acceda Comunidad : http://hdl.handle.net/10553/3 2013-06-19T22:06:04Z 2013-06-19T22:06:04Z 5 arquitecturas en el barrio de San Cristobal Tejera Romero, Rayco http://hdl.handle.net/10553/7641 2012-07-06T11:42:53Z 2012-07-04T23:00:00Z Título : 5 arquitecturas en el barrio de San Cristobal Autor : Tejera Romero, Rayco Resumen : <html /> 2012-07-04T23:00:00Z Zooplankton metabolic activity (respiration and ETS) from three stages of the Malaspina 2010 campaign Maldonado-Uribe, Federico http://hdl.handle.net/10553/6708 2013-04-22T09:16:45Z 2011-11-29T00:00:00Z Título : Zooplankton metabolic activity (respiration and ETS) from three stages of the Malaspina 2010 campaign Autor : Maldonado-Uribe, Federico Resumen : Se analizan resultados de datos obtenidos en la Campaña de circunnavegación Malaspina 2010 Descripción : Primera Tesis de Máster con resultados de la Campaña de Circunnavegación Malaspina 2010 2011-11-29T00:00:00Z Wind-driven cross-equatorial flow in the Indian ocean Pérez-Hernández, M.Dolores Joyce, Terrence Vélez Belchí, Pedro http://hdl.handle.net/10553/4615 2011-08-09T08:26:17Z 2010-12-03T00:00:00Z Título : Wind-driven cross-equatorial flow in the Indian ocean Autor : Pérez-Hernández, M.Dolores; Joyce, Terrence; Vélez Belchí, Pedro Resumen : NCEP Wind-stress and temperature and salinity data from Argo have been used together with a steady model to estimate the meridional velocity and volume and heat transport in the Equatorial Indian Ocean for a seven years period (2003-2009). Total volume transport of the wind stress curl shows a northward and southward flow for theWinter and Summer Monsoon,respectively. The velocity section shows a Somali Current flowing in opposite direction in the Winter and Summer Monsoons. In the Winter Monsoon, the Somali Current is shallow (~ 200 dbar) and flows to the south with and undercurrent below it. In the Summer Monsoon and Transitional Periods, the Somali Current flows to the north and to the south, respectively and extend to (~ 650 dbar) depth. The heat transport across the Equator presents a seasonal reversing, being -0.8PW to the south in the Winter monsoon and +1.2PW in the Summer Monsoon. The annual heat transport is -1.4PW that is mainly carried out by the Somali Current 2010-12-03T00:00:00Z Water masses, mass transport and variability of the Canary current in autumn Mock, Christina http://hdl.handle.net/10553/5695 2012-09-11T07:39:21Z 2011-06-16T23:00:00Z Título : Water masses, mass transport and variability of the Canary current in autumn Autor : Mock, Christina 2011-06-16T23:00:00Z