{"refrec":{"BRefID":234290,"RR":"<b>Reid, Ph.C.; Beaugrand, G.</b> (2012). Global synchrony of an accelerating rise in sea surface temperature. <i>J. Mar. Biol. Ass. U.K. 92(7)</i>: 1435-1450. <a href=\"http://dx.doi.org/10.1017/S0025315412000549\" target=\"_blank\">http://dx.doi.org/10.1017/S0025315412000549</a>","BEntID":225974,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Mar. Biol. Ass. U.K. 92(7)</i>: 1435-1450. <a href=\"http://dx.doi.org/10.1017/S0025315412000549\" target=\"_blank\">http://dx.doi.org/10.1017/S0025315412000549</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Reid, Ph.C.; Beaugrand, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Reid, Ph.C.; Beaugrand, G.","Englishabstract":"The oceans have shown a recent rapid and accelerating rise in temperature with, given the close link between temperature and marine organisms, pronounced effects on ecosystems. Here we describe for the first time a globally synchronous pattern of pulsed short period (~1 year long) emanations of warm sea surface temperature anomalies from tropical seas towards the poles on the shelf/slope with an intensification of the warming after the 1976/1977, 1986/1987 and 1997/1998 El Ni&#241;os. On the eastern margins of continents the anomalies propagate towards the poles in part by largely baroclinic boundary currents, reinforced by regional atmospheric warming. The processes contributing to the less continuous warm anomalies on western margins are linked to the transfer of warmth from adjacent western boundary currents. 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