为什么当热带层变暖时,较低的平流层会变冷.
Jonathan Lin1,2, Kerry Emanuel3
1Lamont-Doherty Earth Observatory, Columbia University, New York, NY 10027.
概括
在热带地区,随着热带层升温,较低层平流层会变冷. 这种观察到的反相关性是由热层层对平流层施加压力的新理论解释的.
科学领域:
- 大气科学 大气科学
- 气候动力学 气候动力学
- 层层层层的过程
背景情况:
- 观测数据表明热带热带层和较低的平流层温度之间存在反向关系.
- 这种现象表明这些大气层之间存在动态联系.
研究的目的:
- 为了证实热带地区热层和较低的平流层温度之间的反相关性.
- 用最近提出的理论来解释这种温度关系.
- 研究这种关系对气候变化趋势的影响.
主要方法:
- 对热带地区观测温度数据的分析.
- 对热层-平流层相互作用的新理论框架的应用.
- 研究气候变化期间的温度趋势,重点关注区域不对称性.
主要成果:
- 这项研究证实,在中热层每升温1°C,下层平流层冷却约2°C.
- 观察到的反相关性是由平流层对热层加热的准平衡反应解释的.
- 在气候变化期间,热带层的区域不对称的变暖反映在较低层平流层的降温中,其幅度相当.
结论:
- 平流层通过准平衡的动力学,除了波浪分散外,也直接受到热层的强迫.
- 热层温度趋势中的区域不对称性显著影响较低的平流层温度趋势.
- 了解这些直接强迫机制对于准确的气候变化预测至关重要.
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