通过观测数据检测臭氧和温室气体驱动的风力趋势
Sukyoung Lee1, Steven B Feldstein
1Department of Meteorology, The Pennsylvania State University, University Park, PA 16802, USA. sxl31@meteo.psu.edu
概括
南极臭氧层的减少显著地推动了西部喷气的极向转移,这比温室气体 (GHG) 的增加更重要. 观测数据分析证实了这一发现,突出了臭氧.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 臭氧层研究 臭氧层研究
背景情况:
- 之前的建模研究将南极臭氧消耗和温室气体 (GHG) 增加与南极夏季西流向极转移联系起来.
- 使用观测数据将臭氧消耗和温室气体强迫的独特贡献分离起来一直是个挑战.
研究的目的:
- 通过使用观测数据,调查南极臭氧消耗和温室气体增加对西流观测到的极向转移的贡献.
- 为了区分臭氧消耗与温室气体对大气循环模式的影响.
主要方法:
- 将集群分析应用于每日ERA-Interim再分析数据.
- 确定了两个不同的7至11天的风集群,代表了对温室气体强迫和臭氧消耗的反应.
- 分析了这些已识别的风集群发生频率的趋势.
主要成果:
- 分析发现了与温室气体强迫和臭氧消耗相关的独特风力模式.
- 集群频率的趋势表明,臭氧消耗对西向喷气转移的贡献大约比温室气体增加多50%.
- 热带对流被确定为温室气体驱动趋势的一个重要因素.
结论:
- 观测数据分析支持建模研究,证实臭氧消耗是澳大利亚夏季西部喷气转移的主要驱动因素.
- 这些发现强调了臭氧层恢复对南半球气候动态的重大影响.
- 热带对流在温室气体引起的循环变化中的作用需要进一步研究.
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