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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).
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Fondeo de una linea de cinco correntometros en el centro del canal entre la isla de Alboran y cabo Tres Forcas, en el punto 35°41.5'N, 03°01'W, a 900 m de fondo.\nTransecto hidrologico Melilla - Adra, con 11 estaciones de CTD
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Observation and modelling of eddy scale geostrophic and ageostro-phic circulation
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1.- LEVANTAMIENTO DE LA LINEA DE CINCO CORRENTOMETROS FONDEADA EN EL ESTRECHO DE GIBRALTAR, A UNA PROFUNDIDAD DE 450m\n2.- VOLVES A FONDEAT LA MISMA LINEA EN EL MISMO SITIO\n3.. PERFILES DE CTD PARA LOCALIZACION Y CONTOL DE LAS MASAS DE AGUA QUE ATRAVIESAN EL ESTRECHO
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Obtencion de serie Historica de datos Oceanograficos para estudio de variacion de ecosistemas
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Cr. First field campaign.
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Obtenci??n de serie hist??rica de datos oceanograficos para el estudio de variaci??n de ecosistemas.
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Oceanographic parameters of water column
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LOCALIZACION DEL CHORRO ATLANTICO ENTRANTE POR EL ESTRECHO DE GIBRALTAR, FRENTES TERMICOS Y HALINO ASOCIADO Y ZONAS DE AFLORAMIENTO AL NOROESTE DEL MAR DE ALBORAN
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Sampling oceanographic and biological variables to staudy the temporal variability.