A new Tulane University study questions the reliability of how sea-level rise in low-lying coastal areas such as southern Louisiana is measured and suggests that the current method underestimates the severity of the problem. This research is the focus of a news article published this week in the journal Science.
Relative sea-level rise, which is a combination of rising water level and subsiding land, is traditionally measured using tide gauges. But researchers Molly Keogh and Torbjörn Törnqvist argue that in coastal Louisiana, tide gauges tell only a part of the story.
Tide gauges in such areas are anchored an average of 20 meters into the earth rather than at the ground surface. “As a result, tide gauges do not record subsidence occurring in the shallow subsurface and thus underestimate rates of relative sea-level rise,” said Keogh, a fifth year PhD student and lead author of the study.
“This study shows that we need to completely rethink how we measure sea-level rise in rapidly subsiding coastal lowlands” said Törnqvist, Vokes Geology Professor in the Tulane School of Science and Engineering.
The study, published in the open-access journal Ocean Science, says that while tide gauges can accurately measure subsidence that occurs below their foundations, they miss out on the shallow subsidence component. With at least 60 percent of subsidence occurring in the top 5 meters of the sediment column, tide gauges are not capturing the primary contributor to relative sea-level rise.