DETERMINACION DE ESPECIES, BATIMETRIA, INDICES DE ABUNDANCIA, RECLUTAMIENTOS, SELECTIVIDAD, MUESTREOS BIOLOGICOS, RECOLECCION DE EJEMPLARES
Obtención de parámetros físicos, químicos y biológicos para el estudio de series temporales (proyecto Ecomálaga)
Cr. CANARIAS 9310. - ref CEDO 9407
Contamination in Ria de Huelva
CAMPANA DE PERIODICIDAD ANUAL PARA ESTUDIAR:\n1.- LAS RELACIONES DE DEIFERENTES VARIABLES AMBIENTALES MARINAS CON LA ABUNDANCIA Y DISTRIBUCION ESPACIAL DE LOS HUEVOS Y LARVAS DE PECES.\n2.- MUESTREOS MULTIDISCIPLINARES EN 85 ESTACIONES
Oceanographic survey collected in the framework of the following research project: INTERCAMBIOS EN EL ESTRECHO DE GIBRALTAR Y SU RESPUESTA A FORZAMIENTOS METEOROLOGICOS Y CLIMATICOS, INGRES 2. This Project is funded by the Education and Science Spanish Ministery.The technical objetive of the mission is to recover and to deploy a mooring system in a monitoring station (Espartel) in the Strait of Gibraltar to estimate the Mediterranean Outflow accurately (ADCP based observations) and the Atlantic Inflow into the Mediterranean Sea, with the help of indirect estimators and incomplete currentmeter data sets
Estudio de la variabilidad de las condiciones hidrodinamicas en aguas de las Islas Baleares Influencia que tienen estas sobre la circulaci??n regional y esta sobre las comunidades planctonicas estudio de tendencias climaticas y su posible relacion con otros parametros biologicos y pesqueros.
ESTUDIO DEL ICTIOPLANCTON Y DEL MEDIO MARINO EN LOS SECTORES NORTE Y SUR DEL MAR DE ALBORAN
DETERMINACION DE ESPECIES, CARTOGRAFIADO, BATIMETRIA, INDICE DE ABUNDANCIA, RECLUTAMIENTOS, SELECTIVIDAD, MUESTREOS BIOLOGICOS, RECOLECCION DE EJEMPLARES
Forty-jour CTD stations were conducted out during the cruise Canarias 9205 qf the R. Ii Francisco de Paula Navarro. The present publication is based on the study of the geostrojic circulation and data on temperature, salinity and density obtained j?om these stations, from the sea surface to a depth of 500 m. Zn the western urea of the region, where the stations are closer togeths the geostrophic circulation shows a cyclonic eddy in the Tenertfe-Gomera channel and another antiqcl nic to the South of these islands. The temperature and salinity distributions also show both eddies. In the middle of the qclonic eddy, the upwelled water comes from a depth of about 75 m. On the another hand, the temperature and salinity distributions show, between Gran Canaria and Fuerteventura Glands, the end of ajilament ofupwelled water on the nearby Aftican coast, that had a thick of about 50 m ofj Punta Janda.