使用纽约州的Mesonet数据来描述2024年完全日食的影响.
Junhong Wang1, Aiguo Dai2, Chau-Lam Yu1
1New York State Mesonet SUNY University at Albany Albany NY USA.
概括
在纽约发生的日全食 (TSE) 导致了显著的表面冷却和大气变化. 行星边界层 (PBL) 变浅和潮湿,而二氧化碳水平由于光合作用减少而上升.
科学领域:
- 大气科学 大气科学
- 地质物理学 地质物理学
- 环境科学 环境科学
背景情况:
- 2024年4月8日,在纽约州 (NYS) 发生了一场罕见的完全日食 (TSE),这是自1925年以来的第一次.
- 纽约证券交易所 Mesonet (NYSM) 网络在活动期间提供了大量数据.
研究的目的:
- 使用NYSM数据分析TSE对地表,行星边界层 (PBL) 和二氧化碳度的影响.
- 描述TSE期间大气和表面流量变化的特征.
主要方法:
- 利用55个位于TSE总体轨道内的NYS Mesonet气象站的数据.
- 在TSE发生之前,期间和之后分析了表面温度,风,湿度,热流和二氧化碳度.
主要成果:
- 峰值表面冷却平均为2.8°C (最大6.8°C) 总体后17分钟.
- 观测到类似夜间的表面反转,平静的风,PBL浅,和加湿.
- 感觉,潜伏和地下热流量减少;由于光合作用减少,近地表二氧化碳增加.
结论:
- 该TSE显著改变了表面能量平衡和PBL动态.
- 在TSE期间减少的太阳辐射导致了可测量的大气和生物圈反应.
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