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千年变化和冷却趋势在陆地表面温暖的季节温度在全新世纪期间
Yukun Zheng1, Hongyan Liu1, Hongya Wang1
1College of Urban and Environmental Sciences and MOE Laboratory for Earth Surface Processes, Peking University, Beijing 100871, China.
Science bulletin
|June 26, 2024
概括
科学家们使用深度学习开发了新的模型来重建过去的季节性温度. 这些模型揭示了由地球轨道变化驱动的全新纪冷却趋势,改善了我们对气候动态的理解.
科学领域:
- 古气候学 古气候学
- 地质化学 地质化学
- 机器学习 机器学习
背景情况:
- 千年级季节性温度的定量重建受到代理和模型稀缺性的限制.
- 了解Holocene热变化及其驱动因素需要强大的温度代理.
研究的目的:
- 通过深度学习建立全球温暖季节温度模型.
- 为了重建Holocene季节性温度,并确定驱动机制.
主要方法:
- 应用深度学习神经网络分析到分支四乙烯膜脂质.
- 利用了全球湖,泥炭地和覆盖全新纪的形状的模型.
主要成果:
- 开发了两个最佳的全球温暖季节温度模型.
- 重建的全新纪温度显示了自早期全新纪以来的降温趋势.
- 由于前行,北半球太阳辐射减少导致冷却.
结论:
- 分支四乙烯膜脂质为千年规模的季节性温度重建提供了有希望的代理.
- 开发的模型可以增强未来的气候研究,包括全球的冬季温度.
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