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Keyword
Algeciras
17 record(s)
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FONDEO DE UNA LINEA DE 5 CORRENTOMETROS EN EL ESTRECHO DE GIBRALTAR A UNA PROFUNDIDAD DE 450 m\nPERFILES DE CTD
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FONDEO DE CADENA DE TERMISTORES Y 3 CORRENTOMETROS EN PUNTA EUROPA, AL SUR DEL ESTRECHO DE GIBRALTAR.\nSONDEO CON CTD EN LA BOCA ESTE DEL ESTRECHO PARA CONOCIEMIENTO DE LA HIDROLOGIA DE LA ZONA.
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To estimate nitrogen (NH4+, NO2-, NO3-), phosphate and silicate fluxes in the Strait of Gibraltar, to quantify and characterise the fluxes of particulate organic carbon and nitrogen (POC/PON) and to estimate of picoplankton, nanoplankton and microplankton biomass distribution in the Strait of Gibraltar. To describe the hydrological structure and the geochemical fields of the region of the Gulf of Cadiz, particularly at the levels influenced by the Mediterranean waters, in order to set a background for interpreting the dynamics of the Outflow
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Cr. CANALES CNL-0396 - ref CEDO 9601
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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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The tidal gauge of Algeciras was located at the harbour and it measured sea level from 1943 to 2002. A new tide gauge (PSMSL ID 2117) replaced this stations with records from 2006 onwards.
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The tidal gauge of Algeciras is located at the harbour and it measures sea level from November 2006 onwards. This station is a replacement gauge for the former Algeciras tide gauge (PSMSL ID 490) with records from 1943 to 2002.
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The tidal gauge of Málaga is located at the harbour and it measures sea level from 1943 onwards, with a gap between 1959 and 1961.
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To estimate nitrogen (NH4+, NO2-, NO3-), phosphate and silicate fluxes in the Strait of Gibraltar, to quantify and characterise the fluxes of particulate organic carbon and nitrogen (POC/PON) and to estimate of picoplankton, nanoplankton and microplankton biomass distribution in the Strait of Gibraltar. To describe the hydrological structure and the geochemical fields of the region of the Gulf of Cadiz, particularly at the levels influenced by the Mediterranean waters, in order to set a background for interpreting the dynamics of the Outflow
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LOCALIZACION DEL CHORRO ATLANTICO ENTRANTE POR EL ESTRECHO DE GIBRALTAR, FRENTE TERMICO Y HALINO ASOCIADO Y ZONAS DE AFLORAMIENTO AL NOROESTE DE ALBORAN