AndreaBozzo/ceres-open-data-index huggingface dataset:
SeaDataNet geographic co-ordinate reference frames

The main objective of the MOOSE-GE cruises is to observe the annual evolution of the Northwestern Mediterranean Sea in the context of the climate change and anthropogenic pressure in order to be able to detect and identify long-term environmental trend and anomalies of the marine ecosystem. The annual cruise focuses on moorings maintenance and hydrology, biogeochemistry and biology monitoring of the Northwestern Mediterranean basin. It aims to follow variability of water masses properties (LIW and WMDW) and biogeochemical and biological content related to these water masses.
BILLION 36  cruise was part of this cruise too.
SeaDataNet geographic co-ordinate reference frames

The objective of cruise DY039 was to service the moorings of the RAPID 26°N project that are deployed to monitor the Atlantic Meridional Overturning Circulation. For each mooring instruments were recovered, data were downloaded and instruments were redeployed. A number of CTDs were made to calibrate the instruments from the moorings. 

In addition to the standard instruments used in previous years on the RAPID array, biogeochemical instruments were deployed for the ABC Fluxes project, along with some additional temperature sensors and ADCPs for the MerMeed project.

During passage from Southampton to Tenerife trial CTDs were completed in international waters. After a short port call in Santa Cruz de Tenerife, departing on the 26th October work commenced on the eastern boundary sub-array comprising of moorings EBH4, EBH4L, EBH3, EBH2, EBH1, EBH1L, EBHi, EB1 and EB1L. A lander was deployed alongside EBHi to provide delayed-mode data telemetry through timed data pod release.

Work on the MAR sub-array commenced on 7th November at mooring MAR3. The other moorings in this sub-array (MAR3L, MAR1, MAR1L, MAR2 and MAR0) were all completed by 12th November. The NOG mooring was also recovered and redeployed as part of the MAR sub-array servicing. 

Mooring WB6 was serviced on 19th November before transiting to Nassau for customs clearance. The remaining western boundary sub-array moorings (WBADCP, WBAL, WB1, WB2, WB2L, WBH2, WB4 and WB4L) were serviced between the 22nd November and the 30th November before docking in Nassau on the 1st December.
SeaDataNet geographic co-ordinate reference frames

<p>The WESTMEDFLUX-2 oceanographic cruise is part of the project that studies the presence of thermal anomalies in the ocean-continent transitions of the Western Mediterranean. The proposed cruise follows WESTMEDFLUX that took place in 2016 and that resulted in mapping regional trends of thermicity in in the Gulf of Lion, offshore Baleares and Sardinia. It also pointed out to the existence of several local heat flow anomalies in particular on the South Balearic slope and deep basin. In the deep oceanic basin, strong anomalies seem to be merely associated to salt diapiric structures, but on the rifted continent and transition zone, other heat sink and sources are suggested (e.g., bottom water currents, slope instabilities and focused fluid migrations). In order to better understand the source of these anomalies and the link with the crustal nature and structuring of the margin, we propose on the South-Balearic margin additional close-spaced heat flow measurement, sediment coring and dredging sites. Sediment cores will be used for turbidite and contourite studies and for geochemical analysis of pore fluids. The dredging operations aim an estimation of age and nature of volcanic rock material from sea mounts.</p>
Mojones de los montes públicos deslindados de la Comunidad Autónoma de Aragón

Mojones que delimitan los montes públicos deslindados de la Comunidad Autónoma de Aragón.
Una vez firme en vía administrativa la orden resolutoria del deslinde, se procede al amojonamiento definitivo. Consiste en marcar sobre el terreno, con carácter permanente, los límites definidos en el deslinde mediante hitos o mojones.
Ortofotografía de 50cm de la Comunidad Autónoma del País Vasco. Año 1984/85

La ortoimagen de la Comunidad Autónoma del País Vasco de 1984/85 ha sido generada a partir del Vuelo Fotogramétrico Nacional de los años 1980-1986, de escala 1:30.000, y propiedad del Instituto Geográfico Nacional. El documento final, en blanco y  negro, tiene una resolución espacial de 50cm y está georreferenciado en ETRS89, proyección UTM-30N.
SeaDataNet geographic co-ordinate reference frames

The research programme of Belgica campaign 2014/14 aimed at assessing the different biogeochemical processes controlling the carbon and nitrogen cycles in oligotrophic N.E. Atlantic waters. These cycles are essential components of the biological Carbon Pump' by which part of atmospheric carbon dioxide is transferred to the ocean's interior. Our approach is based on the use of dual nitrate isotope measurements (natural abundance and enrichment experiments) to disentangle these various nitrogen processes in the marine environment, and in particular the process of diazotrophy by which atmospheric N2 is introduced into the oceanic fixed nitrogen reservoir. This input of new' nitrogen should stand in balance with the denitrification process by which nitrogen is lost from the oceanic system. There are indications that the intensity as well as the geographical distribution of diazotrophic activity has been underestimated till date, in general. It is of particular interest to better document diazotrophic activity at latitudes of 38°N and northward, areas for which only few data are available. During the cruise we studied the different biogeochemical processes acting on the marine N-cycle, including N2 fixation, nitrate (NO3-), ammonium (NH4+) and nitrite (NO2-) uptake, nitrification, along a north-south section through the Gulf of Biscaye to Cape Finisterre and further south in open ocean waters along the Iberian peninsula till about 38°30'N. In addition, the effect of iron limitation on the nitrogen fixation and the nitrification processes was investigated.
SeaDataNet geographic co-ordinate reference frames

<p>The Protevs Swot 2018 campaign aimed to explore the South Balearic zone in early spring to observe the small scales of the oceanic mixed layer using high-resolution sampling devices.</p>

<p>The area was chosen because it was positioned below the SWOT satellite's planned swath in its validation/calibration period. In this sense, it is a precursor experiment of experiments for the year 2022 and as such exploratory of the scales that will be observable by this newly designed altimetry satellite.</p>

<p>A particular focus was placed on an anticyclonic structure in the southern Balearic Islands that is systematically detectable by altimetry but which appears to be an artifact.</p>

<p>These samplings were combined with fine analysis of the surface content of small phytoplankton by flow cytometry to study the shaping of the marine landscape by frontal physical processes.</p>

<p>&nbsp;</p>
SeaDataNet geographic co-ordinate reference frames

Studying the Messinian Salinity Crisis on the Balearic promontory and using its markers to assess post-crisis vertical movement and the reactivation of the region. 
1) Fine-scale continuous mapping of evaporites from land to the deep basin in order to answer the following question: What is the spatial-temporal variability of evaporites of the Balearic Promontory (evaporites on land, very thin or thick evaporates at sea)? 
2) Using the Messinian as a marker of syn- and post-MSC deformations; isolating recent movements from previous deformations and quantifying them in order to reproduce the paleo-bathymetry and paleo-connections during the crisis. Were the evaporites in shallow basins continuous with evaporites in deeper basins before the recent deformations? 
The related project is 'Action Marges', Mediterranean study site.
SeaDataNet geographic co-ordinate reference frames

The area in between the Audierne and St. Nazaire canyons (Gascogne) along the Armorican margin was one of the areas where the "massifs coralliens" were described for the very first time. Within the framework of the HERMES (EC FP6), MiCROSYSTEMS (ESF) and GeNeSis (FWO) projects, this area will be surveyed using multibeam and high resolution seismics during LEG 1. Based on this site survey, the ROV Genesis will be deployed to carry out detailed mapping of these deep-water "hot-spots". Also the hydrography and sediment dynamics of this area will be studied with respect to the steering of the present ecosystems. LEG 2 will focus on the Galicia bank. This location has been assigned as reference area within the ESF project BIOFUN. In addition to a bathymetric and seismic surveying, also biological sampling and experiments are planned here.
SeaDataNet geographic co-ordinate reference frames

The series of PELMED cruises began in 1993.  Their objective is to assess small pelagic resources in the Gulf of Lion, using the echo-integration method and trawling to identify the detections observed. Until 2007, each cruise consisted in systematically prospecting from Port-Vendres to Marseille, along 9 legs set 12 nautical miles apart, perpendicular to the coast, in daytime (6 am to 9 pm), along the entire width of the continental shelf. Acquisition along legs for acoustic prospection covered 440 nautical miles and the catches from trawling to identify the structures encountered led to a complete analysis: number and weight by species, size sampling, otolith samples taken in order to construct size-age keys for sardines, anchovies and hake, updating of biological parameters.
Piquetes de los montes públicos deslindados de la Comunidad Autónoma de Aragón

Piquetes que delimitan los montes públicos deslindados de la Comunidad Autónoma de Aragón.
  Tal y como establece la Ley 15/2006 de Montes de Aragón, el deslinde es el acto administrativo por el que se delimita el monte de titularidad pública y se declara con carácter definitivo su estado posesorio, a reserva de lo que pudiera resultar de un juicio declarativo de la propiedad. En el apeo se colocan hitos o mojones provisionales (piquetes) realizando el correspondiente levantamiento topográfico.
SeaDataNet geographic co-ordinate reference frames

This project was a hydrographic section at latitude 24°N, with physical, chemical and biological measurements. The section was a complete section from continent to continent from North America (Caribbean) to Africa (off the coast of the Western Sahara). The section started and ended in 200 metres water depth, at the edge of the continental shelf.

This was a contribution to the international CLIVAR/Carbon repeat hydrography program (http://ioc3.unesco.org/ioccp/Hydrography/New_GlobalMap.html). Climate change will be studied by comparing the new data with historical measurements. Ocean heat transport plays a major role in the coupled ocean-atmosphere climate system. We will study the present-day circulation by calculating the heat and freshwater transported by the ocean across the 24°N latitude. The ocean western boundary current system, in this case the Gulf Stream flowing through the Florida Strait, plays a crucial role in the oceanic heat transport. Therefore a crossing of the Florida Strait will be carried out to establish the status of this important ocean feature. All data arising from the cruise will be lodged and made available via the British Oceanographic Data Centre (BODC), UK.
SeaDataNet geographic co-ordinate reference frames

The cruise is a component of RAPID-WATCH, whose objectives are: to deliver a decade-long time series of calibrated and quality-controlled measurements of the Atlantic MOC from the RAPID-WATCH array and; to exploit the data from the RAPID-WATCH array and elsewhere to determine and interpret recent changes in the Atlantic MOC, assess the risk of rapid climate change, and investigate the potential for predictions of the MOC and its impacts on climate.

Objectives of this cruise: to recover, calibrate and redeploy moorings from the eastern boundary and mid-Atlantic ridge subarrays of the 26.5N line of RAPID moorings.
SeaDataNet geographic co-ordinate reference frames

Campaign GENESIS 2 "Pen Duick/Melilla", the second of three ROV campaigns, will focus on "Pen Duick Escarpment" in the Gulf of Cadiz or on the recently discovered "Melilla mounds" in the South-East Alboran Sea (Mediterranean Sea). The final choice of the study area will depend on the results of the TTR17 cruise with R/V Logachev (June-July 2008) and the R/V Marion Dufresne cruise (June 2008). One of these study areas will be surveyed using multibeam, side-scan sonar and high resolution seismics. Based on this site survey, the ROV Genesis will be deployed to carry out detailed mapping. Also the hydrography and sediment dynamics of the area will be studied with respect to the steering of the present ecosystems. GENESIS 2 takes place in the framework of the European projects HERMES (EC FP6), MiCROSYSTEMS (ESF) and HERMIONE (EC FP7).
Servicio WMS (Web Map Service) Aguas afectadas por nitratos (RD 47/2022). 2022

El Servicio WMS (Web Map Service) denominado "Aguas afectadas por nitratos (RD 47/2022). 2022" permite la visualización y consulta del conjunto de datos que representan Aguas afectadas por la contaminación de nitratos procedentes de la actividad agraria. Es información básica para la declaración de Zonas Vulnerables conforme al Real Decreto 47/2022, de 18 de enero, sobre protección de las aguas contra la contaminación difusa producida por los nitratos procedentes de fuentes agrarias y a la Directiva 91/676/CEE, relativa a la protección de las aguas contra la contaminación producida por nitratos procedentes de fuentes agrarias ("Directiva de Nitratos").  
La identificación de estas aguas parte de la información recogida en el informe de situación notificado a la Comisión europea sobre la aplicación de la directiva en el cuatrienio 2016-2019.  Esta información plasma sin modificación alguna, la información sobre calidad de las aguas notificada nitratos y, en especial, por los de origen agrario, así como de las aguas que podrían verse afectadas por dicha contaminación si no se toman las medidas oportunas. 
				La URL del servicio es la siguiente: https://wms.mapama.gob.es/sig/Agua/Nitratos/AguasAfectadas
                Los sistemas de referencia que ofrece este servicio son:
				- Para coordenadas geográficas: CRS: 84, EPSG:4230 (ED50), EPSG:4326 (WGS 84), EPSG:4258 (ETRS 89).
				- Para coordenadas U.T.M: EPSG:32627 (WGS 84 / UTM zone 27N) EPSG:32628 (WGS 84 / UTM zone 28N), EPSG:32629 (WGS 84 / UTM zone 29N), EPSG:32630 (WGS 84 / UTM zone 30N), EPSG:32631 (WGS 84 / UTM zone 31N), EPSG:25828 (ETRS 89 / UTM zone 28N), EPSG:25829 (ETRS 89 / UTM zone 29N), EPSG:25830 (ETRS 89 / UTM zone 30N), EPSG:25831 (ETRS 89 / UTM zone 31N), EPSG:23028 (ED50 / UTM zone 28N), EPSG:23029 (ED50 / UTM zone 29N), EPSG:23030 (ED50 / UTM zone 30N), EPSG:23031 (ED50 / UTM zone 31N), EPSG 3857 (WGS84/ Web Mercator)
SeaDataNet geographic co-ordinate reference frames

<p style="text-align:justify">The main scientific objectives of the cruises are threefold:</p>

<ul>
	<li style="text-align: justify;">to asses the large scale circulation in the Western Basin, evaluating the water masses and the fluxes at different key point in the basin (The North Current, The East and West Corsica currents, the Balearic front, Algerian Basin). The final goal was numerical modelling assessment.</li>
	<li style="text-align: justify;">to identify and follow peculiar mesoscale structures such as surface eddies, modal weddies, submesoscale coherent vortices (SCV) meanders or filaments and explore the signature on the sea surface height (altimetry) and the acoustic impact (sound propagation).</li>
	<li style="text-align: justify;">to observe and interpret the submesoscale dynamics such ageostrophic stirring, symmetric instabilities, mixed layer instabilities, subduction and convection.</li>
</ul>

<p style="text-align:justify">The <strong>Protevs2015_leg1&nbsp; </strong>campaign took place from the 8th to 28th of January 2015 on board of the RV <em>Pourquoi Pas?</em> in the north western mediterranean basin. It is focused on physical aspects (hydrology and dynamics). The main objective was the dynamics of the North current from its roots in the Ligurian Sea downstream to the Gulf of Lion. The surveys try to catch not only the meso-scale features but also the submesoscale associated to the the northern current or at least in its vicinity.</p>

<p style="text-align:justify">&nbsp;</p>

<p style="text-align:justify">&nbsp;</p>
SeaDataNet geographic co-ordinate reference frames

Overall objectives in the EU GO project are to assess the promising potential of seismic imaging for physical oceanography, in view of its combination of fine resolution and coverage unmatched by conventional oceanographic measurements. D318 was to provide the means of assessment by obtaining a unique comprehensive  oceanographic and seismic dataset at the same time and place. 

Specific objectives for R.R.S. Discovery cruise 318b were to 
(i) recover four ADCP moorings, three adjacent temperature-logger moorings and STABLE, from 750-1000m depth east of Portimao Canyon
(ii) perform deep water CTD casts 
(iii) carry out seismic sections using the NMF supplied Bolt airgun and streamer, accompanied by regular XBT and less frequent XCTD casts, iv) work with MV Poseidon to test novel seismic data acquistion strategies. 

In addition underway data was logged including ship-borne ADCP, surface temperature and salinity, meteorology, gravity and magnetics (to test new NERC magnetometers).
SeaDataNet geographic co-ordinate reference frames

The purpose of the cruise was the refurbishment of an array of moorings on the mid-Atlantic Ridge and off the Moroccan Coast at nominal latitude of 26.5°N. The moorings are part of an Atlantic-wide mooring array for monitoring the Atlantic Meridional Overturning Circulation and Heat Flux. The array is a joint UK/US programme and is known as the RAPID-WATCH/MOCHA array. 

The RAPID transatlantic array consists of 24 moorings of which 21 are maintained by the UK, and 20 bottom landers of which 16 are maintained by the UK. The moorings are primarily instrumented with self logging instruments measuring conductivity, temperature and pressure. Direct measurements of currents are made in the shallow and deep western boundary currents. The bottom landers are instrumented with bottom pressure recorders (also known as tide gauges), measuring the weight of water above the instrument. 

A sediment trap mooring NOGST was also recovered and redeployed for the Ocean Biogeochemistry and Ecosystems Group at the NOCS. CTD stations were conducted at convenient times throughout the cruise for purposes of providing pre and post deployment calibrations for mooring instrumentation and for testing mooring releases prior to deployment. Shipboard underway measurements were systematically logged, processed and calibrated, including: waves (spectra of energy and significant wave height), surface meteorology (air pressure, temperature, wind speed and direction and radiation (total incident and photosynthetically active), 6m depth sea temperatures and salinities, water depth, navigation (differential GPS measurements feeding two independent and different receivers, heading, pitch and roll from a four antenna Ashtec ADU5 receiver, gyro heading and ships speed relative to the water using an electromagnetic log). Water velocity profiles from 15m to approximately 500m depth were obtained using a ship mounted 75 kHz acoustic Doppler current profiler. Seawater samples from CTD stations and of the sea-surface were obtained for calibration and analysed on a salinometer referencing these samples against standard sea water. For velocity data (wind and currents) measured relative to the ship considerable effort was made to obtain the best possible earth-referenced velocities. 

Four APEX Argo floats supplied by the Met Office were deployed at pre-assigned locations, filling gaps in the network.
SeaDataNet geographic co-ordinate reference frames

Optical (Rrs) and hydrological measurements to determine and quantify particles in suspension and dissolved organic matter at the surface of the water using satellite images. The measurements taken along the Basque country coast are used to validate the algorithms developed using data from the BATEL-1 mission. An additional objective is to supply in-situ optical and hydrological data for the doctoral theses of C. Petus and S.Novoa. The oceanographic mission took place in 2 parts due to a mechanical incident aboard RV Côte de la Manche. The cruise falls under the inter-régional Aquitaine-Euskadi (OOSSEA) programme, CIFRE contract.
WGS 84 / UTM zone 30N

Se muestran a continuación los datos de los fotogramas que se han empleado para la elaboración del mosaico.
                                      Año: 2007 
                                      Vuelo: T.M. Madrid
                                      Fecha:  Julio agosto 2007
                                      Escala: 5.000
                                      Formato: 23x23
                                      Superficie volada: 77.956 has
                                      Hoja: No ind.
                                      Imagen: MADRID_2007_10cm_OF_mos.tif
                                      Volado por: TRES CANTOS, S.A.
                                      Cámara: VEXCEL ULTRACAM D#0048
                                      Focal: 105.200 mm
                                      Película: Color
                                      Incidencia detectada: Manchado(químico, huellas, motas)  Arañado(casual, revelado)  Otros (Rayas errores escaneo) 
                                      Censurado: Con censura
                                      Caja: No ind.
                                      Ref.: 2007
          El vuelo de 10cm esta realizado por dos empresas:
          - TASA que ha realizado las pasadas 57, 59, 61, 63, 65, 67, 69, 71, 73, 75, 148, 149, 970, 971, 972, 973, 974, 975, 976 y 977.
          - SPASA el resto de las pasadas.
Ortofotografía de la Comunidad Autónoma del País Vasco. Años 1977/78

Ortoimagen de la Comunidad Autónoma del País Vasco en los años 1977-1978, generada a partir del vuelo fotogramétrico en blanco y negro de ámbito nacional realizado por encargo de los Ministerios de Agricultura, Defensa, Hacienda y del Instituto Geográfico y Catastral (actual Instituto Geográfico Nacional). Fotogramas en blanco y negro a escala 1:18.000. Tamaño de pixel (GSD) entre 45 cm y 27 cm, según zonas.
WGS 84 / UTM zone 30N

Se muestran a continuación los datos de los fotogramas que se han empleado para la elaboración del mosaico.
                                        Año: 2005 
                                        Vuelo: T.M. Madrid
                                        Fecha:  Julio2005
                                        Escala: 5.000
                                        Formato: 23x23
                                        Superficie volada: 77.956 has
                                        Hoja: No ind.
                                        Imagen: MADRID_2005_10cm_OF_mos.tif
                                        Volado por: CECAF
                                        Cámara: WILD RC-10
                                        Focal: 305.38 mm
                                        Película: Color
                                        Incidencia detectada: Manchado(químico, huellas, motas)  Arañado(casual, revelado)  Otros (Rayas errores escaneo) 
                                        Censurado: Con censura
                                        Caja: No ind.
                                        Ref.: 2005
                                        Observaciones: Sin obs.
                                        Fecha escaneado: N/D