Tsunami Sensor Installation on Barro Colorado Island, 2006
An unusual signal has been detected by the seismic monitoring station at the Smithsonian Tropical Research Institute's research facility on Barro Colorado Island. J. McMillan

An unusual signal has been detected by the seismic monitoring station at the Smithsonian Tropical Research Institute's research facility on Barro Colorado Island.

Scientists say the signal results are from waves in Lake Gatun, the reservoir that forms the Panama Canal channel.

Barro Colorado Island is a hilltop that was isolated by the waters of the reservoir created when the Chagres River was dammed to form Lake Gatun, a critical part of the Panama Canal.

Scientists noticed that sensors on Barro Colorado recorded an intriguing wave pattern at an intermediate frequency. They suspected that this pattern could be caused by standing waves in Lake Gatun.

Standing waves, also known as seiches, are common in enclosed bodies of water like lakes and harbors where waves moving in opposite directions interact. By installing a water-level detection meter along the shoreline, researchers confirmed that changes in the water level of the lake correspond to the unusual seismic signal.

This is not the first report of seiches in Lake Gatun. Earlier reports correlated the release of methane gasses in the sediments below the canal to seiches and bottom currents in the lake. The Panama Canal Authority provided data about the depth of the Canal channel and of Lake Gatun that the authors used to model wave patterns in the lake.

Boat traffic and wind speed correlate with the unusual wave pattern, which was more common during the day than it was at night, but more information is needed to confirm what is actually causing the waves.

The seismic sensor was installed on Barro Colorado Island as installed in 2006 as part of a $37.5 million U.S. presidential initiative to improve earthquake monitoring following the devastating tsunami in the Indian Ocean in 2004. The sensor is one of more than 150 sensors that comprise the U.S. Geological Survey's Global Seismographic Network.

Understanding seismic background signals leads to improved earthquake and tsunami detection in the Caribbean region where 100 tsunamis have been reported in the past 500 years.