’n‹…˜f¯‰ÈŠwêU ’n‹…‰ÈŠwçt‡•”“Á•Êu‰‰‰ï “úŽž: 2009”N11ŒŽ4“ú(…) 16:30 - 18:00 êŠ: ‹ž“s‘åŠw—Šw•”6†ŠÙ 201†Žº ‘è–Ú: Simulation of Younger Dryas Event and Its Iimplication for Future Climate Change u‰‰ŽÒ: ^“çi˜Y æ¶ (ƒvƒŠƒ“ƒXƒgƒ“‘åŠw) u‰‰—vŽ|: Using a coupled ocean-atmosphere model, this study explores the physical mechanism responsible for so-called abrupt climate change such as Younger Dryas events. In response to massive fresh water discharge into northern North Atlantic over 500 years, the simulated thermohaline circulation (THC) weakens in the Atlantic Ocean, reducing surface temperature over the northern North Atlantic and surrounding regions. Upon the termination of fresh water discharge on the 500th year, the THC begins to intensify, regaining its original intensity in a few hundred years. The sudden onset and termination of fresh water induce an irregular, multi-decadal fluctuation in the THC intensity, yielding almost abrupt climate changes. A similar, but much weaker fluctuation of the THC is also evident in the control integration of the coupled model without freshwater forcing. It is often accompanied by the multi-decadal fluctuation of the subarctic gyre, which yields surface salinity anomaly similar to gGreat Salinity Anomalyh. Finally, the role of the THC in future climate change is discussed. –â‚¢‡‚킹æ: “nç²—T”üŽq