森林火灾中的深棕色碳:一个强大的雪辐射强迫剂?
Ganesh S Chelluboyina1, Taveen S Kapoor1, Rajan K Chakrabarty1
1Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO USA.
概括
野火的烟雾使雪变黑,加速融化. 暗棕色碳 (d-BrC) 显著增强了雪的变暖,比黑色碳 (BC) 更容易融化,影响冰川.
科学领域:
- 大气科学 大气科学
- 冰川学的冰川学
- 环境科学 环境科学
背景情况:
- 野火烟雾沉积使雪变黑,导致更快的融化.
- 深棕色碳 (d-BrC) 是野火烟雾中主要的吸光成分.
- 与黑碳 (BC) 相比,d-BrC在降雪变暖中的作用尚不清楚.
研究的目的:
- 量化d-BrC对雪的辐射强迫和融化的影响.
- 为了比较d-BrC与BC的降雪变暖潜力.
主要方法:
- 使用了气溶-雪辐射转移计算.
- 结合了实验室和现场测量的数据.
- 模拟了各种野火烟雾沉积场景.
主要成果:
- d-BrC显著增加了年平均雪的辐射强迫 (0.617.9 W m-2).
- 与单独的BC相比,d-BrC增加了1.6至2.1倍的雪地变暖.
- d-BrC对雪融有很大贡献,特别是在中度冰川中.
结论:
- d-BrC是野火烟雾对雪融的影响的一个关键因素.
- 这些发现凸显了d-BrC对中度冰川质量平衡的重要性.
- 对d-BrC的进一步研究对于了解气候变化对被雪覆盖地区的影响至关重要.
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