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Research and Development of High-performance Explosives
Published on: February 20, 2016
在热带大西洋上空,广泛的素介导臭氧破坏
Katie A Read1, Anoop S Mahajan, Lucy J Carpenter
1Department of Chemistry, University of York, Heslington, York YO10 5DD, UK.
Nature
|June 27, 2008
概括
在模型中低估了热带层臭氧损失. 新的研究证实和化合物在热带海洋边界层显著增加臭氧破坏,影响气候预测.
科学领域:
- 大气化学 大气化学
- 气候科学 气候科学
- 海洋化学 海洋化学
背景情况:
- 热带层臭氧在过去150年里显著增加,导致气候扰乱.
- 热带海洋边界层的臭氧损失主要是由臭氧光解和水蒸气驱动的.
- 以前的模型表明,素化合物可以减少臭氧,但这缺乏观测证据.
研究的目的:
- 为了验证和在热带海洋边界层臭氧损失中的作用.
- 量化素化学对观察到的臭氧消耗率的影响.
- 评估素化学对大气模型和气候预测的影响.
主要方法:
- 在佛得角天文台进行光谱测量,检测和一氧化物.
- 全年在现场进行地表微量气体测量.
- 低水平飞机观测和盒子模型计算.
主要成果:
- 在热带海洋边界层证实白天无处不在的氧化物和氧化物存在.
- 观察到的每日臭氧损失比模拟的模拟模型 (不包括素化学) 大约50%.
- 盒子模型计算表明观察到的素度解释了额外的臭氧损失.
结论:
- 素化学显著影响热带大西洋边界层的光化学臭氧损失.
- 在大气模型中排除素来源和化学物质可能会导致臭氧预算和气候预测的重大错误.
- 准确预测未来的臭氧趋势需要将素化学纳入大气模型.
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