海底地震计揭示了地球最长的流出沉积物流中的冲浪动态
Pascal Kunath1, Peter J Talling2,3, Dietrich Lange1
1GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany.
概括
流是强大的水下流,可以跨越很远的距离. 这项研究表明,密集层中的涌推动了这些流动,解释了它们的长距离范围和破坏性潜力.
科学领域:
- 地质科学 地质科学
- 海洋学 海洋学 海洋学
- 地震学 地震学
背景情况:
- 流是重要的地质因素,塑造海洋底的地形和影响基础设施.
- 直接测量这些强大而破坏性的流动是极其困难的,阻碍了对它们的动态的理解.
研究的目的:
- 开发和应用一种新的遥感方法,用于监测深海的流.
- 阐明长途乱电流流的内部动态和驱动机制.
主要方法:
- 部署海底地震计,将它们安置在流之外的安全位置.
- 分析地震信号,包括功率变化和信号偏振,以推断流动特征.
- 远程监控峡谷冲洗事件以记录流速和结构.
主要成果:
- 流的流量前沿含有密集的,涌的近床层,持续数小时.
- 最快的冲浪,发生在30-60分钟后的流向前线,为长途旅行 (>1000公里) 提供动力.
- 地震数据成功地区分了流和沉积物运输信号,揭示了流动演变.
结论:
- 在密集的近床层中激增是推动长时间流出度流的关键机制.
- 远程地震监测为研究危险的深海流提供了一种可行的方法.
- 了解这些动态对于预测对海底基础设施和地质过程的影响至关重要.
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