On the ¡°spring predictability barrier¡± for strong ... ×÷ÕߣºQI QianQian;DUAN Wan...    À´Ô´ÆÚ¿¯£ºScience China(Earth Sciences)    Äê¾íºÅ£º2017,60(09):1614-1631 ÕªÒª£ºUsing predictions for the sea surface temperature anomaly(SSTA) generated by an intermediate coupled model(ICM)ensemble   Processes involved in the second-year warming of t... ×÷ÕߣºZHANG RongHua;GAO Ch...    À´Ô´ÆÚ¿¯£ºScience China(Earth Sciences)    Äê¾íºÅ£º2017,60(09):1601-1613 ÕªÒª£ºThe tropical Pacific experienced a sustained warm sea surface condition that started in 2014 and a very strong El Niüío e   Genesis of the 2014¨C2016 El Niüío events ×÷ÕߣºLIAN Tao;CHEN DaKe;T...    À´Ô´ÆÚ¿¯£ºScience China(Earth Sciences)    Äê¾íºÅ£º2017,60(09):1589-1600 ÕªÒª£ºThe 2015/2016 El Niüío was one of the strongest El Niüío events in history, and this strong event was preceded by a weak E   Evolution of the 2015_16 El Niüío and historical pe... ×÷ÕߣºYan XUE;Arun KUMAR;    À´Ô´ÆÚ¿¯£ºScience China(Earth Sciences)    Äê¾íºÅ£º2017,60(09):1572-1588 ÕªÒª£ºThe 2015/16 El Niüío developed from weak warm conditions in late 2014 and NINO3.4 reached 3¡æ in November 2015. We describ   Enlightenments from researches and predictions of ... ×÷ÕߣºMu MU;Hong-Li REN;    À´Ô´ÆÚ¿¯£ºScience China(Earth Sciences)    Äê¾íºÅ£º2017,60(09):1569-1571 ÕªÒª£ºEl Niüío is a remarkable climate phenomenon with a basinwide warming of sea surface temperatures(SST) in the easterncentr   ×ܼƣº 19001 Æª   Ê× Ò³  ÉÏÒ»Ò³  ÏÂÒ»Ò³  Ä© Ò³