在阿拉斯加北部受融影响的永久土地形的火灾后稳定
Benjamin M Jones1, Mikhail Z Kanevskiy2, Yuri Shur3
1Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, AK, 99775, USA. bmjones3@alaska.edu.
Scientific reports
|April 11, 2024
概括
2007年阿纳克图武克河火灾导致北极原的永久土广泛融化. 然而,随后的观测显示稳定,永久土堆积和减少融化沉降表明受影响的地形的恢复.
科学领域:
- 北极环境科学 北极环境科学
- 永久土的动态 永久土的动态
- 地质化学 地质化学
背景情况:
- 2007年Anaktuvuk河火灾影响了超过1000平方公里的北极原,其中50%影响了富含冰的合成永久土 (Yedoma).
- 火灾后的初步观测显示,到2014年,耶多马地区的冰明显退化和融化沉降.
研究的目的:
- 评估阿纳克图武克河火灾对永久土的长期影响.
- 为了监测融沉降的变化,地面温度和被烧毁的北极原的永久土恢复.
主要方法:
- 利用2009年,2014年和2021年的重复空中LiDAR数据来绘制解沉降的地图.
- 从2010年到2022年进行地面温度测量,以分析热变化.
- 收集永久土核心以确定融化不一致性并评估永久土恢复.
主要成果:
- 融化沉降最初影响到2014年的研究区域的15%,到2021年降至<1%,表明稳定.
- 接近地表的地面温度显示火灾后的解度日增加,后来下降,平均年地面温度最初上升,然后降温.
- 永久土核心显示了解不一致,恢复的永久土层在冰槽中平均为14.2厘米,在多边形中心为18.3厘米.
结论:
- 在阿纳克图武克河火灾之后,冰丰富的永久土的初始退化之后,出现了一段解停止的时期.
- 观察结果表明永久土堆积和受影响的原地形的稳定.
- 该研究强调了北极永久土在重大火灾干扰后复杂的恢复过程.
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