亚热带模式 日本南部的水影响台风强度
Eitarou Oka1, Shusaku Sugimoto2, Fumiaki Kobashi3
1Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Japan.
Science advances
|September 13, 2023
概括
亚热带模式水 (STMW) 厚度影响北太平洋海面温度和台风强度. 较厚的STMW与较冷的海和较弱的台风相关,而较薄的STMW导致更温暖的海和更强的风暴.
科学领域:
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
- 大气科学 大气科学
背景情况:
- 亚热带模式水 (STMW) 是北太平洋的一个重要海洋特征.
- 它的形成和运动与诸如太平洋十年振荡等气候模式有关.
- STMW对海面温度和大气的影响尚未完全理解.
研究的目的:
- 研究STMW对海面温度 (SST) 和大气条件的反机制.
- 通过STMW厚度量化海洋热结构的十年调制.
- 分析STMW变化与台风强化之间的关系.
主要方法:
- 利用Argo概况浮动数据来分析日本南部的STMW特征.
- 雇佣50年的观察数据.
- 进行数值模拟以评估长期趋势和关系.
主要成果:
- STMW的厚度,每十年变化,通过增加异热升起来调节覆盖的热结构.
- 由STMW引起的十年温度变化可以达到~1°C,特别是在温暖的季节.
- 较厚的STMW年表现出明显较低的SST,上海热量含量和台风强化率.
- 较薄的STMW年表现出更高的SST,上层海洋热量含量和台风强化率.
结论:
- 在规范北太平洋SST和大气现象方面,STMW起着至关重要的作用.
- STMW厚度的十年变化对区域气候有明显的影响,包括台风活动.
- 了解STMW动态对于预测气候变化和极端天气事件至关重要.
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