Coastal Resiliency: SET Up for the Future

Posted Fri, 09/21/2018 - 12:22
By Taryn Sudol, Maryland Sea Grant

Taryn Sudol is the coordinator for the Chesapeake Bay Sentinel Site Cooperative at Maryland Sea Grant. In her blog, Taryn describes the process of collecting surface elevation table (SET) measurements — an important indicator of changing shorelines and sea level rise. Data such as this offers a baseline to refer to for both response and restoration, during and after disasters. Find out more by visiting Maryland Sea Grant.

A photo of a marsh.
Phillips Creek Marsh sits on the eastern side of the Delmarva Peninsula in Virginia within Chesapeake Bay — the largest estuary in North America. Image credit: Maryland Sea Grant.

Phillips Creek Marsh lies on the eastern seaside stretch of the Delmarva Peninsula in Virginia. The marsh is a swath of wetland grasses with patches of reeds and warped remnants of a boardwalk. Pines fringe the marsh, and a flock of seabirds socialize on a distant mudflat to the southeast.

On this Thursday in mid-May, the sky was an overcast, milky blue. The setting certainly beat my usual office window view of a parking lot. That morning, I took my first squishy steps into a marsh where I would help with the Virginia Coast Reserve Long Term Ecological Research annual surface elevation table (SET) measurements. Similar measurements are made in hundreds of marshes around the world including many in the Chesapeake Bay region by Chesapeake Bay Sentinel Site Cooperative members.

A person's feet in boots walking through a marsh.
Image credit: Maryland Sea Grant.

In simplest terms, marshes are the boundaries between terrestrial and aquatic environments; a soggy confusion of the two. Marshes generally are saturated with water and are classified as either tidal or non-tidal, and by the source of water (fresh-, brackish-, salt-water), position in the landscape (coastal, riverine, deltaic), and the type of vegetation. The possible combinations of these characteristics lead to a wide range of marsh types, many of which are found within the Chesapeake Bay — the largest estuary in North America.

Regardless of marsh type, common threats to all of them include development, invasive species, erosion, and, most prominently, sea level rise. We need to keep marshes. When we lose them, we lose wildlife habitat, our capability to store carbon, our ability to filter pollutants, and provide protection from storm surges.

The Chesapeake Bay Sentinel Site Cooperative will bring together scientists, land managers, regulators, and other practitioners in Virginia and Maryland to discuss these threats and to devise adaptation strategies at a Marsh Resilience Summit in February 2019 at the Virginia Institute of Marine Science. We hope that collectively discussing the changes we are seeing will help us devise solutions.

The measurements of marsh surface elevations we are making at Phillips Creek Marsh will provide valuable information about how this marsh responds to increasing sea levels. Phillips Creek Marsh is a saltmarsh dominated by saltmarsh cordgrass (Spartina alterniflora). The marsh’s unique location, hydrology, vegetation density, and the surrounding environment impact the marsh’s surface elevation. When the results of these measurements are compared with those made in other types of marsh by Chesapeake Bay Sentinel Site Cooperative members, scientists may learn how to manage marshes to slow their loss to increasing sea levels and help to preserve the important services provided by Chesapeake Bay marshes.  

I’m one of a dozen helpers who have gathered around wetland microbiologists, Linda Blum (University of Virginia) and Bob Christian (East Carolina University). They have been consistently monitoring Phillips Creek Marsh for the past 21 years. Very few, if any, sites can beat this monitoring record in the U.S.  — it may be one of the longest records in the world. After these two decades, Blum is ready to delicately pass the baton to the next generation of wetland scientists, Keryn Gedan, a wetland ecologist at George Washington University, and Cora Johnston, the new site director for Anheuser Busch Coastal Research Center.

We tromp through the grass and mud until we are told to stop and come no further. Each surface elevation table is framed with wooden posts and planks. In the center is a benchmark, a pipe that has been driven deep into the ground. This benchmark should not move. However, the marsh around it might grow taller or sink down. A SET precisely measures the elevation of the marsh in millimeters.

A group of people standing in a marsh.
Scientists are investigating one of the oldest marshes, with a baseline of measurements to get a handle on what the future might bring. Marshes are a defining feature of estuaries. Image credit: Maryland Sea Grant. 

We learn about marsh elevation when we measure the SET pin height. The SET is a metal arm that attaches to the benchmark; the arm holds nine pins in place. The benchmark and arm are locked into the same place every time. Then, researchers lower pins to the marsh’s surface and measure the height above the arm. The higher the number over time, the more the marsh has gained in elevation.

Over many years, we may observe centimeters’ worth of change. Marshes gain height through new sediment deposits or added organic matter such as plant roots. Marshes lose height through erosion, decomposition, or soil compaction. If a marsh is gaining, it may be able to withstand sea level rise. If a marsh is sinking, sea level rise will cause it to be underwater longer and the land may transition into mudflats or open water. Blum’s and Christian’s work, which is duplicated throughout the Sentinel Site Cooperatives, gives us insight into whether marshes will survive with changing conditions.

While the concept is simple enough, performing the measurement requires precision, since millimeters make all the difference. You can’t get near the SET; otherwise we might be measuring your footprints. The scientists stand, sit, or lay on planks in order to do SET measurements — careful not to touch the ground. Putting the pin on the surface of the marsh is not as easy as it sounds. Sometimes, it’s like navigating through pea soup. Sometimes, sharp reeds surround your face. Two people could measure the same spot and come up with a different number, so it’s important that the same person measure the SET every time. The helpers are there to note the SET arm’s compass orientation, record the measurements, and carry planks to rest on between the sites.

My team has 11 SET sites to measure. It takes us between four and five hours with birds cawing overhead and flies buzzing much closer. I wonder with every step I take if this time I will fall in the mud (I don’t! Whoohoo!). Blum and Christian traverse the marsh visiting and helping the two teams. You can tell they know the marsh like the back of their hands and have seen it grow in and shift in a way imperceptible to most people.

I consider myself lucky to learn this story for at least one day in the marsh. My hope is this new generation will continue to learn and watch Phillips Creek for another 20 years and then they, too, will pass the baton.

Coastal Resiliency: SET Up for the Future

Posted Fri, 09/21/2018 - 12:22

Anonymous

Fri, 09/21/2018 - 18:37

I had often wondered how surface elevation in marshes, or close to water generally, could be measured precisely. Now I have a better idea. Thanks!

robert edward darrow

Mon, 10/15/2018 - 08:10

As hurricanes pick up energy from the warmer water, what if tons of ice are dropped into the hurricane early in the formation of the eye. This would take away the energy from the hurricane and stop it from growing. If there are about a dozen named hurricanes per year and it cost $ 1,000,000 to drop enough ice on each one, the total cost would be $ 12,000,000, which would be a huge cost savings over having hurricanes hitting land in the USA.

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