20世纪工业黑碳排放改变了北极气候,迫使北极气候变化
Joseph R McConnell1, Ross Edwards, Gregory L Kok
1Desert Research Institute, Nevada System of Higher Education, Reno, NV 89512, USA. Joe.McConnell@dri.edu
概括
格陵兰冰芯中黑碳 (BC) 沉积揭示了重要的历史变化. 自1800年代中期以来,工业排放大幅增加了BC度和北极雪地气候强迫.
科学领域:
- 大气化学 大气化学
- 古气候学 古气候学
- 环境科学 环境科学
背景情况:
- 燃烧产生的黑碳 (BC) 影响大气性质和雪白度.
- 对于BC的历史排放和沉积数据是有限的.
- 了解BC在过去气候变化中的作用至关重要.
研究的目的:
- 为了重建在格陵兰的BC的历史排放和沉积.
- 调查生物质燃烧和工业活动对BC度的影响.
- 量化BC对北极雪白度和气候强迫的影响.
主要方法:
- 在格陵兰冰芯中分析BC,酸和非海盐硫.
- 从1788年到现在的冰芯数据.
- 来自BC沉积的表面气候强迫的估计.
主要成果:
- 自1788年以来,格陵兰降水中的BC度发生了显著的变化.
- 从1850年左右开始的工业排放导致BC度增加了七倍,特别是在冬季.
- 峰值BC强迫 (1906-1910) 比工业化前水平高出八倍.
结论:
- 历史上,北极森林火灾和工业活动影响了格陵兰的BC沉积.
- 工业化导致北极地区的BC度大幅增加和气候强迫.
- BC沉积对北极气候产生了显著的,历史上变化的影响.
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