N. Pierdicca 1 , L. Guerriero 2  , R. Giusto 1 , M. Brogioni 3 , A. Egido 4 , N. Floury 5 1 DIET - Sapienza Univ. of Rome,...
Content <ul><li>Introduction: the Leimon project </li></ul><ul><li>Simulator description </li></ul><ul><li>Simulator valid...
LEiMON Project <ul><li>Land MOnitoring with Navigation signals </li></ul><ul><li>Evaluating the potential of GNSS  signals...
The LEIMON experiment FDR and TDR soil moisture probes Meteo station Soil roughness profilometer Bare (different roughness...
Time serie overview West field with developed plants
|Y | 2   Processed signal power at the receiver vs. delay    and frequency  f . P T   The transmitted power of the GPS ...
The BRE integration <ul><li>In order to solve the integral we have to introduce the equations relating all those  variable...
Local vs global frames <ul><li>Given RX and TX trajectory/velocity & epoch, integral is computed in the local frame, where...
 ° electromagnetic modelling Indefinite mean surface plane with roughness at wavelength scale.  Bistatic scattering of lo...
Polarization synthesis for real  antennas <ul><li>Nominal polarization unit vector are  p RHCP =(  0 - j  0 )/ √2   and ...
The signal simulator structure <ul><li>Geometric module: </li></ul><ul><li>GPS TX orbit </li></ul><ul><li>SP position </li...
AIEM vs scattering direction   s ,  s  i =31° m v =20 %   z =1.5 cm l=5 cm H RX =10 km HPBW=120° <ul><li>Incoherent co...
DDM output example DDM’s (delay on the horizontal axes, frequency on the vertical axes) for incoherent  (top) and coherent...
Peak power output example m v =20 %   z =1.5 cm l=5 cm H RX =10 km V RX =180 m/s Head RX =45° HPBW=120° <ul><li>Coherent ...
<ul><li>The incoherent signal fluctuates (speckle) with long correlation time (15 sec) so only incoherent summation was fe...
<ul><li>August 26th  SMC=10%   </li></ul><ul><li>East   Z =0.6 cm   </li></ul><ul><li>West   Z =1cm </li></ul><ul><li>Ap...
<ul><li>August 26th  SMC=10%   </li></ul><ul><li>East   Z =0.6 cm   </li></ul><ul><li>April 8th  SMC=30%   </li></ul><ul>...
<ul><li>General overestimation of the DOWN/UP ratio but good correlation </li></ul><ul><li>Cross talk and/or different dow...
RMSE=7.25 dB Bias=6.1 dB <ul><li>The model underestimates RR polarization, especially at smaller angles </li></ul><ul><li>...
RR underestimation RR August 26th  SMC=10%    Z =0.6cm   <ul><li>At large incidence angle, the RR coherent component is t...
Vegetation o verall comparison Fair correspondence between model and vegetation data (except for largest angle   =55°) Ju...
Sensitivity to SMC Black:  Leimon data (May) and regression line  Blue/ Red : Theoretical simulations, two roughnesses <ul...
Sensitivity to vegetation  Magenta: Leimon data  Green: Theoretical simulations vs. PWC  <ul><li>Model sensitivity reprodu...
Coherent vs Incoherent: vegetation At 35°,   the coherent component   is attenuated by about 1 dB each 1kg/m2, which would...
Conclusions <ul><li>A simulator has been developed which provides DDM’s and waveforms of a GNSS-R system looking at land <...
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FR4.T05.1.ppt

  1. 1. N. Pierdicca 1 , L. Guerriero 2 , R. Giusto 1 , M. Brogioni 3 , A. Egido 4 , N. Floury 5 1 DIET - Sapienza Univ. of Rome, Rome, Italy 2 DISP - University of Tor Vergata, Rome, Italy 3 CNR/IFAC, Sesto Fiorentino. Italy 4 Starlab, Barcelona, Spain 5 ESA/ESTEC, Noordwyik, The Netherland GNSS Reflection from Bare and Vegetated Soils: Experimental Validation of an End-to-end Simulator
  2. 2. Content <ul><li>Introduction: the Leimon project </li></ul><ul><li>Simulator description </li></ul><ul><li>Simulator validation during Leimon </li></ul><ul><li>Conclusions </li></ul>
  3. 3. LEiMON Project <ul><li>Land MOnitoring with Navigation signals </li></ul><ul><li>Evaluating the potential of GNSS signals for remote sensing soil moisture and vegetation biomass, through a ground based experimental campaign </li></ul><ul><li>Developing a simulator to theoretically explain experimental data and predict the capability of a GNSS-R aerospace systems </li></ul>The SAM dual pol GNSS-R instrument (by Starlab) LEiMON set up
  4. 4. The LEIMON experiment FDR and TDR soil moisture probes Meteo station Soil roughness profilometer Bare (different roughness) and vegetated fields Plant height and water content
  5. 5. Time serie overview West field with developed plants
  6. 6. |Y | 2 Processed signal power at the receiver vs. delay   and frequency f . P T The transmitted power of the GPS satellite. G T , G R The antenna gains of the transmitting and the receiving instrument. R R , R T The distance from target on the surface to receiving and transmitting antennas. T i The coherent integration time used in signal processing.  Bistatic scattering coefficient  2 The GPS correlation (triangle) function S 2 The attenuation sinc function due to Doppler misalignment dA Differential area within scattering surface area A (the glistening zone). The mean power of received signal vs. delay  and frequency f is modeled by integral Bistatic Radar Equation which includes time delay domain response    ’  and Doppler domain response S 2 ( f’-f ) of the system (Zavorotny and Voronovich, 2000). The Bistatic Radar Equation
  7. 7. The BRE integration <ul><li>In order to solve the integral we have to introduce the equations relating all those variables to the coordinates over the surface. </li></ul>function of point scattering delay function of point looking direction wrt boresight function of incidence direction function of point wrt RX and TX position function of point bistatic angle (zenith and azimuth) function of point scattering Doppler Integrand variables are the coordinates defined on the surface
  8. 8. Local vs global frames <ul><li>Given RX and TX trajectory/velocity & epoch, integral is computed in the local frame, where soil/vegetation parms are defined </li></ul><ul><li>Elliptic Earth approximation </li></ul><ul><li>x’y’z’ local frame centered in the specular point </li></ul><ul><li>z’ axes along the geodetic vertical </li></ul><ul><li>x’z’ plane coincident with the bistatic scattering plane </li></ul>z’ x’ y’ TX RX SP= [ x s ,y s ,z s ] ECEFF Earth ellipsoide  i  s =  i Earth surface x z y 
  9. 9.  ° electromagnetic modelling Indefinite mean surface plane with roughness at wavelength scale. Bistatic scattering of locally incident plane waves by AIEM Homogeneous vegetation cover. Attenuation and multiple scattering by a discrete medium (Tor Vergata model) INCOHERENT component COHERENT component Scattering of spherical wave by Kirchoff approxi. (Eom & Fung, 1988) attenuated by vegetation
  10. 10. Polarization synthesis for real antennas <ul><li>Nominal polarization unit vector are p RHCP =(  0 - j  0 )/ √2 and p LHCP =(  0 + j  0 )/ √2 </li></ul><ul><li>Real antenna polariz. unit vector </li></ul><ul><li>SCS of “real” antennas and channel cross talk </li></ul>2 orthogonal electric dipoles  /2 phase shifted x y z P = r,  , 
  11. 11. The signal simulator structure <ul><li>Geometric module: </li></ul><ul><li>GPS TX orbit </li></ul><ul><li>SP position </li></ul>E.M. bare soil bistatic  ° model Simulator core E.M. vegetation bistatic  ° model
  12. 12. AIEM vs scattering direction  s ,  s  i =31° m v =20 %  z =1.5 cm l=5 cm H RX =10 km HPBW=120° <ul><li>Incoherent component RR & LR more spread </li></ul><ul><li>Coherent component RR & LR focused around specular  s =31° </li></ul>Azimuth  Azimuth  Zenith  Zenith 
  13. 13. DDM output example DDM’s (delay on the horizontal axes, frequency on the vertical axes) for incoherent (top) and coherent (bottom) component at RHCP (left) and LHCP (right) Spaceborne incoherent airbone incoherent
  14. 14. Peak power output example m v =20 %  z =1.5 cm l=5 cm H RX =10 km V RX =180 m/s Head RX =45° HPBW=120° <ul><li>Coherent and incoherent RR & LR peak power as the satellite moves along the orbit </li></ul>
  15. 15. <ul><li>The incoherent signal fluctuates (speckle) with long correlation time (15 sec) so only incoherent summation was feasible </li></ul><ul><li>Different soil/vegetation conditions investigated </li></ul>Leimon data <ul><li>In the Leimon experiment the instrument records temporal series of the direct and reflected signals (I&Q of the correlator output peak) </li></ul><ul><li>The mean reflected power (both LR and RR pol) normalized to the mean direct power (at RR pol.) is studied vs. the incidence angle </li></ul>reflected direct
  16. 16. <ul><li>August 26th SMC=10% </li></ul><ul><li>East  Z =0.6 cm </li></ul><ul><li>West  Z =1cm </li></ul><ul><li>April 8th SMC=30% </li></ul><ul><li>East field  Z =3cm </li></ul><ul><li>West field  Z =1.75cm </li></ul>Simulator reproduces quite well LR signal versus  at incidence angles  ≤45°. Validation: angular trend
  17. 17. <ul><li>August 26th SMC=10% </li></ul><ul><li>East  Z =0.6 cm </li></ul><ul><li>April 8th SMC=30% </li></ul><ul><li>East  Z =3cm </li></ul>Theoretical simulations show that incoherent component strongly contributes to total signal when soil is rough. Coherent vs. incoherent: soil coherent total
  18. 18. <ul><li>General overestimation of the DOWN/UP ratio but good correlation </li></ul><ul><li>Cross talk and/or different down and up antenna gains could explain the bias </li></ul>RMSE=1.6 dB Bias=-1.4 dB Bare soil overall comparison LR East Side , West Side Bare Soils 10%<SMC<30% 0.6<  z <3cm
  19. 19. RMSE=7.25 dB Bias=6.1 dB <ul><li>The model underestimates RR polarization, especially at smaller angles </li></ul><ul><li>The RR measurements seem to saturate at -18 dB </li></ul><ul><li>A deficiency of the mode could occur </li></ul>Bare soil overall comparison RR East Side , West Side
  20. 20. RR underestimation RR August 26th SMC=10%  Z =0.6cm <ul><li>At large incidence angle, the RR coherent component is the dominant one </li></ul><ul><li>Theoretical incoherent RR scattering (rough case) may be underestimated </li></ul>RR April 8th SMC=30%  Z =3cm coherent total
  21. 21. Vegetation o verall comparison Fair correspondence between model and vegetation data (except for largest angle  =55°) June 28, July 10,28 22<SMC<18% PWC=1.2, 3.6, 6.7 kg/m 2
  22. 22. Sensitivity to SMC Black: Leimon data (May) and regression line Blue/ Red : Theoretical simulations, two roughnesses <ul><li>Model predicts  2.5 dB for a 10% SMC difference </li></ul><ul><li>Leimon shows  2.8 dB </li></ul>
  23. 23. Sensitivity to vegetation Magenta: Leimon data Green: Theoretical simulations vs. PWC <ul><li>Model sensitivity reproduces the measured one </li></ul><ul><li>Sensitivity to vegetation is quite low: about 2 dB for the whole PWC range </li></ul>
  24. 24. Coherent vs Incoherent: vegetation At 35°, the coherent component is attenuated by about 1 dB each 1kg/m2, which would predict a large sensitivity to PWC <ul><li>The Simulator predicts a quite large incoherent component which explains the saturation effect with PWC in the data. </li></ul><ul><li>The model reproduces the measured trend thanks to the consideration of both component </li></ul>
  25. 25. Conclusions <ul><li>A simulator has been developed which provides DDM’s and waveforms of a GNSS-R system looking at land </li></ul><ul><li>It takes as input arbitrary receiver position/velocity, in view GPS satellite PRN code, surface properties (soil moisture, roughness, vegetation parameters). </li></ul><ul><li>It singles out coherent and incoherent signal components. </li></ul><ul><li>A fair agreement has been found at LR polarization and angles <45° (the antenna beamwidth) </li></ul><ul><li>Incoherent component may be high in a ground based configuration, and antenna properties must be considered </li></ul><ul><li>Sensitivity to SMC is significant and well reproduced </li></ul><ul><li>Sensitivity to vegetation is reproduced and it is quite low because of the coherent and incoherent combination. </li></ul><ul><li>A few discrepancies could be due to measurement or model problems (of course) and are under investigation </li></ul>
  26. 26. Thank you for your attention
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