The new method uses the measurement of acoustic gravity waves (AGWs), which occur naturally and move through the deep ocean at the speed of sound.
When objects hit the sea surface they cause a sudden change in water pressure which leads to the generation of AGWs.
Lead author of the study Dr Usama Kadri, from Cardiff University's School of Mathematics, described it as a "completely novel way of locating objects impacting on the sea surface".
He added: "Tracking these acoustic gravity waves opens up a huge range of possibilities, from locating falling meteorites to detecting landslides, snowslides, storm surges, tsunamis and rogue waves."