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Earth Sciences

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William & Mary

2018

Physical Sciences Peer-Reviewed Articles

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Effects Of Marsh Edge Erosion In Coupled Barrier Island-Marsh Systems And Geometric Constraints On Marsh Evolution, Rebecca Lauzon, A Brad Murray, Laura J Moore, David C. Walters, Matthew L. Kirwan, Sergio Fagherazzi, Jun 2018

Effects Of Marsh Edge Erosion In Coupled Barrier Island-Marsh Systems And Geometric Constraints On Marsh Evolution, Rebecca Lauzon, A Brad Murray, Laura J Moore, David C. Walters, Matthew L. Kirwan, Sergio Fagherazzi,

VIMS Articles

Sand washed across barrier islands during storms (called overwash) provides sediment for salt marshes behind those islands, and can allow a marsh which otherwise would drown to grow vertically fast enough to keep up with sea level. We use a barrier island-marsh evolution model (GEOMBEST+) to see what effect marsh edge erosion by waves has on overwash-supported marshes. Consistent with previous research, we find that wave erosion can make marshes more resilient by freeing sediment that can be used elsewhere on the marsh surface. We add that horizontal erosion of the marsh edge provides more sediment per volume eroded than …


Massive Upland To Wetland Conversion Compensated For Historical Marsh Loss In Chesapeake Bay, Usa, Nathalie W. Schieder, David C. Walters, Matthew L. Kirwan Jan 2018

Massive Upland To Wetland Conversion Compensated For Historical Marsh Loss In Chesapeake Bay, Usa, Nathalie W. Schieder, David C. Walters, Matthew L. Kirwan

VIMS Articles

Sea level rise leads to coastal transgression, and the survival of ecosystems depends on their ability to migrate inland faster than they erode and submerge. We compared marsh extent between nineteenth-century maps and modern aerial photographs across the Chesapeake Bay, the largest estuary in North America, and found that Chesapeake marshes have maintained their spatial extent despite relative sea level rise rates that are among the fastest in the world. In the mapped region (i.e., 25% of modern Chesapeake Bay marshland),94 km2of marsh was lost primarily to shoreline erosion,whereas 101 km2of marsh was created by upland drowning.Simple projections over the …