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格陵兰冰盖大量释放的无效
Christian Juncher Jørgensen1, Jens Søndergaard1, Martin Mørk Larsen1
1Department of Ecoscience, Aarhus University, Roskilde 4000, Denmark.
Science advances
|January 26, 2024
概括
这项研究发现,格陵兰冰盖融水中的度并不极高,与此前的报道相反. 冰川融水对格陵兰的风险有限.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 北极研究研究北极研究
背景情况:
- 人为 (Hg) 排放的远程运输是北极地区的主要来源.
- 最近的报道表明,格陵兰冰盖 (GrIS) 融水中的度令人担忧,可能来自基岩来源.
- 以前的发现表明Hg水平比典型的淡水系统高100至1000倍,需要独立验证.
研究的目的:
- 为了独立验证格陵兰冰盖融水中报告的极端度.
- 为了评估融水中的实际含量,从Gris以下.
- 确定GRIS融水对全球预算和当地生态系统的影响.
主要方法:
- 在格陵兰西部的21个冰川出口处进行 (Hg) 测量.
- 分析了从格陵兰冰盖下方收集的融水样本.
- 结果与之前报告的异常度相比较.
主要成果:
- 之前报告的Gris融水的极端度无法再现.
- 从格里斯下方的融水中发现含量非常低.
- 格里斯融水对全球预算的贡献很小.
结论:
- 格陵兰冰盖并不是北极的重要来源.
- 来自Gris的融水对当地社区和自然环境构成的风险非常有限.
- 之前关于异常度和基岩来源的结论没有得到这项研究的支持.
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