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地球连续自由振荡的激发是由大气-海洋-海底合
Junkee Rhie1, Barbara Romanowicz
1Berkeley Seismological Laboratory and Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA.
Nature
|October 1, 2004
概括
地球 地球 地球 地球 地球 地球
科学领域:
- 固体地球地质物理学
- 地震学 地震学
- 海洋学 海洋学 海洋学
背景情况:
- 地球表现出连续的振荡,称为"",在地震记录 (2-7mHz) 中检测到.
- 的激发水平很大,与中度地震相比,不能归因于小地震事件.
- 以前关于声来源的假设,包括缓慢的地震,在很大程度上被排除在外,指向大气或海洋过程.
研究的目的:
- 开发和应用一个基于阵列的方法来检测和定位地球的激发源.
- 确定与的产生相关的主要地理区域和季节性变化.
主要方法:
- 利用基于阵列的地震检测和定位方法.
- 分析了地震数据,确定了2-7毫赫兹范围内的自由振荡峰值的起源.
- 与季节性和地理因素相关的度激发源.
主要成果:
- 地球的声主要是在北半球冬季的北太平洋产生的.
- 声起源于南半球冬季的南方海洋.
- 基于阵列的方法成功检测并定位了的激发源.
结论:
- 地球的声主要是由大气,海洋和海底的相互作用产生的.
- 风暴能量很可能转化为海洋的低重力波,然后与海底的地形相互作用,产生.
- 这项研究提供了强有力的证据,证明了一种机制将天气模式与全球地震湿度联系起来.
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