scholarly journals Turbulence and suspended sediment processes in the Garonne River tidal bore in November 2016

2019 ◽  
Vol 34 (5) ◽  
pp. 496-508
Author(s):  
David Reungoat ◽  
Xinqian Leng ◽  
Hubert Chanson
Author(s):  
Lucille Furgerot ◽  
Pierre Weill ◽  
Dominique Mouazé ◽  
Bernadette Tessier

2013 ◽  
Vol 14 (3) ◽  
pp. 591-616 ◽  
Author(s):  
David Reungoat ◽  
Hubert Chanson ◽  
Bastien Caplain

2015 ◽  
Vol 53 (3) ◽  
pp. 291-301 ◽  
Author(s):  
David Reungoat ◽  
Hubert Chanson ◽  
Claire E. Keevil

2020 ◽  
Author(s):  
Pierre Zeiger ◽  
José Darrozes ◽  
Frédéric Frappart ◽  
Guillaume Ramillien ◽  
Laurent Lestarquit ◽  
...  

<p>The Reflected Global Navigation Satellite System (GNSS-R) is a bi-static radar system in which the receiver collect GNSS signals reflected from the Earth surface and compares them with corresponding direct signals. Measurements can be performed on the waveforms to determine the elevation of the free surface, leading to applications such as ocean altimetry, inland water level variations, soil moisture, snow depth and atmospheric water changes. This study presents the potential of in-situ GNSS-R for tidal bore detection and characterization, and compares it to high rate GNSS observations and other reference datasets.</p><p>The data we used were acquired on 17<sup>th</sup> and 18<sup>th</sup> October 2016 in the Garonne River, at 126 km upstream the mouth of the Gironde estuary. We processed GNSS-based elevations from data acquired on a buoy at a 20 Hz sampling rate using differential GNSS (DGNSS) technique. Acoustic Doppler Current Profiler (ADCP) measurements as well as pressure data were used for validation purposes. These techniques show good results in estimating the amplitude of the first wave, the period of the tidal bore and the oceanic tides. All of these datasets were compared to the retrieval of GNSS-R signals above the river. We have processed the changes in water height throughout the acquisition using <em>Larson et al.</em> (2013) and <em>Roussel et al.</em> (2015) techniques. We finally separate the atmospheric component from the tidal bore and the oceanic tides ones.</p><p> </p><p>Larson, K. M., Löfgren, J. S., and Haas, R. (2013). Coastal sea level measurements using a single geodetic gps receiver. Advances in Space Research, 51(8):1301–1310.</p><p>Roussel, N., Ramillien, G., Frappart, F. et al. (2015). Sea level monitoring and sea state estimate using a single geodetic receiver. Remote Sensing of Environment, 171:261 – 277.</p>


2015 ◽  
Vol 40 (12) ◽  
pp. 1574-1586 ◽  
Author(s):  
Claire E. Keevil ◽  
Hubert Chanson ◽  
David Reungoat

2006 ◽  
Author(s):  
M. R. Delgado Blanco ◽  
M. Olabarrieta Lizaso ◽  
A. Giardino ◽  
R. Banasiak ◽  
R. Verhoeven ◽  
...  

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