臭氧污染的年间变化与中国东部的双极结构有关,与西藏高原的春季热力强迫有关
Qingjian Yang1, Tianliang Zhao1, Yongqing Bai2
1Climate and Weather Disasters Collaborative Innovation Center, Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, PREMIC, Nanjing University of Information Science &Technology, Nanjing 210044, China.
The Science of the total environment
|March 7, 2024
概括
西藏高原的热条件影响了中国东部的臭氧污染. 较强的热效应在北部增加臭氧,在南部减少臭氧,影响区域气候和空气质量.
科学领域:
- 大气化学和物理大气化学和物理
- 气候科学 气候科学
- 环境科学 环境科学
背景情况:
- 西藏高原 (TP) 显著影响中国东部下游地区的气候.
- 臭氧 (O3) 污染对气象变化很敏感,但其与TP动态的联系尚未得到充分研究.
- 了解TP在O3污染中的作用对于区域空气质量管理至关重要.
研究的目的:
- 调查西藏高原春季热力强迫对中国东部温暖季节臭氧污染的影响.
- 分析导致臭氧变化的空间模式和气象机制.
- 确定TP热强迫源对臭氧污染的影响.
主要方法:
- 中国高空气污染物O3产品 (1980-2020) 的分析.
- 利用了气象变量的ERA5再分析数据.
- 研究了TP热强迫和O3污染模式之间的相关性.
主要成果:
- 春季的TP热强迫在EC臭氧污染中产生双极模式.
- 较强的TP热强迫导致欧洲共同体北部的O3增加,欧洲共同体南部的O3减少.
- 相关的气象异常包括压力系统,云层,太阳辐射和温度.
结论:
- TP热强迫是EC年间臭氧污染变化的关键驱动因素.
- 这些发现为TP对大气环境变化的影响提供了新的见解.
- 这项研究为预测和减轻欧洲共同体的臭氧污染提供了基础.
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