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- W308052952 abstract "Seasonal variability at the entrance to the Gulf of California is described using high resolution CTD data from a section across the entrance to the gulf that was occupied eight times between 1992 and 1998. Variability decreased rapidly below 100 dbar, so that standard deviations exceeding 0.5oC and 0.05 for temperature and salinity, respectively, were confined to the upper 150 dbar. The mean salinity field wasasymmetric, with fresher waters (S 34.8) above 50 dbar and between 100 and 150 dbar near Baja California. A seasonal thermocline developed in the upper 50 dbar, increasing from 21oC in February surface temperatures to 31oC in August. Below 100 dbar, temperature at a given pressure was typically colder in the center of the section, indicating cyclonic flow (flow into the gulf next to Sinaloa and out of the gulf next to Baja California). The subsurface mid-gulf cooling (cyclonic flow) was strongest during winter and spring when the exchange of heat between the gulf and the Pacific Ocean is large. Subsurface mid-gulf heating (corresponding to anticyclonic flow) was not observed. Temporal and spatial distribution of saline water masses suggests that heat exchanges take place by alternating the inflow and outflow of warm (surface) and cold (subsurface) water masses. The 1997–1998 El Nino resulted in a 50 dbar deepening of the thermocline in November 1997, as well as a freshening of 0.1 to 0.2 of waters above the thermocline." @default.
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- W308052952 date "2000-01-01" @default.
- W308052952 modified "2023-09-27" @default.
- W308052952 title "VARIACIÓN ESTACIONAL DE LA TEMPERATURA Y SALINIDAD EN LA ENTRADA DEL GOLFO DE CALIFORNIA, MÉXICO SEASONAL VARIATION OF THE TEMPERATURE AND SALINITY AT THE ENTRANCE TO THE GULF OF CALIFORNIA, MEXICO" @default.
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