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热带地区范围内的季节内振荡.

Jiawei Bao1, Sandrine Bony2, Daisuke Takasuka3

  • 1Institute of Science and Technology Austria, Klosterneuburg 3400, Austria.

Proceedings of the National Academy of Sciences of the United States of America
|November 24, 2025
PubMed
概括

在热带地区发现了一种新的热带范围内的季内振荡 (TWISO),持续30-60天. 这种振荡影响天气和气候,虽然与马登-朱利安振荡 (MJO) 相关,但它可以独立发生.

关键词:
马登朱利安振荡的发生.在季内波动的季内波动.辐射-传递平衡的辐射-传递平衡.热带地区的平均振荡.

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科学领域:

  • 气候科学 气候科学
  • 大气科学 大气科学
  • 热带气象学 热带气象学

背景情况:

  • 热带气候的变化是由各种时间尺度的振荡驱动的.
  • 缓慢的过程,如季节性和跨年变化,通常解释主要的热带气候变化.

研究的目的:

  • 为了识别和描述以前未被识别的热带范围内的季内振荡 (TWISO).
  • 调查TWISO,马登-朱利安振荡 (MJO) 和辐射-对流平衡之间的关系.
  • 评估TWISO对热带天气和气候的潜在影响.

主要方法:

  • 分析卫星观测和气候再分析.
  • 识别30至60天周期的振荡.
  • 检查对流,辐射,表面流和大规模循环之间的相互作用.

主要成果:

  • 确定了一个明显的热带范围内的季内振荡 (TWISO),周期为30-60天.
  • TWISO涉及对流,辐射,表面流和热带循环的合变化.
  • TWISO阶段与MJO阶段发生一致,但TWISO不需要MJO.

结论:

  • TWISO是热带气候变化的重要组成部分.
  • 虽然MJO可以调节TWISO,但它不是唯一的驱动器.
  • 由于TWISO的广泛传播,这表明它对区域热带天气和气候产生了重大影响.