{"refrec":{"BRefID":260828,"RR":"<b>Schmittner, A.</b> (2016). The smoking gun for Atlantic circulation changes. <i>Science (Wash.) 353(6298)</i>: 445-446. <a href=\"http://dx.doi.org/10.1126/science.aag3156\" target=\"_blank\">http://dx.doi.org/10.1126/science.aag3156</a>","BEntID":252846,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 353(6298)</i>: 445-446. <a href=\"http://dx.doi.org/10.1126/science.aag3156\" target=\"_blank\">http://dx.doi.org/10.1126/science.aag3156</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Schmittner, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Schmittner, A.","Englishabstract":"The Atlantic meridional overturning circulation (AMOC) has long been implicated in rapid climate changes during the most recent ice age. However, convincing observational evidence from the deep ocean has remained limited. 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