PIE LTER Publications
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The Role of Waves, Shelf Slope, and Sediment Characteristics on the Development of Erosional Chenier Plains. Geophysical Research Letters. 45:8435-8444.. 2018.
Salt marsh erosion rates and boundary features in a shallow Bay. Journal of Geophysical Research: Earth Surface. 121:1861-1875.. 2016.
The Salt Marsh Geomorphology: Physical and Ecological Effects on Landform. AGU Chapman Conference. 86:57-58.. 2004.
Salt marsh geomorphology: Physical and ecological effects on landform. Estuarine, Coastal and Shelf Science. 69:309-310.. 2006.
Salt marsh vegetation promotes efficient tidal channel networks. Nature Communications. 7. 2016.
Sea Level Rise and the Dynamics of the Marsh-Upland Boundary. Frontiers in Environmental Science.. 2019.
Soil creep in a mesotidal salt marsh channel bank: Fast, seasonal,and water table mediated. Geomorphology. 334:126-137.. 2019.
Soil creep in salt marshes. Geology.. 2016.
Spatially integrative metrics reveal hidden vulnerability of microtidal salt marshes. Nature Communications. 8. 2017.
Stage-discharge relationship in tidal channels. Limnology and Oceanography. 15:394-407.. 2017.
Time-dependent behavior of a placed bed of cohesive sediment subjected to erosion and deposition cycles. Ocean Dynamics. 65:287-294.. 2015.
Tradeoffs among hydrodynamics, sedimentfluxes and vegetationcommunity in the Virginia Coast Reserve, USA. Estuarine and Coastal Shelf Science. 210:98-108.. 2018.
Variations in persistence and regenerative zones in coastal forests triggered by sea level rise and storms.. Remote Sensing. 11. 2019.
Velocity skew controls the flushing of a tracer in a system of shallow bays with multiple inlets.. Continental Shelf Research. 192. 2020.