{"refrec":{"BRefID":228558,"RR":"<b>Guerreo, R.A.; Piola, A.R.; Molinari, G.N.; Osiroff, A.P.; Jáuregui, S.I.</b> (2010). Climatología de temperatura y salinidad en el Río de la Plata y su frente marítimo Argentina-Uruguay. <i>Contribución INIDEP</i>, 1555. INIDEP: Mar del PLata . ISBN 978-987-1443-03-1. 95 pp.","BEntID":220275,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Contribución INIDEP</i>, 1555. INIDEP: Mar del PLata . ISBN 978-987-1443-03-1. 95 pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Guerreo, R.A.; Piola, A.R.; Molinari, G.N.; Osiroff, A.P.; Jáuregui, S.I.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Guerreo, R.A. <i>et al.</i>","Englishabstract":"The study on climatology comprises the compilation and processing of historic data on the Río de la Plata and its adjacent region. It involved a total of 7,757 oceanographic stations performed between 1911 and 2003. The data were grouped in a warm period (November- March) and a cold one (June-September). The variability in the continental discharge of the Río de la Plata made it necessary to group data as a function of three flow levels: high, mean and low. Previous studies reveal a marked change in the average flow regime of the river basin that stars at the beginning of the 70’s with a cycle of humid characteristics during which 86% of the oceanographic stations were collected. Consequently, the hydrological series used to determine the discharge levels corresponds to the 1972-2001 period. The mean flow was 24,045 m3 s-1 and the high and low discharge values were determined at 28,000 m3 s-1 and 17,370 m3 s-1, respectively. The data were analyzed in ten horizontal levels between the surface and 500 m; the levels were defined at: 0 m, 10 m, 20 m, 30 m, 50 m, 75 m, 100 m, 150 m, 250 m and 500 m. Temperature and salinity horizontal distribution for every level, every warm and cold period and every flow condition was mapped. 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