从太空中确定的大气氧化在森林上的年间变化
Joshua D Shutter1, Dylan B Millet1, Kelley C Wells1
1Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108, USA.
Science advances
|May 15, 2024
概括
大气基 (OH) 的可变性尚不清楚. 卫星数据显示,由于排放,压力因素和气候,森林的OH变化影响了地球的氧化能力.
科学领域:
- 大气化学 大气化学
- 气候科学 气候科学
- 地球系统科学 地球系统科学
背景情况:
- 基 (OH) 是地球热带层的主要氧化剂,对于调节大气化学是至关重要的.
- 了解OH的时间变化对于预测大气组成变化至关重要.
- 影响OH度的因素,如排放和气候,是复杂的和相互关联的.
研究的目的:
- 在温带和热带森林中调查氧基 (OH) 度的时间变化.
- 将观察到的OH变化归因于排放趋势,生物压力因素和气候变化.
- 在不断变化的环境条件下,预测大气氧化能力的未来变化.
主要方法:
- 从2012年至2020年利用基于卫星的异二烯和甲测量结果.
- 在不同的森林生态系统中分析了连贯的OH变化.
- 与排放数据,气候参数和生物应激指标相关的OH变化.
主要成果:
- 在美国东南部发现OH多年下降.
- 证明更热,更干燥的夏季可以减少因异烯影响的区域氧化潜力.
- 在厄尔尼诺现象期间,在热带雨林中观察到交替的高/低OH异常,由火灾和生物源排放驱动.
结论:
- 森林OH度表现出明显的时间变化,受到排放,气候和生物因素的影响.
- 未来大气氧化潜力对温度变化,干旱和生物排放敏感.
- 厄尔尼诺现象可以导致热带大气氧化中的复杂,局部变化,这是由于相互竞争的排放来源.
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