David is a biological science tech with the Eastern Ecological Science Center at the Patuxent Research Refuge in Laurel, MD
David is a wetland ecologist, researching how coastal wetlands respond to sea level rise. With a background in biological and physical sciences, his work focuses on the interaction between wetland plant species and their physical environment.
Professional Experience
2020-Present - U.S. Geological Survey, Eastern Ecological Science Center, Biologist, Coastal Wetlands Group
2017-2020 - NSA Contractor with U.S. Geological Survey, Patuxent Wildlife Research Refuge, Coastal Wetlands Group
2013-2017 - Virginia Institute of Marine Science, Laboratory and Research Specialist
Education and Certifications
M.S., University of North Carolina- Chapel Hill, Geology (2013)
B.S., Longwood Univerity, Biology, concentration in Ecology (2011)
Science and Products
Minerals Science Team
Climate-driven tradeoffs between landscape connectivity and the maintenance of the coastal carbon sink
GPS data from 2019 and 2020 campaigns in the Chesapeake Bay region towards quantifying vertical land motions
Experimental tree mortality does not induce marsh transgression in a Chesapeake Bay low-lying coastal forest
Sea level driven marsh expansion in a coupled model of marsh erosion and migration
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
Minerals Science Team
The Minerals Integrated Science Team focuses on contaminant exposures in the environment that might originate from mineral resource activities including, transportation, storage, extraction and waste management. Perceived health risks to humans and other organisms will be distinguished from actual risks, if any. If actual risks are identified the science produced by this team can inform how to... - Multimedia
- Publications
Climate-driven tradeoffs between landscape connectivity and the maintenance of the coastal carbon sink
Ecosystem connectivity tends to increase the resilience and function of ecosystems responding to stressors. Coastal ecosystems sequester disproportionately large amounts of carbon, but rapid exchange of water, nutrients, and sediment makes them vulnerable to sea level rise and coastal erosion. Individual components of the coastal landscape (i.e., marsh, forest, bay) have contrasting responses to sAuthorsKendall Valentine, Ellen R. Herbert, David C Walters, Yaping Chen, Alexander J. Smith, Matthew L. KirwanGPS data from 2019 and 2020 campaigns in the Chesapeake Bay region towards quantifying vertical land motions
The Chesapeake Bay is a region along the eastern coast of the United States where sea-level rise is confounded with poorly resolved rates of land subsidence, thus new constraints on vertical land motions (VLM) in the region are warranted. In this paper, we provide a description of two campaign-style Global Positioning System (GPS) datasets, explain the methods used in data collection and validatioAuthorsGabrielle Troia, Sarah Stamps, R. Russell Lotspeich, James M. Duda, Kurt J. McCoy, William Moore, Philippe Hensel, Ryan Hippenstiel, Thomas McKenna, David C. Andreasen, Charles Geoghegan, Thomas P Ulizo, Madeline Kronebusch, Joel A. Carr, David Walters, Neil WinnExperimental tree mortality does not induce marsh transgression in a Chesapeake Bay low-lying coastal forest
Transgression into adjacent uplands is an important global response of coastal wetlands to accelerated rates of sea level rise. “Ghost forests” mark a signature characteristic of marsh transgression on the landscape, as changes in tidal inundation and salinity cause bordering upland tree mortality, increase light availability, and the emergence of tidal marsh species due to reduced competition. ToAuthorsDavid C Walters, Joel A. Carr, Alyssa Hockaday, Joshua A Jones, Eliza McFarland, Katya Kovalenko, Matthew L. Kirwan, Donald Cahoon, Glenn R. GuntenspergenSea level driven marsh expansion in a coupled model of marsh erosion and migration
Coastal wetlands are among the most valuable ecosystems on Earth, where ecosystem services such as flood protection depend nonlinearly on wetland size and are threatened by sea level rise and coastal development. Here we propose a simple model of marsh migration into adjacent uplands and couple it with existing models of seaward edge erosion and vertical soil accretion to explore how ecosystem conAuthorsMatthew L. Kirwan, David C. Walters, William G. Reay, Joel A. CarrNon-USGS Publications**
Lauzon, R., Murray, A. B., Moore, L. J., Walters, D. C., Kirwan, M. L., & Fagherazzi, S. (2018). Effects of marsh edge erosion in coupled barrier island-marsh systems and geometric constraints on marsh evolution. Journal of Geophysical Research: Earth Surface, 123, 1218– 1234. https://doi.org/10.1029/2017JF004530Moore, L.J. et al. (2018). The Role of Ecomorphodynamic Feedbacks and Landscape Couplings in Influencing the Response of Barriers to Changing Climate. In: Moore, L., Murray, A. (eds) Barrier Dynamics and Response to Changing Climate. Springer, Cham. https://doi.org/10.1007/978-3-319-68086-6_10Schieder, N.W., Walters, D.C. & Kirwan, M.L. Massive Upland to Wetland Conversion Compensated for Historical Marsh Loss in Chesapeake Bay, USA. Estuaries and Coasts 41, 940–951 (2018). https://doi.org/10.1007/s12237-017-0336-9Walters, D.C. & M.L. Kirwan, Optimal hurricane overwash thickness for maximizing marsh resilience to sea level rise, Ecology and Evolution (2016). https://onlinelibrary.wiley.com/doi/10.1002/ece3.2024Moore, L.J., Walters, D.C., et al., Ecomorphodynamic feedbacks and couplings between landscape units affect barrier island response to changing climate. In: Coastal Sediments, (2015). https://www.worldscientific.com/doi/10.1142/9789814689977_0246Walters, D., et al., Interactions between barrier islands and backbarrier marshes affect island system response to sea level rise: Insights from a coupled model, Journal of Geophysical Research: Earth Surface, (2014). https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014JF003091**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.