| _version_ | 1867168498704187392 |
|---|---|
| author | Arístegui, Javier Montero, María Fernanda Hernández-Hernández, Nauzet Alonso-González, Iván J Baltar, Federico Calleja, Maria Ll Duarte, Carlos Manuel |
| author_facet | Arístegui, Javier Montero, María Fernanda Hernández-Hernández, Nauzet Alonso-González, Iván J Baltar, Federico Calleja, Maria Ll Duarte, Carlos Manuel |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The present data were collected from two cruises that took place in the Canary Current from September 10 to October 1, 2002 (COCA I) and from May 21 to June 7, 2003 (COCA II). The study was conducted along two zonal sections (21ºN and 26ºN) extending from the coastal upwelling to the open ocean at 26ºW, and focused on the epipelagic (0-200 m) and mesopelagic (200-1000 m) zones. The cruises consisted of a total of 31 hydrographic stations and 10 biogeochemical stations, half of them along each section, which were roughly equidistant. At each hydrographic station, conductivity, temperature and pressure were recorded by means of a Seabird 911+ CTD, mounted on a General Oceanics rosette sampler equipped with 24 10L-Niskin bottles. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_930889 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Physical oceanography during Hespérides cruises COCA-1 and COCA-2 Arístegui, Javier Montero, María Fernanda Hernández-Hernández, Nauzet Alonso-González, Iván J Baltar, Federico Calleja, Maria Ll Duarte, Carlos Manuel 29HE20020910; 29HE20030520; Calculated; Canary Current; Canary Current upwelling region; COCA-1; COCA-1_02-3; COCA-1_04-3; COCA-1_06-3; COCA-1_08-3; COCA-1_10-3; COCA-1_12-3; COCA-1_14-3; COCA-1_16-3; COCA-1_18-3; COCA-1_20-3; COCA-1_22-3; COCA-1_26-3; COCA-1_29-3; COCA-1_32-3; COCA-1_42-3; COCA-1_44-3; COCA-1_46-3; COCA-1_48-3; COCA-1_50-3; COCA-1_52-3; COCA-1_54-3; COCA-1_56-3; COCA-1_58-3; COCA-1_60-3; COCA-1_63-3; COCA-1_66-3; COCA-2; COCA-2_02-3; COCA-2_04-3; COCA-2_06-3; COCA-2_08-3; COCA-2_10-3; COCA-2_12-3; COCA-2_14-3; COCA-2_16-3; COCA-2_18-3; COCA-2_20-3; COCA-2_22-3; COCA-2_24-3; COCA-2_26-3; COCA-2_29-3; COCA-2_32-3; COCA-2_42-3; COCA-2_44-3; COCA-2_46-3; COCA-2_48-3; COCA-2_50-3; COCA-2_52-3; COCA-2_54-3; COCA-2_56-3; COCA-2_58-3; COCA-2_60-3; COCA-2_63-3; COCA-2_66-3; Constraining organic carbon fluxes in an eastern boundary upwelling ecosystem (NW Africa): the role of non-sinking carbon in the context of the biological pump; CTD; CTD, Sea-Bird SBE 911plus; Density, sigma-theta (0); DEPTH, water; Dissolved Organic Carbon; ETS activity; Event label; FLUXES; Hespérides; Latitude of event; Longitude of event; mesopelagic respiration variability; Pressure, water; Salinity; Station label; SUMMER; suspended and sinking particulate organic carbon; Sustainable Management of Mesopelagic Resources; Temperature, water; Temperature, water, potential The present data were collected from two cruises that took place in the Canary Current from September 10 to October 1, 2002 (COCA I) and from May 21 to June 7, 2003 (COCA II). The study was conducted along two zonal sections (21ºN and 26ºN) extending from the coastal upwelling to the open ocean at 26ºW, and focused on the epipelagic (0-200 m) and mesopelagic (200-1000 m) zones. The cruises consisted of a total of 31 hydrographic stations and 10 biogeochemical stations, half of them along each section, which were roughly equidistant. At each hydrographic station, conductivity, temperature and pressure were recorded by means of a Seabird 911+ CTD, mounted on a General Oceanics rosette sampler equipped with 24 10L-Niskin bottles. |
| title | Physical oceanography during Hespérides cruises COCA-1 and COCA-2 |
| topic | 29HE20020910; 29HE20030520; Calculated; Canary Current; Canary Current upwelling region; COCA-1; COCA-1_02-3; COCA-1_04-3; COCA-1_06-3; COCA-1_08-3; COCA-1_10-3; COCA-1_12-3; COCA-1_14-3; COCA-1_16-3; COCA-1_18-3; COCA-1_20-3; COCA-1_22-3; COCA-1_26-3; COCA-1_29-3; COCA-1_32-3; COCA-1_42-3; COCA-1_44-3; COCA-1_46-3; COCA-1_48-3; COCA-1_50-3; COCA-1_52-3; COCA-1_54-3; COCA-1_56-3; COCA-1_58-3; COCA-1_60-3; COCA-1_63-3; COCA-1_66-3; COCA-2; COCA-2_02-3; COCA-2_04-3; COCA-2_06-3; COCA-2_08-3; COCA-2_10-3; COCA-2_12-3; COCA-2_14-3; COCA-2_16-3; COCA-2_18-3; COCA-2_20-3; COCA-2_22-3; COCA-2_24-3; COCA-2_26-3; COCA-2_29-3; COCA-2_32-3; COCA-2_42-3; COCA-2_44-3; COCA-2_46-3; COCA-2_48-3; COCA-2_50-3; COCA-2_52-3; COCA-2_54-3; COCA-2_56-3; COCA-2_58-3; COCA-2_60-3; COCA-2_63-3; COCA-2_66-3; Constraining organic carbon fluxes in an eastern boundary upwelling ecosystem (NW Africa): the role of non-sinking carbon in the context of the biological pump; CTD; CTD, Sea-Bird SBE 911plus; Density, sigma-theta (0); DEPTH, water; Dissolved Organic Carbon; ETS activity; Event label; FLUXES; Hespérides; Latitude of event; Longitude of event; mesopelagic respiration variability; Pressure, water; Salinity; Station label; SUMMER; suspended and sinking particulate organic carbon; Sustainable Management of Mesopelagic Resources; Temperature, water; Temperature, water, potential |
| url | https://doi.org/10.1594/PANGAEA.930889 |