高地Yedoma taliks是大气甲的一个不可预测的来源
K M Walter Anthony1, P Anthony2, N Hasson2
1Water and Environmental Research Center, University Alaska Fairbanks, Fairbanks, AK, USA. kmwalteranthony@alaska.edu.
Nature communications
|July 18, 2024
概括
北极永久土的融化可以释放大量的甲. 富含冰的Yedoma沉积物,在融化成taliks时,会发出更多的甲,特别是在冬季,放大永久土-甲-气候反.
科学领域:
- 地球科学 地球科学 地球科学
- 环境科学 环境科学
- 气候科学 气候科学
背景情况:
- 永久土的融化预计将增加北极土壤中的甲氧化.
- 富含碳的Yedoma永久土可能会遵循不同的排放路径.
- 塔利克斯 (永久土中的融化土壤) 正在以前结的地区形成.
研究的目的:
- 为了调查Yedoma永久土的甲排放情况.
- 量化从未和的耶多马高地释放的甲.
- 评估对永久土-甲-气候反的影响.
主要方法:
- 在Yedoma高地对甲排放的实地观测.
- 用土壤样本进行实验室实验.
- 塔利克形成的遥感和数值建模.
- 排放率与北方湿地的比较.
主要成果:
- 在高地地区的Yedoma taliks中,甲排放量很高 (35-78 mg m−2 d−1夏季,150-180 mg m−2 d−1冬季).
- 每年的山地Yedoma talik排放量几乎是北方湿地排放量的三倍.
- 冬季排放量约占年度甲排放总量的70%.
- 冬季表面土壤的结减少了甲的氧化,使得塔利克斯可以更好地逃脱.
结论:
- 高地Yedoma taliks是北极甲排放的重要来源.
- 广泛的塔利克形成被投射到泛北极Yedoma领域.
- 永久土-甲-气候反可能被低估,特别是在耶多马地区.
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