在全球表面空气风中热带地区的扩大
Stephen S Leroy1, Sara Vannah2
1Atmospheric and Environmental Research, JANUS Research Group, Lexington, Massachusetts, MA, USA. stephen.leroy@janusresearch.us.
Scientific reports
|March 15, 2026
概括
热带地区正在扩大,每十年向极地扩大约40公里. 在地表风力数据中检测到的这种扩张对气候模型和未来荒漠化风险有影响.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 海洋学 海洋学 海洋学
背景情况:
- 哈德利细胞边缘是由表面风达到零的度定义的.
- 以前的研究还没有完全量化热带扩张的速度.
研究的目的:
- 用全球表面风数据集分析哈德利细胞边缘度的趋势.
- 为了确定热带扩张的速度和半球分布.
主要方法:
- 使用了跨校准多平台 (CCMP) 表面风数据集 (1995-2024).
- 通过定位零风度来确定哈德利细胞边缘.
- 分析了全球海洋上这些度的趋势.
主要成果:
- 检测到热带地区每十年大约[公式:参见文本]向极地显著扩大.
- 在北半球和秋冬季季节,扩大更为明显.
- 气候模型准确地复制了南半球的扩大,但低估了北半球的趋势.
结论:
- 热带地区正在向极地扩张,这对全球天气模式有影响.
- 观察到的扩大趋势对气候模型的准确性提出了挑战,特别是在北半球.
- 潜在的后果包括沙漠化增加,特别是在北美.
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