Wöppelmann Guy

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Professor in Earth Sciences
University of La Rochelle
Associated scientific institute at CNRS: INSU
Corresponding member of the BDL since 2022

Key words : Vertical land motion, GPS methods, sea level change, tide gauges
CV & Publications
Publications

Research interests

 

  • vertical displacements of the Earth’s surface at the coast using space geodetic methods (GPS, InSAR...);
  • sea level change over the past decades to century timescales using tide gauges;
  • performances of modern tide gauge technologies (acoustic, radar) and explore new ones (e.g., GNSS-IR);
  • data archeology: rescue, digitization and quality control of historical sea level records;
  • detection of spatial fingerprints of contemporary land ice melting in sea level records by combining in situ and satellite data;
  • unification of vertical references, in particular chart datums.

An example of tide gauge and GPS data combination:

 

 

  The figure on the right (click on the image to enlarge) shows how well can work corrections of tide gauge records using GPS velocities obtained from a state-of-the-art data analysis strategy. The left panels display annual mean sea levels from high-quality tide gauge records in three different regions of the world coasts (data available at the PSMSL international service). The right pannels show these records corrected for vertical land motion using GPS velocities from our latest solution of the ULR consortium. The spread observed in the rates of sea level change in the left panels is substantially reduced in the three regions (standar deviation of 0.3 mm/year). These results are updated from Wöppelmann et al. (2009) in Geophysical Research Letters.

 

 

  In the illustration on the left (click on the image) are represented the principal elements of the observational situation at a tide gauge. Satellite radar altimetry plays an increasing important role in sea level observation. However, to be useful for coastal studies on impacts (submersion, erosion, civil engineering, etc), its data requires a correction in order to transform the satellite geocentric sea levels into relative sea levels with respect to the land. High-precision GPS methods, for instance, can provide this supplementary data such as S = N - U (notations from the illustration) in the idealized case study depicted in the illustration. The situation can indeed be more complex, in particular because here is assumed that the tide gauge and the satellite are observing the same sea levels at the coast and offshore, respectively.


Articles representative of my recent scientific activities (5):

(Complete personal bibliography)

Contribution to books:



Scientific and administrative responsibilities (current)

 

  • since 2007: Member of the IAPSO Commission on Mean sea level and tides (IAPSO: International Association for the Physical Sciences of the Oceans);
  • since 2011: Director of the GNSS at tide gauge data assembly center of the GLOSS program of the IOC/UNESCO, hosted at SONEL;
  • since 2011: Member of the International GNSS Service (IGS) tide gauge (TIGA) working group;
  • since 2012: Chair of the science steering group of the GLOSS program above mentioned;
  • since 2015: Member of the CNES (French space agency) committee for the Solid Earth area (TOSCA).


Ph-D. Thesis Supervisions

 

  • Pira A. (2022-ongoing). GNSS-Reflectometry applied to sea level observation at high-frequency sampling and its extremes in hostile coastal areas. La Rochelle University, Viva scheduled in Autumn 2025.
  • Challis J. (2020-ongoing). Temporal evolution of tidal characteristics on the north-west European continental shelf. La Rochelle University in collaboration with BRGM and Shom, Viva scheduled in Autumn 2023.
  • Poitevin C. (2015 - 2019). Variabilité du niveau marin relatif le long du littoral de Brest (France) par combinaison de méthodes géodésiques spatiales (altimétrie radar, InSAR et GPS). Thèse de doctorat de l’université de la Rochelle, soutenue le 29 mai 2019.
  • Sakic P. (2013 - 2016). Apport de la géodésie de fond de mer à l’évaluation de l’aléa sismique côtier : distancemétrie en mer de Marmara et simulation GNSS/A aux Antilles. Thèse de doctorat de l’université de la Rochelle, soutenue le 9 décembre 2016.
  • Gouriou T. (2007- 2012). Evolution des composantes du niveau marin à partir d’observations de marégraphie effectuées depuis la fin du 18e siècle en Charente-Maritime. Thèse de doctorat de l’université de la Rochelle, soutenue le 26 mars 2012.
  • Santamaria-Gomez A. (2007-2010). Estimation des mouvements verticaux de l’écorce terrestre par GPS dans un repère géocentrique, dans le cadre du projet TIGA. Thèse de doctorat de l’Observatoire de Paris, soutenue le 11 octobre 2010.
  • Letetrel C. (2006-2010). Mouvements verticaux à la surface de la Terre par altimétrie radar embarquée sur satellite, marégraphie, et GPS. Thèse de doctorat de l’université de la Rochelle, soutenue le 25 août 2010.
  • Pouvreau N. (2004-2008). Trois cents ans de mesures marégraphiques en France : outils, méthodes et tendances des composantes du niveau de la mer au port de Brest. Thèse de doctorat de l’université de la Rochelle, soutenue le 26 septembre 2008.