是重力波还是兰姆波导致了汤加火山喷发的大规模热层反应?

IF 8.3 Q1 GEOSCIENCES, MULTIDISCIPLINARY
AGU Advances Pub Date : 2025-04-03 DOI:10.1029/2024AV001470
Ruoxi Li, Jiuhou Lei, Shun-Rong Zhang, Feifan Liu, Xuetao Chen, Xiaoli Luan, Xing Meng
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引用次数: 0

摘要

2022年1月15日,汤加火山爆发,火山喷出的物质高度超过50公里,是自卫星时代以来观测到的最高火山喷发。这次喷发引起了从水圈到热圈的重大扰动。我们最近的调查发现了卫星高度的热层反应。然而,这项研究提供了两个主要可能过程的物理见解,即二次重力波(GWs)和兰姆波,它们可以解释观测到的大尺度热层扰动。模拟与观测结果的比较表明,MESORAC-HIAMCM的二次GWs在时间和幅度上与GRACE-FO测量到的全球传播热层密度扰动一致。WACCM-X模拟表明,兰姆波可以作为一个尖锐的窄波包到达热层,在510 km处可能占总扰动的25%左右。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Were Gravity Waves or Lamb Waves Responsible for the Large-Scale Thermospheric Response to the Tonga Eruption?

Were Gravity Waves or Lamb Waves Responsible for the Large-Scale Thermospheric Response to the Tonga Eruption?

The extraordinary eruption of the Tonga volcano on 15 January 2022 lofted material to heights exceeding 50 km, marking the highest observed since the satellite era. This eruption caused significant disturbances spanning from the hydrosphere up to the thermosphere. Our recent investigation discovered the dramatic thermospheric responses at satellite altitudes. This study, however, provides physical insights into two main possible processes, secondary gravity waves (GWs) and Lamb waves, which may explain those observed large-scale thermospheric disturbances. The comparison between the simulations and observations suggests that the MESORAC-HIAMCM secondary GWs are consistent with GRACE-FO measured global-propagation thermospheric density disturbances in timing and amplitude. WACCM-X simulations suggest that the Lamb wave can reach the thermosphere as a sharp, narrow wave packet, and may contribute about 25% to the total disturbances at 510 km.

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