南京大学学报(自然科学版) ›› 2011, Vol. 47 ›› Issue (6): 670678.
胡海波1,2,张媛2,于亮1
Hu Hai-Bo1,Zhang Yuau2,Yu Liang1
摘要: 摘要:利用Fast Ocean-Atmosphere Model (FOAM)海气祸合模式,分析了CO2加倍后热带太平洋海气系统的变化趋势并进行了机制研究.结果表明,CO2加倍后,模式中整个赤道海域海洋表面温度升
高,但赤道西太平洋海面温度的增幅要强于东赤道太平洋的现象.产生这种增暖趋势的主要原因是由于热带区域160ºF以东海面东风的增强及东赤道次表层海洋冷水上翻的增强,使得赤道太平洋东部海域
上层海洋增暖减缓.CO2增加后,模式中Nino事件的演变过程与控制试验相似,但La Nina事件的演变在两个试验中有明显区别:CO2加倍试验中La Nina事件的冷海温异常强度更强、维持时间更久,且Fl
Nino-Southern Oscillation circulation (FNSO)事件的周期也有所增长.ENS0周期的改变是由于模式中CO2浓度增加后,热带与热带外热容量交换的减小,使得热带海域热容量的充放电速度减慢,根据“充放
电理论”,FNSO事件周期将拉长.
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