AndreaBozzo/ceres-open-data-index huggingface dataset:
Lidar data acquired by drone in the Louchats forest, Gironde, France

[Lien vers la fiche source] Acquisition date : 2022/07/06 Sensor :Yellowscan, Surveyor - GNSS-inertial station: Applanix APX-15 UAV - Lidar: Velodyne VLP16 (Puck) : Wavelength: 905 nm / 300,000 pulses per second (300 kHz) / 2 echoes per pulse / Angle of view: 360 deg - Accuracy: 4cm Vector: DJI Matrice 600 Pro drone Flight conditions : - Trajectory design: double grid, distance between lines: 40 m - Speed: 5m/s - Flight height: 50m above ground level, constrained by IGN DTM at 5m spatial resolution -Flight planning software: UGCS-4.0.134 Pre-processing software : - Applanix POSPac UAV 8.4: trajectory post-processing based on the UAV's GNSS inertial unit data, using a reference GNSS base station. The correction solution for each trajectory is exported as an ASCII SBET (Smoothed Best Estimated Trajectory) file. - Yellowscan CloudStation V2106.0.0: The SBET file is integrated into the software to generate point clouds in .las format projected in RGF93/Lambert 93.
Lidar data acquired by drone at the Bordeaux observatory (Floirac)

[Lien vers la fiche source] Acquisition date : 2022/07/06 Sensor :Yellowscan, Surveyor - GNSS-inertial station: Applanix APX-15 UAV - Lidar: Velodyne VLP16 (Puck) : Wavelength: 905 nm / 300,000 pulses per second (300 kHz) / 2 echoes per pulse / Angle of view: 360 deg - Accuracy: 4cm Vector: DJI Matrice 600 Pro drone Flight conditions : - Trajectory design: double grid, distance between lines: 40 m - Speed: 5m/s - Flight height: 50m above ground level, constrained by IGN DTM at 5m spatial resolution -Flight planning software: UGCS-4.0.134 Pre-processing software : - Applanix POSPac UAV 8.4: trajectory post-processing based on the UAV's GNSS inertial unit data, using a reference GNSS base station. The correction solution for each trajectory is exported as an ASCII SBET (Smoothed Best Estimated Trajectory) file. - Yellowscan CloudStation V2106.0.0: The SBET file is integrated into the software to generate point clouds in .las format projected in RGF93/Lambert 93.
Recueil des arrêtés et décisions du Département de Loire-Atlantique

Ensemble des arrêtés et décisions prises par le Département de Loire-Atlantique depuis 2023. A noter que les délibérations depuis 2008 sont publiées de façons individualisées dans un jeu dédié. Ce jeu contient plusieurs types de documents : * des recueils généralement mensuels : * le Recueil des arrêtés et décisions ne contient plus les délibérations. mais uniquement les arrêtés et décisions à compter de juin 2022 ; * le Recueil des Actes Administratifs regroupe jusqu'en juin 2022 les délibérations de l'assemblée départementales et les décisions de la commission permanente ainsi que les actes du Président du Département à caractère réglementaire. (dépublié jusqu'à anonymisation des fichiers) * des arrêtés ou délibérations spécifiques comme : * les arrêtés délégations de signature du président ; * les arrêtés d'interim du Président. Voir aussi : * [Rapports, délibérations et procès-verbaux du Conseil départemental de Loire-Atlantique] * [Rechercher une délibération (depuis 2008)] * [Procès-verbaux du Conseil départemental de Loire-Atlantique] * [Les jeux de données des budgets primitifs du budget principal et des budgets annexe]s * [Les jeux de données des comptes administratifs du budget principal et des budgets annexes] * [Élu·e·s du Conseil départemental de Loire-Atlantique] * [Représentations des élu·e·s du Conseil départemental de Loire-Atlantique]
Enquêtes de demande-consommation de produits maraîchers en Côte d'Ivoire, en 2021

[Lien vers la fiche source] Données issus d'enquêtes administrées à 5514 ménages répartis dans les quartiers d’Abidjan, de Yamoussoukro, de Bouaké et de Korhogo, à domicile, entre juillet et septembre 2021. Les enquêtes incluent des questions visant à faire une caractérisation socio-économique des ménages. Les données ont été obtenus pour informer le choix de produits maraîchers à étudier dans le projet MARIGO.
Cadastre-napo-Nimes_occupsol

Ce jeu de données, contenant les modes d'occupation des sols, produit par Catherine Fruchart, contient les données obtenues à partir du géoréférencement du cadastre ancien de Nîmes (1825). Ce travail a été réalisé dans le cadre du programme de recherche PARCEDES sur l’histoire des parcellaires agraires (« Parcellaires agraires et dynamiques d’exploitation du sol dans la longue durée ») et financé par l’ANR.
Octroi de mer - Guadeloupe

L’octroi de mer est une imposition spécifique dans les départements d’Outre-mer : les opérations soumises à l’octroi de mer sont les importations de biens et les livraisons de biens, faites à titre onéreux, par des personnes qui y exercent des activités de production. Fichiers mis à disposition * TARIF OM 2021.xlsx * TARIF OM 2022.xlsx * TARIF OM 2023.xlsx * TARIF OM 2024.xlsx
Oak Provenances database

[Lien vers la fiche source] The Oak provenance database contains passport data of Quercus petraea and Quercus robur provenances and provenance tests established in Europe. Passport data comprise geographic data of the source stands of provenances and of the provenance tests. Additional information on seed collections in the source stands and on the plantation protocol and experimental design of provenance tests are also available. The database was constructed and populated during the FAIROAK project (1996-1999) supported by the EU (http://www.pierroton.inra.fr/Fairoak/) by partners of FAIROAK hosting oak provenance tests. It does not contain all provenance tests and provenances present in Europe. The database was upgraded within the EVOLTREE network of excellence.
Data for "Surface albedo and thermal radiation dynamics under conservation and conventional agriculture from two contrasting soils in sub-humid Zimbabwe"

[Lien vers la fiche source] These are the raw data of the paper "Surface albedo and thermal radiation dynamics under conservation and conventional agriculture from two contrasting soils in sub-humid Zimbabwe” authored by Souleymane Diop, Rémi Cardinael, Ronny Lauerwald, Morgan Ferlicoq, Christian Thierfelder, Regis Chikowo, Marc Corbeels, Eric Ceschia and submitted for publication in a peer-reviewed journal.
COOPER: flood vulnerability modeling of a cooperative wine system

[Lien vers la fiche source] The COOPER model is built to serve as a virtual laboratory for the ex-ante estimation of the impacts of a wide variety of flooding events on a cooperative wine system. The COOPER model reproduces the functioning of a cooperative wine system seen as a wine production system linking economic entities (a cooperative and wineries). The system is composed of material entities of three different natures (parcels, farm buildings, cooperative buildings) that interact with each other according to the organizational rules of the cooperative system and of each of the wineries. The production of the system depends on the performance of the material entities and on the possible disorganization propagated by the interaction between these entities. The performance of the entities varies according to their state, which can evolve "naturally" (aging of the plant material for example), according to the occurrence of floods at the place where they are located (damage or destruction), and the actions of the economic entities (repair or investment). The COOPER model makes it possible to evaluate the impacts of flooding and to trace the origin, persistence and duration of disturbances within the system. It allows to observe the state and performance of each entity at any time. It also allows to produce impacts in the economic sense (vision without double counting) or in the financial sense (vision from the point of view of a particular economic entity). Written in Netlogo v6.2.0
Biens patrimoine mondial UNESCO - Zones tampon

Cette couche de données contient la localisation des périmètres des zones tampon des biens inscrits sur la Liste du patrimoine mondial de l’UNESCO en Région wallonne. La zone tampon est une aire entourant le bien afin d’assurer un surcroit de protection à ce bien et d’en préserver la valeur universelle exceptionnelle. La zone tampon peut inclure l’environnement immédiat du bien, les perspectives visuelles importantes et d’autres aires ou attributs ayant un rôle fonctionnel important en tant que soutien apporté au bien. Lorsqu’un élément du patrimoine ou une partie du territoire est reconnu en tant que patrimoine mondial, l’article 4 du Code du Patrimoine stipule qu’il y a lieu de prendre en compte dans les autorisations d’actes et de travaux qui s’y rapportent, la protection de cette valeur universelle exceptionnelle, le plan de gestion du bien et sa zone tampon. Cette disposition s’applique sans préjudice des autres couches de protection patrimoniales déjà applicables.
Bathymetry from Les Saintes area (Lesser Antilles volcanic arc): 10m grid from the Bathysaintes cruise

[Lien vers la fiche source] Bathymetry grid, with a pixel resolution of 10 m, from bathymetry data acquired during the 2010 Bathysaintes cruise (https://doi.org/10.17600/10030020). Data were controlled and processed with the Ifremer Caraibes software.
A survey of spontaneous species and cover crop communities in an experimental banana fallow in Guadeloupe: densities and functional traits

[Lien vers la fiche source] This dataset was obtained from a vegetation survey conducted on an experimental improved fallow preceding a banana crop, in Guadeloupe, French West indies. In this experiment, 8 treatments that correspond to a combination of two practices (soil tillage and cover crop species) were tested on 5 blocks (repetitions). For each modality, one sown cover crop species (among three species tested) was combined with one soil tillage modality (among two modalities tested) to test the effect of these practices on the sponatenous vegetation. The spontaneous vegetation and the cover crops were monitored (species determination, densities/m²) on permanent quadrats (25cm x 25cm) each month for 12 months. Nine aboveground traits were measured at flowering peaks on the 12 most abundant species. Dynamic of height over the 12 months and some global descriptors of the community (biomass, cover rate) were also measured. For details on variables measurements, see the related published papers.
Replication Data for: WHOIS Right? An Analisis of WHOIS and RDAP Consistency

[Lien vers la fiche source] This data was collected during the research work that led to the publication of the article "WHOIS Right? An Analysis of WHOIS and RDAP Consistency", published at Passive and Active Measurements 2024. To compare the consistency of registration data accross the WHOIS and RDAP data sources, we selected a random subset of 55M domain names that had both WHOIS and RDAP entries, we collected and parsed their multiple entries. This dataset contains the collected parsed data of this study: 156M parsed WHOIS and RDAP entries, across 55M domains.
Têtes de bassins versants du SAGE Estuaire de la Loire

Les têtes de bassins versants sont les zones où les cours d'eau prennent naissance. Elles représentent la surface drainée de la source de chacun des petits tributaires jusqu'à constituer ou rejoindre l'axe principal d'un cours d'eau (rang Strahler supérieur ou égal à 3).
Supplementary information for Colinet et al. 2023: Convergent origin and accelerated evolution of vesicle-associated RhoGAP proteins in two unrelated parasitoid wasps

[Lien vers la fiche source] Supplementary information for the manuscript entitled Convergent origin and accelerated evolution of vesicle-associated RhoGAP proteins in two unrelated parasitoid wasps by Colinet et al. 2023.
OrthoImage - 2018

Orthophotographie couleur haute résolution (5 cm) issue de prises de vues aériennes réalisées à l'été 2018. Techniquement, il s'agit d'une OrthoImage vraie réalisée dans le cadre de la production du Photomaillage 3D. Elle est directement issue du photomaillage 3D et correspond à une projection orthogonale de celui-ci sur un plan horizontal. Le résultat est comparable à une orthophotographie vraie 2D (absence de dévers), mais l’ortho-image contient des artefacts visuels liés au mode de production (ombres mixées, absence d’éléments de petites tailles comme le mobilier urbain, présence partielle ou multiple d’éléments mobiles (véhicules)). Ces artéfacts ne constituent cependant pas un frein à l’utilisation de l’ortho-image comme image2D de référence du territoire. Les usages possibles sont identiques à ceux d’une orthophotographie classique. [Lien de téléchargement] de l’orthoimage (Format ECW – 39 Go) Ces données ont été produites avec le soutien du FEDER (Fonds Européen de Développement Régional). Mention obligatoire sur tout support de diffusion : Ville et Eurométropole de Strasbourg - Données produites avec le soutien du FEDER Les logos de l'Eurométropole de Strasbourg et de l'Union Européenne doivent figurer sur tout support de diffusion. Lien vers [les métadonnées]
Onshore fishing activities assessment in Mayotte's Marine Protected Area

[Lien vers la fiche source] These data were collected by ULM flight during low tides and different environmental conditions (day of the week, sea level during low tide, weather, time of the day, month, etc.). Assessment was done by photo-analysis. Fishermen were divided in different categories according to gear and targeted species : onshore gathering (targets octopus and shellfish), swimming fishers (with or without boat - illegal inside the lagoon), spearfishing (illegal inside the lagoon), netfishing (targets demersal reef associated species, illegal if not professional and performed on healthy coral), traditional netfishing (targets small pelagic species), angling (targets demersal reef associated species).
Mooring data at Yermak Pass from September 2017 to July 2020 : raw and 50 hr high pass filtered data

[Lien vers la fiche source] The mooring was deployed on 15 September 2017 from Norwegian Research Vessel Lance at 80.6°N and 7.26°E (depth of 730 m) in the Yermak Pass over the Yermak Plateau north of Svalbard. It comprised 3 instruments: an upward-looking RDI 75kHz, a Long Ranger Acoustic Doppler Current Profiler (ADCP) at 340 m with 16 m vertical resolution (25 bins of 16 m each) and a 2-hour sampling time; a Seabird SBE37 measuring temperature, salinity and pressure at 348 m with 10-minute sampling time; and an Aquadopp current meter at 645 m with a 2-hour sampling time. The mooring was retrieved on the 19 July 2020 by Norwegian Icebreaker K.V. Svalbard. The present dataset features: The ADCP 50-hour high pass filtered velocities and the Aquadopp 50-hour high pass filtered velocities.
Arctic Makarov Basin : IAOOS14, IAOOS15 and IAOOS25 ocean CTD-DO profiles in 2015 and 2017

[Lien vers la fiche source] IAOOS14, IAOOS15 and IAOOS25 were deployed from the Korean Icebreaker R/V Araon during cruises in the northern Chukchi Sea. IAOOS14 and IAOOS15 were deployed 300 m apart on the same floe on 12 August 2015 in the Makarov Basin (80.8°N;173°E) and they drifted together remaining always less than 6 km apart. IAOOS25 was deployed on 15 August 2017 south-west Mendeleev Ridge (77.7°N;180°E) and drifted westward to the continental slope of the East Siberian Sea. IAOOS14 and IAOOS25 stopped transmitting on 9 October 2015 and 19 November 2017 respectively, likely due to the loss of their profilers while crossing relatively shallow bathymetry. IAOOS15 dataset ends in 15 October 2015. Ocean profilers were PROVOR SPI (from French manufacturer NKE) equipped with a Seabird SBE41 CTD (Conductivity, Temperature, Depth) and a dissolved oxygen (DO) Aandera 4330 optode. The profilers were set to perform two upward profiles a day from 800 m (IAOOS 14), 300 m (IAOOS 15) and 420 m (IAOOS 25), upward starting at approximately 6 am and 6 pm. The present dataset is composed of CTD-DO data from IAOOS 14 and 15, and CTD data from IAOOS 25 in the Makarov Basin, corrected from salinity errors and interpolated vertically every 0.5 m.
Arctic Western Eurasian Basin: IAOOS 23 physical and biogeochemical profiles in 2017

[Lien vers la fiche source] In April 2017, two Ice Atmosphere Arctic Ocean Observing System platforms (IAOOS 23 and IAOOS 24) were deployed near the North Pole. Over the next 8 months, they meandered southwards with the ice in the Transpolar Drift, collecting measurements in the upper 250 m of Amundsen Basin, Nansen Basin and Fram Strait. The ocean profilers are PROVOR SPI (from French manufacturer NKE), which includes a Seabird SBE41 CTD (Conductivity, Temperature, Depth) and a dissolved oxygen (DO) Aandera 4330 optode. IAOOS 23 also featured a bio-optics sensor suite and a submersible ultraviolet nitrate analyzer (SUNA, Satlantic-Seabird Inc.). The bio-optics sensor suite (called Pack Rem A) combines a three-optical-sensor instrument (ECO Triplet, WET Labs Inc.) and a multispectral radiometer (OCR-504, Satlantic Inc.). The present dataset is composed of chlorophyll-a fluorescence, backscatter, irradiances (at 412, 490 and 555 nm), photosynthetically active radiation (PAR), nitrate and colored-dissolved organic matter data from the IAOOS 23 platform, as well as composites of absolute salinity, conservative temperature and apparent oxygen utilization data from both profilers. The profilers were set to perform two upward profiles a day from 250 m starting at approximately 6 am and 6 pm. In this dataset, chlorophyll-a, PAR and irradiances were corrected with a shift to set dark values to zero. Nitrate was interpolated vertically every 5 m, and all other parameters were interpolated vertically every 0.5 m.
Geochemical data on otoliths of chaetodon speculum from New Caledonia

[Lien vers la fiche source] Coral reefs are one of the most diverse ecosystems on Earth. They are currently exposed to increasing levels of anthropogenic perturbations. Several recent reviews point to the lack of good indicators for these perturbations especially to monitor their effects on fish populations or fish assemblages. The SW lagoon of New Caledonia is an ideal location to test indicator species in this context as contrasting sites are present within a small geographical range. This study analysed fish from four sites, one with heavy industrial pollution, another dominated by domestic waste, a third with historic mining activities, and the fourth as a control. The butterfly fish, Chaetodon speculum, was chosen to determine C. speculum’s potential as an indicator species due to its link to coral, its sedentary behaviour and its wide geographical distribution. The size distribution, growth rate, age distribution and whole otolith composition were analysed at each site. Age and mean growth rate were analysed from daily increments of the otoliths. The concentrations of eight elements (Li, Mg, Co, Cu, Rb, Sr, and Ba) were measured by ICP-MS in the otoliths. The sites under anthropogenic impact were distinct from the control site by fish size frequencies, age distributions, and the chemical content of their otoliths. The chemical elements Mg, Co, Cu, and Rb showed differences amongst sites. Fish belonging to the sites furthest from Noume´a could be discriminated in nearly 80% of samples or 60% of the cases when otolith weight or fish age respectively were taken into account. Ni concentrations of the otoliths were also higher in the bays where water concentrations of this element were known to be higher, but these differences were no longer significant once corrected for otolith weight.
Improved accuracy and spatial resolution for bio-logging-derived chlorophyll a fluorescence measurements in the Southern Ocean

[Lien vers la fiche source] The ocean’s meso- and submeso-scales (1-100 km, days to weeks) host features like filaments and eddies that have a key structuring effect on phytoplankton distribution, but that due to their ephemeral nature, are challenging to observe. This problem is exacerbated in regions with heavy cloud coverage and/or difficult access like the Southern Ocean, where observations of phytoplankton distribution by satellite are sparse, manned campaigns costly, and automated devices limited by power consumption. Here, we address this issue by considering high-resolution in-situ data from 18 bio-logging devices deployed on southern elephant seals (Mirounga leonina) in the Kerguelen Islands between 2018 and 2020. These devices have submesoscale-resolving capabilities of light profiles due to the high spatio-temporal frequency of the animals’ dives (on average 1.1 +-0.6 km between consecutive dives, up to 60 dives per day), but observations of fluorescence are much coarser due to power constraints. Furthermore, the chlorophyll a concentrations derived from the (uncalibrated) bio-logging devices’ fluorescence sensors lack a common benchmark to properly qualify the data and allow comparisons of observations. By proposing a method based on functional data analysis, we show that a reliable predictor of chlorophyll a concentration can be constructed from light profiles (14 686 in our study) and matchups with satellite ocean-color data, thus enabling effective (1) homogenization then calibration of the bio-logging devices’ fluorescence data and (2) filling of the spatial gaps in coarse-grained fluorescence sampling. The developed method improves the spatial resolution of the chlorophyll a field description from ~30 km to ~12 km. These results open the way to empirical study of the coupling between physical forcing and biological response at submesoscale in the Southern Ocean, especially useful in the context of upcoming high-resolution ocean-circulation satellite missions like SWOT.
50h low pass filtered Mooring data at Yermak Pass from September 2017 to July 2020

[Lien vers la fiche source] The mooring was deployed on 15 September 2017 from Norwegian Research Vessel Lance at 80.6°N and 7.26°E (depth of 730 m) in the Yermak Pass over the Yermak Plateau north of Svalbard. It comprised 3 instruments: an upward-looking RDI 75kHz, a Long Ranger Acoustic Doppler Current Profiler (ADCP) at 340 m with 16 m vertical resolution (25 bins of 16 m each) and a 2-hour sampling time; a Seabird SBE37 measuring temperature, salinity and pressure at 348 m with 10-minute sampling time; and an Aquadopp current meter at 645 m with a 2-hour sampling time. The mooring was retrieved on the 19 July 2020 by Norwegian Icebreaker K.V. Svalbard. The present dataset features: (i) the ADCP 50-hour smoothed daily velocities, conservative temperature and pressure time series interpolated every 10 meters within the 20-330m layer, (ii) the Aquadopp 50-hour smoothed daily velocities and pressure time series at 645 m; and (iii) the SBE37 50-hour smoothed daily conservative temperature, absolute salinity and pressure time series at 348 m.