It's hard to believe it's been almost one month since Hurricane Isaac reached the Gulf Coast on August 28 -- eerily close to the seventh anniversary of Hurricane Katrina. And while locals and cleanup crews are still hard at work recovering from the damage, national attention has all but moved on.
For the now-destabilized Gulf Coastal wetland ecosystems, a slow-moving hurricane with heavy rain and high, shoreline-pounding surf may be the most damaging type of storm. This is true especially around the mouth of the Mississippi River, which took a direct hit from Hurricane Isaac. The storm surge associated with Hurricane Isaac showed firsthand the devastating effects that a long, slow hurricane has on fragile coastal ecosystems.
The storm surge associated with a hurricane wreaks havoc on the natural world around it, especially on storm-protection buffers provided by nature, which take the form of barrier islands and buffers composed of wetlands and forests between the coast and coastal communities or cities. This powerful surge force topples trees, rips off wetland soils, especially floating mats of wetland vegetation, and introduces saltwater into freshwater wetlands and the soils beneath these wetlands. Salt further destabilizes the muck and peat substrates, contributing to their further decline and collapse.
Many cities in India and other tropical locations learned of the self-inflicted devastation created as mangrove ecosystems were removed for the timber resources and development. New Orleans and other U.S. Gulf Coastal cities need to brace themselves for more intense and further-exacerbated onslaughts from storms as these critical natural barriers are diminished in size and altered in their plant composition and durability -- all of which essentially reduce the effectiveness of the buffers.
Forty-three percent of the lower 48 states are connected to tributaries to the Mississippi River Basin. Currently, there is a coordinated effort over a vast area of the U.S. and a small portion of Canada to reduce nutrient loading and ensure that a balance of coarse sediments to fine sediments enters the Gulf. That means that primarily fine, clay-sized particles stay suspended in the moving river waters, and bigger sand, gravel, and larger soil particles are captured behind dams on the river. Thus, only the finest soil fractions of clay-sized particles with the absorbed nutrients regularly make it to the Gulf. This has to change if we intend to rebuild and protect our natural buffer areas.
In March 2012 I flew over the Gulf Coastal wetlands from Corpus Christi, Texas, to Mobile, Ala. to check out ground conditions. This trip led to some startling observations, some of which were previously unreported and have no doubt worsened since August:
- The storm surge does something more insidious that historically may not have mattered as much. Today, the nutrient-rich fine mud and associated chemically bound agricultural fertilizers from the Mississippi River and other watersheds gets re-suspended from shallow areas, where it has been deposited (for example, off the mouth of the Mississippi and Athachaflaya Rivers). It is then carried by the storm surge into the coastal wetlands, where a blanket of this nutrient-rich mud of varying depths is deposited. In the Gulf these mud and nutrients contribute to the devastating Gulf hypoxia risk occurring annually.
Addressing the decline in the Gulf Coastal ecosystem will require an ecosystem restoration and watershed approach supported by policies and various incentives offered throughout the tributary watersheds. Any restoration approach must also recognize other threats, including the rapid spread of invasive, non-native species. One example of an invasive threat is giant reed canary grass, which has the potential to dismantle entire ecosystems if left unchecked. If recent years are any indication, hurricanes will continue to roar through the Gulf, making a dire situation even worse.
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