Publications scientifiques

Cette page liste les productions scientifiques ou autres liées notamment à l'observation du niveau de la mer, à l'instrumentation ou aux applications.

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Coastal flooding of urban areas by overtopping: dynamic modelling application to the Johanna storm (2008) in Gâvres (France)

Recent dramatic events have allowed significant progress to be achieved in coastal flood modelling over recent years. Classical approaches generally estimate wave overtopping by means of empirical formulas or 1-D simulations, and the flood is simulated on a DTM (digital terrain model), using soil roughness to characterize land use. The limits of these methods are typically linked to the accuracy of overtopping estimation (spatial and temporal distribution) and to the reliability of the results in urban areas, which are places where the assets are the most crucial.
  • Article scientifique

S. Le Roy, R. Pedreros, C. André, F. Paris, S. Lecacheux, F. Marche, C. Vinchon
NHESS, volume 15
 Validation of the total sea level (tide and storm surge) and of the storm surge simulated with MARS in Port-Tudy (observation from http://refmar.shom.fr).

Sea level monitoring and sea state estimate using a single geodetic receiver

GNSS-Reflectometry (GNSS-R) altimetry has demonstrated a strong potential for sea level monitoring. Interference Pattern Technique (IPT) based on the analysis of the Signal-to-Noise Ratio (SNR) estimated by a GNSS receiver, presents the main advantage of being applicable everywhere by using a single geodetic antenna and receiver, transforming them to real tide gauges. Classical SNR analysis method used to estimate the variations of the reflecting surface height h(t) has a limited domain of validity due to its variation rate (dh/dt)(t) assumed to be negligible.
  • Article scientifique

N. Roussel, G. Ramillien, F. Frappart, J. Darrozes, A. Gay, R. Biancale, N. Striebig, V. Hanquiez, X. Bertin, D. Allain
Remote Sensing of Environment, volume 171
 Principle of GNSS tide gauge using a single GNSS antenna. ε : satellite elevation angle, δ: additional path covered by the reflected way (green line).

Estimation des niveaux marins extrêmes avec et sans l’action des vagues le long du littoral métropolitain

Pour caractériser le risque de submersion marine, il est très important d'avoir une connaissance précise des lois de distribution des niveaux d'eau marins, et plus particulièrement des niveaux d'eau extrêmes. En effet ce sont eux qui sont à l'origine des conséquences les plus dramatiques. Le programme de recherche mené au cours de cette thèse a été financé par le Ministère de l'Écologie, du Développement Durable et de l'Énergie.
  • Article scientifique

X. Kergadallan
Laboratoire d'Hydraulique Saint-Venant - Université Paris-Est
Mer du Nord, Manche et Atlantique : Niveaux d’eau moyens annuels recalés par rapport au port de Brest

Rapport technique final du projet NIVEXT - NIVeaux EXTrêmes

Ce rapport rend compte du travail effectué dans le cadre du projet NIVEXT financé par la DGPR. Le SHOM disposant de mesures marégraphiques sur les côtes françaises depuis 1850, en base de données numériques ou en dormance sous forme papier dans les archives, la possibilité d’établir un bilan de ce que ces données peuvent apporter à la connaissance des niveaux extrêmes est apparue une action nécessaire et cohérente avec la ligne portée par l’Etat.
  • Rapport d'étude

C. Daubord
Shom
Exemple de marégramme ancien : marégramme de Rochefort couvrant la période du 1 au 31 janvier 1890, récupéré pour l’analyse de l’évènement T16 (21 janvier 1890)

How historical information can improve estimation and prediction of extreme coastal water levels: application to the Xynthia event at La Rochelle (France)

The knowledge of extreme coastal water levels is useful for coastal flooding studies or the design of coastal defences. While deriving such extremes with standard analyses using tide-gauge measurements, one often needs to deal with limited effective duration of observation which can result in large statistical uncertainties. This is even truer when one faces the issue of outliers, those particularly extreme values distant from the others which increase the uncertainty on the results.
  • Article scientifique

T. Bulteau, D. Idier, J. Lambert, M. Garcin
NHESS, volume 15
Study site and water level data localisation

Tidal notches in Mediterranean Sea: a comprehensive analysis

Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean.
  • Article scientifique

F. Antonioli, V. Lo Presti, A. Rovere, L. Ferranti, M. Anzidei, S. Furlani, G. Mastronuzzi, P. E. Orru, G. Scicchitano, G. Sannino, C. R. Spampinato, R. Pagliarulo, G. Deiana, E. de Sabata, P. Sansò, M. Vacchi, A. Vecchio
Quaternary Science Reviews, volume 119
Morphometric measures: A) Average notch width, B) Notch depth, C) Bottom depth (reef when present), D) reef and step (if present) thickness, E) Depth of cliff toe at mean sea level.

Diet of Haplognathia ruberrima (Gnathostomulida) in a Caribbean marine mangrove

Haplognathia ruberrima is a cosmopolitan gnathostomulid species found in sulfur bacterial mats in mangroves in Guadeloupe (French West Indies). Haplognathia ruberrima presents a δ13C value lower than all measured meiofaunal grazers and lower than the available measured food sources of this environment. This low δ13C value can not be due to specific ingestion of 13C-depleted methanogenic bacteria because abundances of those bacteria are reduced in surficial and deep sediments as revealed by δ13C of bacterial fatty acid.
  • Article scientifique

P.-Y. Pascal, C. Bellemare, W. Sterrer, H. T. S. Boschker, S. Gonzalez-Rizzo, O. Gros
Marine Ecology, volume 36
 Scanning electron microscope analysis of Haplognathia ruberrima individuals freshly collected from marine mangrove. (A): In low magnification, the entire body surface of the individuals analysed presented this general aspect. (B and C): The general aspect is due to the presence of numerous long filaments individually attached to the body surface of the animal. (D): Higher magnification reveals these filaments to be long cilia that are likely responsible for the gliding movement observed in H. ruberrima ind

Regional circulation around New Caledonia from two decades of observations

The regional and near-coastal circulation around New Caledonia is investigated using a compilation of more than 20 years of observations. Velocity profiles acquired by Shipboard Acoustic Doppler Current Profiler (SADCP) during 109 research cruises and ship transits since 1991 are analyzed and compared with absolute geostrophic currents inferred from hydrographic profiles and Argo floats drifts. In addition, altimetric surface currents are used to explore the variability of the circulation at various timescales.
  • Article scientifique

S. Cravatte, E. Kestenare, G. Eldin, A. Ganachaud, J. Lefèvre, F. Marin, C. Menkes, J. Aucan
Journal of Marine Systems, volume 148
Journal of Marine Systems

A new hybrid model for filling gaps and forecast in sea level: application to the eastern English Channel and the North Atlantic Sea (western France)

This research is carried out in the framework of the program Surface Water and Ocean Topography (SWOT) which is a partnership between NASA and CNES. Here, a new hybrid model is implemented for filling gaps and forecasting the hourly sea level variability by combining classical harmonic analyses to high statistical methods to reproduce the deterministic and stochastic processes, respectively.
  • Article scientifique

I. Turki, B. Laignel, N. Kakeh, L. Chevalier, S. Costa
Ocean Dynamics, volume 65
Sea level components at studied stations: the astronomical tides AT(t) (grey points), the residual surges S(t) (white line), and the component SL(t) −MSLV (black line)