东亚的综合气候学与大西洋的多十年变化相关
1Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan.
Journal of environmental management
|December 5, 2024
概括
大西洋多年周期振荡 (AMO) 影响东亚的天气. 一个负的AMO阶段会改变喷流,改变冷浪和台风的频率,从而使气候预测成为可能.
科学领域:
- 气候学 气候学 气候学
- 大气科学 大气科学
- 气象学 天气学
背景情况:
- 大西洋多季度振荡 (AMO) 是一个重要的气候模式,有观察到的历史数据.
- AMO已经证明了与全球综合气候变化的潜在联系,可以用于气候预测.
- 了解AMO对区域天气模式的影响对于长期预报至关重要.
研究的目的:
- 研究AMO诱导的东亚西部喷射流对天气模式的影响.
- 分析AMO对冬季寒潮和夏末台风频率的影响.
- 评估基于AMO时间表的东亚长期综合气候学预测的可行性.
主要方法:
- 利用集群分析来检查1941年至2021年的天气模式频率.
- 分析了AMO阶段与冷浪和台风的发生之间的关系.
- 研究了上热带层西部喷流位置的变化.
主要成果:
- 在负AMO阶段,西喷流的向南转移被观察到.
- 这种转变导致冬季冷浪频率的反向变化:增加波列车波浪和减少阻塞波浪.
- 夏末更明显的波浪模式和向南的喷流转移与台风频率的增加有关.
结论:
- 由AMO引起的喷流转移显著影响东亚的天气模式,包括寒潮和台风.
- 在AMO时间尺度上对东亚综合气候学的长期预测似乎是可行的.
- 该研究强调AMO是理解和预测区域气候变化的关键因素.
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