Brian Breitsch
...
2018 May 11
dielectric constant of sea water \(\varepsilon\)
dependent on frequency, temperature, and salinity
GPS satellite transmitting signals at three frequencies
(1.1-1.5 GHz)
High-gain dish antenna collects right-hand circular (RHC) and left-hand circular (LHC) polarized signals
want to try to measure these
Receiver measures received signal power at multiple frequencies and grazing angles
non-magnetic material
GPS satellite transmits RHP
\(R = \) RHC, \(L =\) LHC, \(V = \) vertical, \(H = \) horizontal
complex Fresnel relations
refractive indices
reflected power
FOR SPECULAR REFLECTION
L1
L2
L5
LHC
RHC
increasing temperature
increasing salinity
assume constant sea surface parameters, then fit curve to data
L1
L2
L5
different transmitted power
tropospheric scintillation irrelevant data
use this part
LHC
RHC
Text
Zavorotny, Valery U., and Alexander G. Voronovich. "Scattering of GPS signals from the ocean with wind remote sensing application." IEEE Transactions on Geoscience and Remote Sensing 38.2 (2000): 951-964.
Valencia, E., et al. "Improving the accuracy of sea surface salinity retrieval using GNSS‐R data to correct the sea state effect." Radio Science 46.6 (2011).
http://www.salinityremotesensing.ifremer.fr/sea-surface-salinity/salinity-distribution-at-the-ocean-surface