{"refrec":{"BRefID":133237,"RR":"<b>Klein, B.; Tomczak, M.</b> (1994). Identification of diapycnal mixing through optimum multiparameter analysis 2. Evidence for unidirectional diapycnal mixing in the front between North and South Atlantic Central Water. <i>J. Geophys. Res. 99(C12)</i>: 25275-25280. <a href=\"http://dx.doi.org/10.1029/94JC01948\" target=\"_blank\">http://dx.doi.org/10.1029/94JC01948</a>","BEntID":127205,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 99(C12)</i>: 25275-25280. <a href=\"http://dx.doi.org/10.1029/94JC01948\" target=\"_blank\">http://dx.doi.org/10.1029/94JC01948</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Klein, B.; Tomczak, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Klein, B.; Tomczak, M.","Englishabstract":"Optimum multiparameter (OMP) analysis is used to analyze mixing in the central water boundary of the tropical North Atlantic Ocean. Diapycnal mixing is found to be prevalent in the frontal region. OMP analysis shows that the mixing is unidirectional (South Atlantic Central Water is always mixed upward into North Atlantic Central Water) but cannot identify the process responsible for the observed diapycnal mixing. A histogram of stability ratios R<i>p</i> for all mixing lines shows R<i>p</i> values between unity and the value found in the parent water masses. 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