Texas A&M Galveston professor warns of beach erosion from Harvey
Hurricane Harvey left its mark on much of the Texas coast, leaving at least $100 billion in damages, but it very likely worsened a problem that has been plaguing the coast for years – beach erosion. How much erosion occurred is still being determined, says a Texas A&M University at Galveston expert.
Jens Figlus, assistant professor of ocean engineering at Texas A&M Galveston, says the question of how much beach erosion occurred may be hard to answer because erosion always goes hand-in-hand with deposition somewhere else.
There’s no doubt that beach erosion in Texas, as in numerous other U.S. locations, is a huge problem. Studies show that about 64 percent of the Texas coast is eroding at an average rate of 6 feet per year, but some areas are losing more than 20 feet per year. On average, the Texas coast is losing about 2.3 feet a year to erosion.
That presents obvious problems. In America, people like to live near the water: according to the Environmental Protection Agency, of the 25 most densely populated U.S. counties, 23 of them are near a coast.
“If we take the whole coastal system (the parts you can see once the water recedes like the beaches, dunes, and back-barrier areas, as well as the parts you cannot see under the water) most likely Harvey caused some areas to loose sediment and others to gain,” says Figlus.
“The question is, where is sediment lost and where is sediment gained?”
“The impacts from Harvey on the Texas coast in terms of coastal erosion most likely vary dramatically by proximity to landfall location. Near the location of landfall, I expect to see a lot more dune over wash, breaching and erosion, whereas the central and upper Texas coast (closer to Galveston) experienced mostly accretion on the beach portions that are normally above the water. Every storm has its own characteristics and results on coastal morphology. Harvey produced fairly large offshore waves but relatively little storm surge – especially further away from the landfall location.”
“What that means is that the storm waves did not have enough water to ‘ride in’ closer to the coast before breaking and dissipating that energy as they erode sediment. Essentially, as we move further away from the landfall location, the waves would break further offshore, erode sediment there and carry it onshore to be deposited on the beach.”
“As I said, every storm is unique and there is no easy estimate for erosion without detailed reconnaissance investigations,” he adds.