ACOUSTIC-GRAVITY WAVES, THEORY & APPLICATIONS

声重力波是一种压缩波，其振幅受重力恢复力的影响。它们是由风浪相互作用、表面波相互作用和构造岩石圈板块运动产生的。它们在水中以音速传播，携带着关于它们来源的信息。利用特设工作组，我们的目标是改善目前的海况预警系统，特别是对海啸的早期检测。

Acoustic-gravity waves (AGWs) are compression-type waves propagating with amplitudes governed by the restoring force of gravity. They are generated, by wind-wave interactions, surface wave interactions, and movements of the tectonic lithosphere plates. They travel at the speed of sound in water carrying information on their source. Employing AWGs we aim to improve current sea-state warning systems with a particular focus on early detection of tsunami.