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在卫星前的时代,Thwaites冰川迅速退缩
Alastair G C Graham1, Anna Wåhlin2, Kelly A Hogan3
1College of Marine Science, University of South Florida, St Petersburg, FL USA.
概括
斯威特斯冰川是一个冰川.
科学领域:
- 冰川学的冰川学
- 南极洲的研究研究.
- 海平面上升研究的研究.
背景情况:
- 特威茨冰川的退缩对于预测南极海平面上升至关重要.
- 冰川接地区的演变受到海底地形的影响.
- 了解过去的退缩机制对于未来的预测至关重要.
研究的目的:
- 通过海底数据调查Thwaites冰川的历史撤退.
- 为了记录过去接地区撤退的海底印记.
- 分析特威茨冰川冰面的撤退速度和机制.
主要方法:
- 在Thwaites冰川冰面上使用自主水下车辆 (AUV) 收集地质物理数据.
- 对海底沉积脊的分析表明了每日接地线的退缩.
- 与卫星观测的AUV衍生后退率的比较.
主要成果:
- 在接地线上确定了由潮过程形成的每日倒退的沉积脊.
- 记录了超过每年2.1公里的接地区撤退率,超过5.5个月.
- 观察到的撤退速度是2011-2019年间卫星测量速度的两倍.
结论:
- 在过去的两个世纪里,Thwaites冰川经历了持续的快速撤退脉冲.
- 随着接地区离开稳定海底高点,快速撤退脉冲可能会再次出现.
- 这些发现凸显了Thwaites冰川未来加速海平面贡献的潜力.
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