@article {8794,
	title = {Recent Acceleration of Wetland Accretion and Carbon Accumulation Along the U.S. East Coast},
	journal = {Earth{\textquoteright}s Future},
	volume = {11151},
	year = {2023},
	month = {Jan-03-2023},
	issn = {2328-4277},
	doi = {10.1029/2022EF003037},
	url = {https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022EF003037https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2022EF003037},
	author = {Weston, Nathaniel B. and Rodriguez, Elise and Donnelly, Brian and Solohin, Elena and Jezycki, Kristen and Demberger, Sandra and Sutter, Lori A. and Morris, James T. and Neubauer, Scott C. and Craft, Christopher B.}
}
@article {alizad_integrated_2022,
	title = {Integrated Modeling of Dynamic Marsh Feedbacks and Evolution Under Sea-Level Rise in a Mesotidal Estuary (Plum Island, MA, USA)},
	journal = {Water Resources Research},
	volume = {58},
	year = {2022},
	pages = {e2022WR032225},
	abstract = {Around the world, wetland vulnerability to sea-level rise (SLR) depends on different factors including tidal regimes, topography, creeks and estuary geometry, sediment availability, vegetation type, etc. The Plum Island estuary (PIE) is a mesotidal wetland system on the east coast of the United States. This research applied a newly updated Hydro-MEM (integrated hydrodynamic-marsh) model to assess the impacts of intermediate-low (50 cm), intermediate (1 m), and intermediate-high (1.5 m) SLR on marsh evolution by the year 2100. Model advancements include capturing vegetation change, inorganic and below and aboveground organic matter portion of marsh platform accretion, and mudflat creation. Although the results indicate a low vulnerability marsh at the PIE, the vegetation changes from high to low marsh under all SLR scenarios (2\%{\textendash}22\%), with the higher bounds belonging to higher rise scenarios. Lower SLR produces more productive marsh (13\% gain in high productivity regions), whereas the highest SLR scenario causes increased tidal inundation, which leads to loss in productivity (12\% change from high to low productivity regions), generation of mudflats (17\% of the domain land), and marsh migration to higher lands. Sensitive nonlinear tidal flow changes, which may be increased or decreased with SLR as a result of mudflat creation, marsh migration, and bottom friction change, emphasize the importance of integrated modeling approaches that include dynamic marsh feedbacks in hydrodynamic modeling and varying hydrodynamic effects on the marsh system.},
	keywords = {hydro-MEM, mesotidal system, salt marsh, sea-level rise},
	issn = {1944-7973},
	doi = {10.1029/2022WR032225},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2022WR032225},
	author = {Alizad, Karim and Morris, James T. and Bilskie, Matthew V. and Passeri, Davina L. and Hagen, Scott C.}
}
@article {tornqvist_coastal_2021,
	title = {Coastal {Wetland} {Resilience}, {Accelerated} {Sea}-{Level} {Rise}, and the {Importance} of {Timescale}},
	journal = {AGU Advances},
	volume = {2},
	number = {1},
	year = {2021},
	month = {mar},
	issn = {2576-604X, 2576-604X},
	doi = {10.1029/2020AV000334},
	url = {https://onlinelibrary.wiley.com/doi/10.1029/2020AV000334},
	author = {T{\"o}rnqvist, Torbj{\"o}rn E. and Cahoon, Donald R. and Morris, James T. and Day, John W.}
}
@article {tornqvist_coastal_2021,
	title = {Coastal Wetland Resilience, Accelerated Sea-Level Rise, and the Importance of Timescale},
	journal = {AGU Advances},
	volume = {2},
	year = {2021},
	pages = {e2020AV000334},
	abstract = {Recent studies have produced conflicting results as to whether coastal wetlands can keep up with present-day and future sea-level rise. The stratigraphic record shows that threshold rates for coastal wetland submergence or retreat are lower than what instrumental records suggest, with wetland extent that shrinks considerably under high rates of sea-level rise. These apparent conflicts can be reconciled by recognizing that many coastal wetlands still possess sufficient elevation capital to cope with sea-level rise, and that processes like sediment compaction, ponding, and wave erosion require multidecadal or longer timescales to drive wetland loss that is in many cases inevitable.},
	keywords = {coastal wetlands, sea-level rise},
	issn = {2576-604X},
	doi = {10.1029/2020AV000334},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1029/2020AV000334},
	author = {T{\"o}rnqvist, Torbj{\"o}rn E. and Cahoon, Donald R. and Morris, James T. and Day, John W.}
}
@article {cahoon_how_2021,
	title = {How {Plants} {Influence} {Resilience} of {Salt} {Marsh} and {Mangrove} {Wetlands} to {Sea}-{Level} {Rise}},
	journal = {Estuaries and Coasts},
	volume = {44},
	number = {4},
	year = {2021},
	month = {jun},
	pages = {883{\textendash}898},
	issn = {1559-2723, 1559-2731},
	doi = {10.1007/s12237-020-00834-w},
	url = {https://link.springer.com/10.1007/s12237-020-00834-w},
	author = {Cahoon, Donald R. and McKee, Karen L. and Morris, James T.}
}
@inbook {morris_marsh_2021,
	title = {Marsh Equilibrium Theory: Implications for Responses to Rising Sea Level},
	booktitle = {Salt Marshes: Function, Dynamics, and Stresses},
	year = {2021},
	pages = {157{\textendash}177},
	publisher = {Cambridge University Press},
	organization = {Cambridge University Press},
	address = {Cambridge},
	abstract = {The analysis presented here was motivated by an objective of describing the interactions between the physical and biological processes governing the responses of tidal wetlands to rising sea level and the ensuing equilibrium elevation. We define equilibrium here as meaning that the elevation of the vegetated surface relative to mean sea level (MSL) remains within the vertical range of tolerance of the vegetation on decadal time scales or longer. The equilibrium is dynamic, and constantly responding to short-term changes in hydrodynamics, sediment supply, and primary productivity. For equilibrium to occur, the magnitude of vertical accretion must be great enough to compensate for change in the rate of sea-level rise (SLR). SLR is defined here as meaning the local rate relative to a benchmark, typically a gauge. Equilibrium is not a given, and SLR can exceed the capacity of a wetland to accrete vertically.},
	isbn = {9781107186286},
	doi = {10.1017/9781316888933.009},
	url = {https://www.cambridge.org/core/books/salt-marshes/marsh-equilibrium-theory/DA7B5EFE9C8CE403EF2190CC60D968EF},
	author = {Morris, James T. and Cahoon, Donald R. and Callaway, John C. and Craft, Christopher and Neubauer, Scott C. and Weston, Nathaniel B.},
	editor = {FitzGerald, Duncan M. and Hughes, Zoe J.}
}
@article {morris_tidal_2020,
	title = {Tidal and {Hurricane} {Impacts} on {Saltmarshes} in the {Northeastern} {Coastal} and {Barrier} {Network}: {Theory} and {Empirical} {Results}},
	journal = {Estuaries and Coasts},
	volume = {43},
	number = {7},
	year = {2020},
	month = {nov},
	pages = {1658{\textendash}1671},
	issn = {1559-2723, 1559-2731},
	doi = {10.1007/s12237-020-00790-5},
	url = {https://link.springer.com/10.1007/s12237-020-00790-5},
	author = {Morris, James T. and Lynch, James and Renken, Katherine A. and Stevens, Sara and Tyrrell, Megan and Plaisted, Holly}
}
@article {bortolus_supporting_2019,
	title = {Supporting \textit{{Spartina}} : {Interdisciplinary} perspective shows \textit{{Spartina}} as a distinct solid genus},
	journal = {Ecology},
	volume = {100},
	number = {11},
	year = {2019},
	issn = {0012-9658, 1939-9170},
	doi = {10.1002/ecy.2863},
	url = {https://onlinelibrary.wiley.com/doi/10.1002/ecy.2863},
	author = {Bortolus, Alejandro and Adam, Paul and Adams, Janine B. and Ainouche, Malika L. and Ayres, Debra and Bertness, Mark D. and Bouma, Tjeerd J. and Bruno, John F. and Ca{\c c}ador, Isabel and Carlton, James T. and Castillo, Jesus M. and Costa, Cesar S. B. and Davy, Anthony J. and Deegan, Linda and Duarte, Bernardo and Figueroa, Enrique and Gerwein, Joel and Gray, Alan J. and Grosholz, Edwin D. and Hacker, Sally D. and Hughes, A. Randall and Mateos-Naranjo, Enrique and Mendelssohn, Irving A. and Morris, James T. and Mu{\~n}oz-Rodr{\'\i}guez, Adolfo F. and Nieva, Francisco J. J. and Levin, Lisa A. and Li, Bo and Liu, Wenwen and Pennings, Steven C. and Pickart, Andrea and Redondo-G{\'o}mez, Susana and Richardson, David M. and Salmon, Armel and Schwindt, Evangelina and Silliman, Brian R. and Sotka, Erik E. and Stace, Clive and Sytsma, Mark and Temmerman, Stijn and Turner, R. Eugene and Valiela, Ivan and Weinstein, Michael P. and Weis, Judith S.}
}
