PIE LTER Publications
Repeated erosion of cohesive sediments with biofilms. Advances in Geosciences. 39:9-14.
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2014. The Role of Waves, Shelf Slope, and Sediment Characteristics on the Development of Erosional Chenier Plains. Geophysical Research Letters. 45:8435-8444.
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2018. Salt marsh erosion rates and boundary features in a shallow Bay. Journal of Geophysical Research: Earth Surface. 121:1861-1875.
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2016. Salt marsh geomorphology: Physical and ecological effects on landform. Estuarine, Coastal and Shelf Science. 69:309-310.
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2006. Salt marsh vegetation promotes efficient tidal channel networks. Nature Communications. 7
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2016. Sea Level Rise and the Dynamics of the Marsh-Upland Boundary. Frontiers in Environmental Science.
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2019. Soil creep in a mesotidal salt marsh channel bank: Fast, seasonal,and water table mediated. Geomorphology. 334:126-137.
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2019. Soil creep in salt marshes. Geology.
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2016. Spatially integrative metrics reveal hidden vulnerability of microtidal salt marshes. Nature Communications. 8
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2017. Stage-discharge relationship in tidal channels. Limnology and Oceanography. 15:394-407.
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2017. Time-dependent behavior of a placed bed of cohesive sediment subjected to erosion and deposition cycles. Ocean Dynamics. 65:287-294.
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2015. Tradeoffs among hydrodynamics, sedimentfluxes and vegetationcommunity in the Virginia Coast Reserve, USA. Estuarine and Coastal Shelf Science. 210:98-108.
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2018. Variations in persistence and regenerative zones in coastal forests triggered by sea level rise and storms.. Remote Sensing. 11
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2019. Velocity skew controls the flushing of a tracer in a system of shallow bays with multiple inlets.. Continental Shelf Research. 192
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2020.