Physics Department & Centre of Environmental and Marine Studies, University of Aveiro, 3810-193 Aveiro, Portugal.
Applied Ocean Physics and Engineering Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA.
JASA Express Lett. 2021 Dec;1(12):126001. doi: 10.1121/10.0008939.
An M7.4 submarine earthquake occurred in the Kermadec Trench, northeast of New Zealand, on 18 June, 2020. This powerful earthquake triggered energetic tertiary waves (T-waves) that propagated through the South Pacific Ocean into the South Atlantic Ocean, where the T-waves were recorded by a hydrophone station near Ascension Island, 15 127 km away from the epicenter. Different T-wave arrivals were identified during the earthquake period with arrival angles deviating from the geodesic path. A three-dimensional sound propagation model has been utilized to investigate the cause of the deviation and confirm the horizontal diffraction of the T-waves at the Drake Passage.
2020 年 6 月 18 日,新西兰东北部的克马德克海沟发生了一次 M7.4 级海底地震。这次强烈的地震引发了能量充沛的三次波(T 波),这些 T 波穿过南太平洋传播到南大西洋,在阿森松岛附近的一个水听器站记录到了这些 T 波,该站距离震中 15127 公里。在地震期间,通过利用三维声传播模型来研究该偏差的原因,确定了 T 波在德雷克海峡的水平绕射。