中国未来的热应力均升高,由空间异质的水蒸气变化驱动
Fan Wang1,2, Meng Gao3,4, Cheng Liu5,6
1Department of Geography, Hong Kong Baptist University, Kowloon Tong, 999077, Hong Kong SAR, China.
Nature communications
|May 28, 2024
概括
中国的湿球温度 (Tw) 趋势显示出空间差异,由水蒸气压力变化和区域变暖驱动. 中国东部将在本世纪末面临广泛的热应激.
科学领域:
- 气候学 气候学 气候学
- 环境科学 环境科学
- 公共卫生 公共卫生
背景情况:
- 湿球温度 (Tw) 是评估与热有关的健康风险的关键指标.
- 了解Tw趋势的空间变化对于适应气候变化至关重要.
研究的目的:
- 研究1979年至2018年中国Tw的空间异质趋势.
- 确定观察到的Tw趋势背后的驱动因素.
- 为了在中国预测未来的热应力.
主要方法:
- 在中国 (1979-2018) 地区对Tw趋势的分析.
- 使用气候模型模拟的归因分析.
- 研究水蒸气压力 (Ea) 和区域变暖的作用.
主要成果:
- 在中国南部和北部之间观察到空间异质的Tw趋势.
- 实际的水蒸气压力 (Ea) 变化是不同的Tw趋势的主要驱动因素.
- 东亚高度地区的更快变暖影响了大气模式,影响了中国南部的Tw.
- 预计到本世纪末,中国东部 (94%的人口) 将经历广泛,均的升温热应激.
结论:
- 气候变化引起的气候变暖和水蒸气动态显著影响中国的区域Tw趋势.
- 在中国东部,迫切需要制定适应热应激的适应策略.
- 这些发现对其他面临类似气候变化影响的地区有更广泛的影响.
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