气候学
拉尼娜现象
厄尔尼诺南方涛动
模式(计算机接口)
全球变暖
大气(单位)
环境科学
南方涛动
气候变化
大气科学
海洋学
地质学
地理
气象学
计算机科学
操作系统
作者
Alexey V. Fedorov,S. George Philander
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2000-06-16
卷期号:288 (5473): 1997-2002
被引量:686
标识
DOI:10.1126/science.288.5473.1997
摘要
Recent advances in observational and theoretical studies of El Nino have shed light on controversies concerning the possible effect of global warming on this phenomenon over the past few decades and in the future. El Nino is now understood to be one phase of a natural mode of oscillation-La Nina is the complementary phase-that results from unstable interactions between the tropical Pacific Ocean and the atmosphere. Random disturbances maintain this neutrally stable mode, whose properties depend on the background (time-averaged) climate state. Apparent changes in the properties of El Nino could reflect the importance of random disturbances, but they could also be a consequence of decadal variations of the background state. The possibility that global warming is affecting those variations cannot be excluded.
科研通智能强力驱动
Strongly Powered by AbleSci AI