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在全球变暖下,湖泊的增强加热效应
Yuanlin Qiu1,2, Jie Chen3,4, Deliang Chen5
1Wuhan University, State Key Laboratory of Water Resources Engineering and Management, Wuhan, China.
Nature communications
|April 27, 2025
概括
全球气候变化正在增加湖泊的热量释放,特别是在中高度地区. 降低的冰盖增强了这种效应,未来的预测表明这些重要的淡水体会释放更多的热量.
科学领域:
- 环境科学 环境科学
- 气候科学 气候科学
- 水文学的水文学
背景情况:
- 湖泊通过大气热交换显著影响区域气候.
- 全球气候变化正在改变这些湖泊与大气之间的相互作用.
- 了解全球湖泊释放的热量及其未来趋势至关重要.
研究的目的:
- 为了研究全球湖泊散热模式的变化.
- 为了确定驱动特定区域放大热释放的因素.
- 预测湖泊释放热量的未来趋势.
主要方法:
- 全球湖泊散热模式的分析.
- 识别与湖泊冰盖相关的反机制.
- 对比不同度的热释放变化.
主要成果:
- 观察到全球湖泊释放的热量增加了.
- 中高度 (>45°N) 显示特别明显的增加.
- 减少的湖冰覆盖增加了热量的吸收和释放,特别是通过热辐射.
- 潜在热量流的季节性变化在更温暖的时期加剧了热量释放.
结论:
- 湖泊的热量释放在全球范围内正在增加,由于冰盖减少,中高度的热量显著放大.
- 这种放大的热释放是由减少绝缘和增加吸收,主要是通过热辐射驱动的.
- 未来的预测表明,湖泊释放的热量将大幅增加,超过历史趋势.
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