Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry

Ocean altimetry with Global Navigation Satellite Systems signals (GNSS) signals is a remote sensing technique that measures the height of the sea surface through the difference in path length of the direct and reflected signal. Code altimetry estimates this parameter by tracking the code delay after...

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Main Authors: Santiago Ozafrain, Pedro A. Roncagliolo, Carlos H. Muravchik
Format: Article
Language:English
Published: IEEE 2019-01-01
Series:IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
Subjects:
Online Access:https://ieeexplore.ieee.org/document/8962226/
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author Santiago Ozafrain
Pedro A. Roncagliolo
Carlos H. Muravchik
author_facet Santiago Ozafrain
Pedro A. Roncagliolo
Carlos H. Muravchik
author_sort Santiago Ozafrain
collection DOAJ
description Ocean altimetry with Global Navigation Satellite Systems signals (GNSS) signals is a remote sensing technique that measures the height of the sea surface through the difference in path length of the direct and reflected signal. Code altimetry estimates this parameter by tracking the code delay after performing correlations with a GNSS signal replica. It is of limited precision due to the low signal-to-noise ratio (SNR) and narrow bandwidth of the ocean-reflected GNSS signal. However, the potential advantages of the GNSS-R systems such as high temporal resolution and spatial coverage are a motivation to improve its altimetric precision. In this article, we present a performance assessment of the Likelihood Map Waveform tracking technique, a method based on Maximum Likelihood Estimation theory that exploits the available reflected power in a more efficient way than the single tracking point methods. We use a modification of the theoretical optimal solution that achieves a better performance than previous methods. We estimate it, in terms of SNR gain, using Monte Carlo method with a detailed stochastic model of the signal, and with actual signals from the Cyclone Global Navigation Satellite System. The gain values obtained were between 1.64 and 3.66 dB in the theoretical analysis, and between 1.69 and 2.62 dB with the real data, confirming the potential of the proposed approach.
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spelling doaj.art-20012b9ae24a43fc9968eac5ca80cf942022-12-21T21:58:43ZengIEEEIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing2151-15352019-01-0112125379538410.1109/JSTARS.2019.29635598962226Likelihood Map Waveform Tracking Performance for GNSS-R Ocean AltimetrySantiago Ozafrain0https://orcid.org/0000-0002-1068-0420Pedro A. Roncagliolo1https://orcid.org/0000-0002-1582-7030Carlos H. Muravchik2https://orcid.org/0000-0003-2954-6675Sistemas Electrónicos de Navegación y Telecomunicaciones, Facultad de Ingeniería, Universidad Nacional de La Plata, La Plata, ArgentinaSistemas Electrónicos de Navegación y Telecomunicaciones, Facultad de Ingeniería, Universidad Nacional de La Plata, La Plata, ArgentinaInstituto de Investigaciones en Electrónica, Control y Procesamiento de Señales (LEICI; UNLP-CONICET) and CIC-PBA, La Plata, ArgentinaOcean altimetry with Global Navigation Satellite Systems signals (GNSS) signals is a remote sensing technique that measures the height of the sea surface through the difference in path length of the direct and reflected signal. Code altimetry estimates this parameter by tracking the code delay after performing correlations with a GNSS signal replica. It is of limited precision due to the low signal-to-noise ratio (SNR) and narrow bandwidth of the ocean-reflected GNSS signal. However, the potential advantages of the GNSS-R systems such as high temporal resolution and spatial coverage are a motivation to improve its altimetric precision. In this article, we present a performance assessment of the Likelihood Map Waveform tracking technique, a method based on Maximum Likelihood Estimation theory that exploits the available reflected power in a more efficient way than the single tracking point methods. We use a modification of the theoretical optimal solution that achieves a better performance than previous methods. We estimate it, in terms of SNR gain, using Monte Carlo method with a detailed stochastic model of the signal, and with actual signals from the Cyclone Global Navigation Satellite System. The gain values obtained were between 1.64 and 3.66 dB in the theoretical analysis, and between 1.69 and 2.62 dB with the real data, confirming the potential of the proposed approach.https://ieeexplore.ieee.org/document/8962226/GNSS+RLow Earth Orbit (LEO)maximum likelihood estimationocean altimetryremote sensing
spellingShingle Santiago Ozafrain
Pedro A. Roncagliolo
Carlos H. Muravchik
Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry
IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
GNSS+R
Low Earth Orbit (LEO)
maximum likelihood estimation
ocean altimetry
remote sensing
title Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry
title_full Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry
title_fullStr Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry
title_full_unstemmed Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry
title_short Likelihood Map Waveform Tracking Performance for GNSS-R Ocean Altimetry
title_sort likelihood map waveform tracking performance for gnss r ocean altimetry
topic GNSS+R
Low Earth Orbit (LEO)
maximum likelihood estimation
ocean altimetry
remote sensing
url https://ieeexplore.ieee.org/document/8962226/
work_keys_str_mv AT santiagoozafrain likelihoodmapwaveformtrackingperformanceforgnssroceanaltimetry
AT pedroaroncagliolo likelihoodmapwaveformtrackingperformanceforgnssroceanaltimetry
AT carloshmuravchik likelihoodmapwaveformtrackingperformanceforgnssroceanaltimetry