Bathymetric and topographic model of the island of La Réunion. Topography is from IGN data. Bathymetry is derived from the multibeam data acquired during the campaigns Forever (2006, EM12D sounder) Eroder1 (2006, EM120 sounder) and Eroder2 (2007, EM120 sounder). The grid spacing is 300m.

Bathymetric model (DTM) of the Mediterranean. MediMap group. Bathymetry data acquired by multibeam sounders during campaigns Almofront.leg1 and Almofront.leg2, Almofront, Bretane, Seamewe2, Heralis, Medee, Anaxiprobe, Almofront2 - leg1 and leg2, Prismed2, Marmara, Fanil, Tvic5 et 6, Progres, Maradja, Blac, Nautinil, Medor-Simed1 / 2 / 3 / 4 / 5, Maradja2, Sardinia, Prisme, Assemblage and Thertou. Integration of partner organizations DTM. This DTM is available at two cell sizes : 500 m and 1000 m.

This bathymetric model is the result of compiling data and numerical models prior to 2008 in the Bay of Biscay. These datasets are available at a resolution of 500 m and 1000 m. Contours are also available for both digital terrain model (DTM). Public access granted under certain conditions.

Bathymetric model (DTM) of the North-East Atlantic, generated from conventional multibeam bathymetry data, prior to the year 2000. The grid spacing is 1000 meters. Bibliographic reference : Sibuet J.C. & al., (2004) - Carte bathymétrique de l'Atlantique nord-est et du golfe de Gascogne : implications cinématiques. Bull. Soc. géol. Fr.T. 175, n°5, pp. 429-442

Bathymetry – Lesser Antilles volcanic arc: compilation of multibeam data, grid resolution 1/16 arc minute, 2020. Restriction : the DTM largely overlaps national EEZ. The entire product cannot be freely disseminated. Processing : Since the beginning of the 1990s, the scientific exploration of the West Indian arc has provided the opportunity for regular acquisition of multibeam bathymetry. About twenty scientific cruises and valued transits feed a remarkable database and offer a wide bathymetric coverage of this geological structure. They were assembled to produce a bathymetric model of the entire region. Multibeam data were controlled and processed with the Ifremer Globe software. A similar processing flow is applied to each dataset: - Selection of relevant profiles for acoustic coverage of the study area - Automatic and manual filtering of outliers and erroneous data - Control of overlapping zones - Production of a digital terrain model. Depth layer is calculated as the average of soundings in each pixel. All DTMs are merged into a unique DTM for the area. The final product is a double-layer raster at 1/16 minute steps (~ 100 m), a bathymetric layer and data source identifier layer. Data processing is described in this specific report : "Talbot Sophie (2019). Evaluation d'une méthodologie pour la compilation de données bathymétriques." https://w3.ifremer.fr/archimer/doc/00613/72480/ Multibeam data from scientific cruises from 1992 to 2017: - ESCARTIN Javier, LE FRIANT Anne, FEUILLET Nathalie (2017) SUBSAINTES cruise, RV L'Atalante, https://doi.org/10.17600/17001000 - MARCAILLOU Boris, KLINGELHOEFER Frauke (2016) ANTITHESIS 3 cruise, RV Pourquoi pas ?, https://doi.org/10.17600/16001700 - MARCAILLOU Boris, KLINGELHOEFER Frauke (2013) ANTITHESIS LEG1 cruise, RV L'Atalante, https://doi.org/10.17600/13010070 - FEUILLET Nathalie (2009) GWADASEIS cruise, RV Le Suroît, https://doi.org/10.17600/9020020 - LEBRUN Jean Frédéric (2009) KASHALLOW 2 cruise, RV Le Suroît, https://doi.org/10.17600/9020010 - LAIGLE Mireille, LEBRUN Jean Frédéric, HIRN Alfred (2007) SISMANTILLES 2 cruise, RV L'Atalante, https://doi.org/10.17600/7010020 - PATRIAT Martin (2007) ANTIPLAC cruise, RV L'Atalante, https://doi.org/10.17600/7010010 - DEPLUS Christine, BOUDON Georges (2002) CARAVAL cruise, RV L'Atalante, https://doi.org/10.17600/2010030 - MASCLE Alain (2002) CARAMBA cruise, RV L'Atalante, https://doi.org/10.17600/2010010 - DEPLUS Christine (1998) AGUADOMAR cruise, RV L'Atalante, https://doi.org/10.17600/98010120 - LE PICHON Xavier, LALLEMANT Siegfried (1992) MANON cruise, RV L'Atalante, https://doi.org/10.17600/92000211 Valued transits Leve_smf (https://doi.org/10.17600/16010800), Lobestory (https://doi.org/10.17600/4010030), Guyaplac (https://doi.org/10.17600/3010050), TRtoufdf, transit from Toulon to Fort-de-France Dormasis (https://doi.org/10.17600/92000411), Faranaut/15N (https://doi.org/10.17600/92000311), Fara-Seadma1 (https://doi.org/10.17600/91004411), Fara Published DTM : Ryan, W.B.F., S.M. Carbotte, J.O. Coplan, S. O'Hara, A. Melkonian, R. Arko, R.A. Weissel, V. Ferrini, A. Goodwillie, F. Nitsche, J. Bonczkowski, and R. Zemsky (2009), Global Multi-Resolution Topography synthesis, Geochem. Geophys. Geosyst., 10, Q03014, doi: 10.1029/2008GC002332