ t < t}. (5 3 Comparison between Gaussian and non-gaussian surfaces Refs.[] and [5] have studied the case of the backscattering surface with Gaussian distribution. In this section, we should apply the mathematical theory of excursions of random functions to investigate the problems of two specific random surfaces satisfied the non-gaussian distributions: Rayleigh or Exponential distribution, and give the comparison between Gaussian and non-gaussion cases in the following paper. 3. The first and second travel time Firstly, we study the case of Rayleigh surfaces. When the surface is a Rayleigh distribution (RD, the PDFs of surface elevation ξ and slope ξ ɺ can be written: ξ ξ exp( ω( ξ = σ σ, ξ >, ξ (6 When the inequality x L<< R(t holds, the wave front equation can be represented approximately in the following form: x Z( x, t = H R ( t x H R( t + R( t (9 Substituting (6-(9 into (, ( and (4, we obtain the probability function F ( : ( exp L F = π T ( dy L Φ (a L Φ( F ( = exp π T dy L ( + y exp[ ] (b where π = +, ISSN: 9-777 6 Issue 3, Volume, March

H R =, σ T = T, γ T = H, πσ x y =, Hσ L L =, Hσ ( Φ = y. ( + y exp[( ( + y erfc( π T where, σ and γ are variances of the elevations and slopes, respectively. And the definitions of and T are the same with Fuks and Godin []. It is clearly that the probability of the travel time of the first arrival is only the function of the dimensionless parameter T, which depends on the height of the source and variances of the surface statistics. Secondly, when the surface satisfies Exponential distribution (ED, the PDFs of the surface elevation ξ and slope ɺ ξ are written: ξ exp( ω( ξ = σ σ, ξ >, ξ ( ɺ ξ exp( ω( ɺ ξ = γ γ, ɺ ξ >, ɺ ξ ( where, σ and γ are the variances of the elevations and slopes, respectively. The mean value of ξ and ɺ ξ are σ and γ. At this case, the cumulative PDF also satisfied Equation (8. Substituting (8-( into (, ( and (4, yields the probability function F ( : πt exp( F ( = exp L y exp[ ( y + dy ] L πt (3a πt exp( ( exp y F = exp[ ( y + (3b L πt dy ] L exp[ ( + y ] Where = +, T = T, x y =, Hσ L L =. Hσ The PDFs of the first and the second travel times are given by: F ( ( = n ω n, n=, (4 d We conclude from (3 that the probability distribution of the travel time of the first arrival is only determined by the dimensionless parameter T. Furthermore, the discrepancy between (a and (b or between (3a and (3b can be neglected for any > when T >> in terms of our numerical results. Therefore, it is reasonable that we only apply the Equation (a in the following analysis. In Figure, the probability distribution functions of F ( *, and the corresponding PDFs are shown for a set of T parameters for the surfaces with Gaussian (solid, Rayleigh (dotted and Exponential (dashed distributions, respectively. According to [], the probability distribution function F ( of the travel time of the second arrival satisfies the following equation: * From equations ( and (3, we may obtain π F ( = F ( for Rayleigh 4 π 4 π distribution and F ( = F ( for Exponential distribution ISSN: 9-777 6 Issue 3, Volume, March

F ( = [ ln F ( ] F ( (5 Then the probability functions F, the PDFs ω ( of the second travel time are easily obtained by using Equations (-(5, as shown in Figure 3. The parameters are taken same as that in Figure. From Figure and 3, it is seen that for a given T F ( and F ( are different for three rough surfaces. For the peak values of PDFs of travel times of the first and second arrivals, the Gaussian surface correspond to the maximum, and the Exponential surface is minimum. The maximums of PDFs of travel times increase with T increasing for Rayleigh and Gaussian surfaces and are not related with T approximately for Exponential distributions. F(.8.6.4. T= 3 4 5 3 4 3 5 4 T= 5 Gaussian Reyleigh Exponential 3 4 5 6 7 8 9 ω(.5.5 5 4 T= 3 4 5 3 3 4 T= 5 Gaussian Reyleigh Exponential 3 4 5 6 7 8 9 Fig.. Comparison of probability distributions of travel time of the first arrival of a short pulse backscattered by Gaussian (solid lines, Rayleigh(dotted lines and Exponential(dashed lines surfaces. ISSN: 9-777 63 Issue 3, Volume, March

F( ω(.8.6 T= 3 4 3 4 5 T= 4.4 5 5 Gaussian. Reyleigh Exponential 3 4 5 6 7 8 9.5.5 T= 3 5 4 4 5 3 3 4 T= 5 Gaussian Reyleigh Exponential 3 4 5 6 7 8 9 Fig.3. Comparison of probability distributions of travel time of the second arrival of a short pulse backscattered by Gaussian (solid lines, Rayleigh(dotted lines and Exponential(dashed lines surfaces. 3. The median value of travel time The median values of the first and second travel times are defined as the following forms: F ( m =, (6 F ( = In the limiting case >>, the equations ( and (3 have the following simple expressions F ( = exp[ π π T exp( (7 F ( = exp[ π T exp( ] (8 Accepting the equations (7 and (8, in term of the definitions of median value of travel times of the first and the second arrival, the median values m and should satisfy the following equations m ] m exp[ m π π m exp( ] = RD (9 exp[ π T exp( m ] = ED ( When ln T >>, applying the similar method in [], the asymptotic solution to (9 is given π m (lnt+ 5.98 ( We may easily obtain the solution to ( RD m lnt +. ED ( Then the median value m and m of the second arrivals takes the form similar to ( and (: ISSN: 9-777 64 Issue 3, Volume, March

π m (ln T+ 4. RD (3 m lnt +.3 ED (4 At the case of ln T >>, the difference between the median values is given.34 δ = m m RD lnt (5 δ = m m.88 ED (6 Table shows the median values and time delay of travel times of the first and the second arrivals for the Gaussian, Rayleigh and Exponential cases. It can be seen from Table that for the Rayleigh distribution, the median values of the travel times of the first and second arrivals are proportional to ln T, and the difference between m and m are inversely proportional to ln T. There exits similar relation in the case of Gaussian distribution [], but these proportional constants are all different to the that of Gaussian surface. For example, the proportional constant between (or m and ln T is m at the case of Rayleigh surface, but for the Gaussian surface. And for the Exponential distribution, it is found that the mean values m, m are proportional to ln T, and δ is a constant and not associated with the parameter T. 3.3 Relations between the median values of travel times and the altitude of source The dimensionless parameter T can be written as: T = H S (7 γ where H is the altitude of source, S =. As is πσ known that ln( H S = ln H+ ln S, the relations between the median values of travel times and the altitude of source are given Ζ=Κ ln H+Β (8 where Ζ is the function of m (or m, which is different for the Gaussian, Rayleigh and Exponential surfaces cases (see Table, Κ is the slope, Β is a constant. The relations between the median values of travel times and the altitude of source for the Gaussian, Rayleigh and Exponential cases are shown in Table. Ζ and Κ are calculated in terms of the analytical expresses shown in Table. Κ, Κ and Κ 3 are the numerical results when H is varying in the range 7,.5, and, respectively. It can be [ ] 4.5.8 T= 3 F(δ.6.4. T= 3 W(δ.5.5.5 δ.5.5 δ ISSN: 9-777 65 Issue 3, Volume, March

.5 F(δ.8.6.4. T= 4 W(δ.5 T= 4.5.5 δ.5.5 δ.5 F(δ.8.6.4. T= 5 W(δ.5 T= 5.5.5 δ.5.5 δ Fig. 4. The probability distributions and corresponding PDFs of the travel time delay between the first and the second arrivals of a short pulse backscattered by Gaussian (solid lines, Rayleigh (dotted lines and Exponential (dashed lines surfaces. seen from Table that there is the linear relation between Ζ and Κ. And the values of Κ are almost a constant. It is clear that the relations between the median values of travel times and the altitude of source are different for the Gaussian, Rayleigh and Exponential surfaces cases. Therefore, the results shown in Table suggest that the relation between ( and the altitude of source can be used to m m judge whether the scattering surface is Gaussian distribution or not. After the statistical characteristic of the rough surface is specified in advance, we may apply the similar method in Refs.[] to obtain the parameters of the rough surface. 3.4 Time delay between the first and the second arrival In [], Fuks and Godin think the scale of time delay being sensitive only to σ. Thus, we should discuss the statistical properties of the time delay between the first and second arrival in this subsection. It is helpful to determine the parameters of surface with non-gaussian distributions under our considering circumstance. Table.. The median values and time delay of the first and the second arrivals of a short pulse backscattered by Gaussian (GD, Rayleigh (RD and Exponential surfaces (ED GD RD ED m lnt+.73 m lnt.4 π (ln T+ 5.98 π (ln T+ 4. ln T+. ln T+.3 ISSN: 9-777 66 Issue 3, Volume, March

δ.88 lnt.34 lnt.88 Table.. The relations between the median values of travel times and the altitude of source for Gaussian (GD, Rayleigh (RD and Exponential cases (ED GD RD SD Ζ m m m + π m + π m m Κ.33.5 Κ.95.4.5 Κ.97.38.5 Κ 3.98.36.5 The probability distribution function of the time delay between the first and second arrivals is also derived: F ( δ = C ω( + δ F ( d (9 W ( δ = Cθ ( δ ω( + δ ω ( d (3 Where = ω ( ( C F d = ω ( F ( d θ (x is the unit step function:, x θ ( x =, x< (3 Figure 4 is the probability distributions and corresponding PDFs of the travel time delay between the first and second arrivals for Gaussian, (solid lines, Rayleigh (dotted lines and Exponential (dashed lines surfaces. The values of 3 4 5 T in Figure 4 are chosen to, and, respectively. From Figure 4, the PDF of time delay between the first and second arrivals is determined by the parameter T for Rayleigh surfaces. At the case of Exponential distributions, the PDFs of time delay are holding constant for different values of T. When δ is small, the PDF of the case of Gaussian is maximum, Rayleigh is following and Exponential is minimum, while for the large δ, on the contrary, that is, Exponential is the maximum and Gaussian is the minimum. 4 Conclusion We have considered the problem of travel time of a short pulse backscattered from rough surface with special non-gaussian (Rayleigh and Exponential distributions, which are different from []. The main results obtained are summarized below: ( For all consider cases, the probability distributions of travel times of the first and second arrival are only the function of the dimensionless parameter T. ( For the Rayleigh distribution, the median values of the travel times of the first and second ISSN: 9-777 67 Issue 3, Volume, March

arrivals are proportional to ln T, and the difference δ between m and m are inversely proportional to ln T. The proportional constants of these relations above are all different to that of Gaussian surface. For the Exponential distribution, and are proportional to ln T, and δ is independent approximately with the parameter T. (3 It is confident that we are able to distinguish surfaces among Gaussian, Rayleigh and Exponential by use of the results in Table in section 3.3. After the statistical characteristic of the rough surface is specified in advance, the results of this paper can be applied to retrieve the parameters of the non-gaussian (Rayleigh and Exponential random surface. 5 Acknowledgments The authors would like to thank the reviewers of the paper for their relevant comments. And the author also wishes to thank Prof. WANG N, Dr. GAO D Z and Dr. WANG H Z of Department of Physics, Ocean University of China for their invaluable suggestions. References: [] A. G. Voronovich, Wave Scattering from Rough Surfaces, Berlin: Springer, 998. [] R. J. Dobosy, T. L. Crawford, D. C. Vandemark, Measurement of ocean surface in shoaling zones by laser array and Ka-band radar, Proc. 4 th Int. Airborne Remote Sensing Conf, Vol., 999, pp: 66-73. [3] D. R. Watts, H. T. Rossby, Measuring dynamic heights with inverted echo sounders: results from MODE, J. Phys. Oceanogr, Vol.7, No.3, 977, pp: 345-358. [4] D. B. Chelton, E. J. Walsh, J. L. Mac Artur, Pulse compression and sea level tracking in satellite altimetry, J. Atmos. Ocean. Technol, Vol.6, No.3, 989, pp: 47-438. [4] [5] V. M. Frolov, Multiple reflection of a beam from the disturbed surface of the ocean, Sov. Phys. Acoust, Vol.3, 985, pp: 58-6. m m [6] V. M. Frolov, Condition for the applicability of ray tracing in a waveguide with a rough boundary, Sov. Phys. Acoust, Vol.36, 99, pp:6-64. [7] T. Elfouhaily, D. R. Thompson, B. Chapron, Improved electromagnetic bias theory, J. Geophys. Res, Vol.5, No.C,, pp: 99-3. [8] T. Elfouhaily, D. R. Thompson, L. Linstrom, Delay-Doppler analysis of bistatically reflected signals from the ocean surface: theory and application, IEEE Trans. Geosci. Remote Sens, Vol.4, No.3,, pp:56-573. [9] O. A. Godin, I. M. Fuks, Travel-time statistics for signals scattered at a rough surface, Waves Random Media, Vol.3, No.4, 3, pp: 5-. [] M. R. Leadbettter, G. Lindgren, H. Rootzen, Extremes and Related Properties of Random Sequences and Processes, New York: Springer, 983. [] Y. A. Fomin, Excursions Theory of Stochastic Processes, Moscow: Nauka, 98. [] I. M. Fuks, O. A. Godin, Probability distributions of travel time and intensity of the earliest arrivals of a short pulse backscattered by a rough surface, Waves Random Media, Vol.4, No.4, 4, pp: 539-56. [3] I. M. Fuks, Probability distributions of elevation and curvature of specular points at a statistically rough surface, Antennas and Propagation Society International Symposium, IEEE, Vol.3A, 5, pp: 437-44. [4] I. M. Fuks, M. I. Charnotskii, Statistics of specular points at a randomly rough surface, J. Opt. Soc. Am. A., Vol.3, No., 6, pp: 73-8. [5] W. Gao, N. Wang, Inversion of rough surface parameters based on travel-time statistics of backscattered pulses, Chinese Journal of Geophysics, Vol.5, No., 8, pp: 6-66. [6] B. G. Smith, Geometrical shadowing of random rough surfaces, IEEE Trans. Antennas. Propag., Vol.5, 967, pp: 668-67 ISSN: 9-777 68 Issue 3, Volume, March