南半球大气循环的大规模大气循环的周期性变化
David W J Thompson1, Elizabeth A Barnes
1Department of Atmospheric Science, Colorado State University, Fort Collins, CO, USA.
概括
南半球大气循环显示了20-30天的周期,与巴罗临床环状模式有关. 这种气候振荡影响热量,能量和降雨,影响中度变化.
科学领域:
- 气候科学 气候科学
- 大气动力学 大气动力学
- 气象学 天气学
背景情况:
- 气候系统的周期性对于天气预测和了解气候变化至关重要.
- 南半球大气循环模式影响全球气候系统.
研究的目的:
- 为了识别和描述南半球大气循环中的周期性行为.
- 为了研究驱动这种观察到的周期性的物理机制.
主要方法:
- 分析大气数据的半球尺度平均值.
- 检查热的流,的动能和降水.
- 对气候动态的观测和理论分析.
主要成果:
- 在南半球大气循环中表现出明显的周期性 (20-30天).
- 将这种周期性与南半球的巴洛克林尼克环状模式联系起来.
- 在热流,动能和降雨中观察到周期性的出现.
结论:
- 这种20-30天的振荡是由外热带气候变暖,波浪热流和辐射阻尼之间的反驱动的.
- 这种振荡显著影响了南半球中度地区的气候变化.
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