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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Ecoregional and temporal dynamics of dugong habitat use in a complex coral reef lagoon ecosystem

Mobile marine species display complex and nonstationary habitat use patterns that require understanding to design effective management measures. In this study, the spatio-temporal habitat use dynamics of the vulnerable dugong (Dugong dugon) were modelled from 16 satellite-tagged individuals in the coral reef lagoonal ecosystems of New Caledonia, South Pacific.
  • Article scientifique

S. Derville, C. Cleguer, C. Garrigue
Scientific Reports 12, article 552
Figure 1  Interpolated dugong GPS tracks recorded in 2012, 2013 and 2019 over the west coast of New Caledonia, South Pacific. The 16 tracks are split in different colors depending on the ecoregion they are in. Ecoregions identified through hierarchical clustering of environmental lagoon characteristics are represented with colored polygons. Ecoregion 3 is divided into two separate parts, one to the north of ecoregion 2 and another in between ecoregion 1 and 2. Land is shown in black and shallow reefs are sh

The Mw 7.5 Tadine (Maré, Loyalty Islands) earthquake and related tsunami of 5 December 2018: seismotectonic context and numerical modeling

On 5 December 2018, a magnitude Mw  7.5 earthquake occurred southeast of Maré, an island of the Loyalty Islands archipelago, New Caledonia. This earthquake is located at the junction between the plunging Loyalty Ridge and the southern part of the Vanuatu Arc, in a tectonically complex and very active area regularly subjected to strong seismic crises and earthquakes higher than magnitude 7 and up to 8.
  • Article scientifique

J. Roger, B. Pelletier, M. Duphil, J. Lefèvre, J. Aucan, P. Lebellegard, B. Thomas, C. Bachelier, D. Varillon
NHESS, volume 21
New Caledonia and the south Vanuatu subduction zone. The colored dots represent the seismicity from the USGS database for the period from 1 January 1900 to 24 January 2019, with the size of dots being proportional to the event's magnitude. Tsunamigenic earthquakes recorded in New Caledonia (Roger et al., 2019b; US Geological Survey, 2019) are highlighted with black-outlined circles and linked to dates. The black line symbolizes the Vanuatu Trench. The white arrows symbolize the subduction directions and rat

Wave overtopping and overflow hazards: application on the Camargue sea-dike

Dike breaches occurs regularly during storm events. This phenomenon contributes to amplify considerably the impact of floods on coastal areas. It represents an important cost for repairing existing infrastructures in the vicinity of the sea-dike. Then, they must be upgraded to prevent breaches. In the present study, ANEMOC and REFMAR dataset were analysed, off Camargue coasts, to quantify the storm hazards in terms of wave height and sea level wind setup. Repartition laws were adjusted on dataset to build a 2D-copula which is used to estimate events return periods.
  • Article scientifique

T. Paul, C. Lutringer, A. Poupardin, A. Bennabi, J. Jeaong, P. Sergent
Conf. TUC 2020, BE, Antwerp
Gumbel copula built from ANEMOC and REFMAR dataset and by fitting events with a Generalized Extreme Value Distribution (GEV)

Predicting Storm Surges

In this chapter, we present a second example of statistical estimation of extreme quantiles: millennial quantiles for storm surges at Brest (France), based on hourly sea-level measurements. We run sensitivity tests on parameter values, on the choice of analytic models for distributions, and on the statistical estimation methods chosen. Uncertainty in estimates and associated confidence intervals are also calculated and compared.
  • Article scientifique

M. Andreewsky
Extreme Value Theory with Applications to Natural Hazards, pp345-359, Springer, Cham
Extreme Value Theory with Applications to Natural Hazards From Statistical Theory to Industrial Practice

Improving storm surge and wave forecasts from regional to nearshore scales

Submersion risks assessment requires different tools and methods from regional to coastal scales. The Shom’s strategy relies on numerical modelling and observational systems applied in a challenging multi-scale context. At regional scales, storm surge and wave models Hycom and Wavewatch III, bathymetric digital terrain models (DTMs) and observational tide/buoy networks used within the operational national storm surge service (Homonim project with Météo-France) are presented, as well as their applications in climatological 40-year hindasts.
  • Article scientifique

A. Pasquet, H. Michaud, L. Seyfried, R. Baraille, L. Biscara, Y. Krien, D. Jourdan
9ᵗʰ EuroGOOS Conference, Virtual Edition
. 100- year return levels for Skew Surge observations (left), 100- year return levels for Hs observations (center) and 100- year return level  errors for Skew Surge and Hs (right).

Advances in estimating Sea Level Rise: A review of tide gauge, satellite altimetry and spatial data science approaches

Significant developments have been made in the observation systems and techniques of estimating sea level towards meeting the standard accuracy requirement of Global Climate Observation Systems (GCOS). This study undertakes a systematic review of the current advances in estimating sea level change in the context of the 4th industrial revolution. Trends in the use of main observation systems such as tide gauges, satellite altimetry, and ancillary systems such as GNSS and Autonomous Surface Vehicles were explored.
  • Article scientifique

N. Adebisi, A.-L. Balogun, T. Hee Min, A. Tella
Ocean & Coastal Management, volume 208
Graphical abstract

Sea Level Fusion of Satellite Altimetry and Tide Gauge Data by Deep Learning in the Mediterranean Sea

Satellite altimetry and tide gauges are the two main techniques used to measure sea level. Due to the limitations of satellite altimetry, a high-quality unified sea level model from coast to open ocean has traditionally been difficult to achieve. This study proposes a fusion approach of altimetry and tide gauge data based on a deep belief network (DBN) method.
  • Article scientifique

L. Yang, T. Jin, X. Gao, H. Wen, T. Schöne, M. Xiao, H. Huang
Remote Sensor
Graphical abstract

Timescale of emergence of chronic flooding in the major economic center of Guadeloupe

Sea-level rise due to anthropogenic climate change is projected not only to exacerbate extreme events such as cyclones and storms but also to cause more frequent chronic flooding occurring at high tides under calm weather conditions. Chronic flooding occasionally takes place today in the low-lying areas of the Petit Cul-de-sac marin (Guadeloupe, West Indies, French Antilles). This area includes critical industrial and harbor and major economic infrastructures for the islands.
  • Article scientifique

Le Cozannet G., D. Idier, M. de Michele, Y. Legendre, M. Moisan, R. Pedreros, R. Thiéblemont, G. Spada, D. Raucoules, Y. de la Torre
NHESS, volume 21
The Petit Cul-de-sac marin area in Guadeloupe, showing urbanized areas and altitudes (map created by BRGM; data: IGN, SHOM; © BRGM, IGN, SHOM).

Statistical Prediction of Extreme Storm Surges Based on a Fully Supervised Weather-Type Downscaling Model

Increasing our capacity to predict extreme storm surges is one of the key issues in terms of coastal flood risk prevention and adaptation. Dynamically forecasting storm surges is computationally expensive. Here, we focus on an alternative data-driven approach and set up a weather-type statistical downscaling for daily maximum storm surge (SS) prediction, using atmospheric hindcasts (CFSR and CFSv2) and 15 years of tidal gauge station measurements. We focus on predicting the storm surge at La Rochelle–La Pallice tidal gauge station.
  • Article scientifique

W. Costa, D. Idier, J. Rohmer, M. Menendez, P. Camus
Journal of Marine Science and Engineering
(A) Daily maximum storm surge (SS) time series at La Rochelle–La Pallice tidal gauge from 2000 to 2014 and the extreme events of Xynthia (February 2010) and Joachim (December 2011). (B) Descriptive probability distribution (bars) and cumulative probability of SS (dashed line).