Science. 1994 Oct 28;266(5185):632-4. doi: 10.1126/science.266.5185.632.
An atmospheric general circulation model was forced with observed interannual changes in the global sea surface temperatures (SSTs) for the period 1982 to 1993. The simulated seasonal surface air temperature patterns over land areas closely resemble the observed. Over most of the globe, the patterns also resemble those associated with EI Niño events and are also reproduced in simulations with weak warm tropical SSTs near the date line. An exception is northern Asia, where the mechanisms for the observed warming are unclear. The results suggest that enhanced air-sea interactions resulting from recent, more persistent warm oceanic conditions in the tropics contributed to the observed global warming trend during this period.
利用观测到的 1982 年至 1993 年全球海表温度(SST)的年际变化,对大气环流模型进行了强迫。模拟的陆地地区季节性地表气温模式与观测结果非常相似。在全球大部分地区,这些模式也与厄尔尼诺事件相关,并且在模拟中,热带地区日期线附近的弱暖 SST 也产生了这些模式。一个例外是北亚地区,那里的观测变暖机制尚不清楚。结果表明,由于热带地区最近更持久的暖海洋条件导致的增强的海气相互作用,可能导致了这一时期观测到的全球变暖趋势。