Contrasting Feedback Attributions of Atmospheric and Surface Temperature Anomalies Related to Eastern Pacific ENSO and Central Pacific ENSO
Different feedback processes cause distinct spatial patterns of atmospheric and surface temperature anomalies in boreal winter between two types of El Nino–Southern Oscillation (ENSO):Eastern-Pacific (EP) type and Central-Pacific (CP) type.The decomposition of feedback processes is achieved by a climate feedback–response analysis method (CFRAM),which decompose s local temperature anomalies into partial temperature anomalies due to oceanic dynamics/heat storage,clouds,atmospheric dynamics,water vapor,ozone,and surface albedo.The sum of these diagnosed partial temperature anomalies is equal to the observed temperature anomaly of each type of ENSO.
Xiaoming Hu Song Yang Ming Cai
Department of Atmospheric Sciences,Sun Yat-sen University,135 West Xingang Road,Guangzhou 510275,Chi Department of Earth,Ocean,and Atmospheric Science,Florida State University,Tallahassee,FL 32306,USA
国内会议
北京
英文
1-1
2014-10-01(万方平台首次上网日期,不代表论文的发表时间)