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Optimal Hurricane Overwash Thickness for Maximizing Marsh Resilience to Sea Level Rise W&M ScholarWorks VIMS Articles Virginia Institute of Marine Science 2016 Optimal hurricane overwash thickness for maximizing marsh resilience to sea level rise David C. Walters Virginia Institute of Marine Science Matthew L. Kirwan Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/vimsarticles Part of the Marine Biology Commons Recommended Citation Walters, D. C. and Kirwan, M. L. (2016), Optimal hurricane overwash thickness for maximizing marsh resilience to sea level rise. Ecol Evol, 6: 2948–2956. doi:10.1002/ece3.2024 This Article is brought to you for free and open access by the Virginia Institute of Marine Science at W&M ScholarWorks. It has been accepted for inclusion in VIMS Articles by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Optimal hurricane overwash thickness for maximizing marsh resilience to sea level rise David C. Walters & Matthew L. Kirwan Department of Physical Sciences, Virginia Institute of Marine Science, College of William and Mary, PO Box 1346, Gloucester Point, Virginia 23062 Keywords Abstract Climate change, coastal geomorphology, disturbance event, ecosystem resiliency, press The interplay between storms and sea level rise, and between ecology and sedi- and pulse stresses, salt marsh, storm ment transport governs the behavior of rapidly evolving coastal ecosystems such deposition. as marshes and barrier islands. Sediment deposition during hurricanes is thought to increase the resilience of salt marshes to sea level rise by increasing Correspondence soil elevation and vegetation productivity. We use mesocosms to simulate burial David C. Walters, Department of Physical of Spartina alterniflora during hurricane-induced overwash events of various Sciences, Virginia Institute of Marine Science, thickness (0–60 cm), and find that adventitious root growth within the over- College of William and Mary, PO Box 1386, Gloucester Point, VA 23062. wash sediment layer increases total biomass by up to 120%. In contrast to most Tel: (804) 684-7131; previous work illustrating a simple positive relationship between burial depth Fax: (804) 684-7250; and vegetation productivity, our work reveals an optimum burial depth (5– E-mail: [email protected] 10 cm) beyond which burial leads to plant mortality. The optimum burial depth increases with flooding frequency, indicating that storm deposition ame- Funding Information liorates flooding stress, and that its impact on productivity will become more This work was supported by NSF LTER important under accelerated sea level rise. Our results suggest that frequent, #1237733, NSF Coastal SEES #1426981. low magnitude storm events associated with naturally migrating islands may Received: 16 November 2015; Revised: 7 increase the resilience of marshes to sea level rise, and in turn, slow island January 2016; Accepted: 23 January 2016 migration rates. Synthesis: We find that burial deeper than the optimum results in reduced growth or mortality of marsh vegetation, which suggests that future Ecology and Evolution 2016; 6(9): 2948– increases in overwash thickness associated with more intense storms and artifi- 2956 cial heightening of dunes could lead to less resilient marshes. doi: 10.1002/ece3.2024 Introduction from storms. Including storm protection, recent work val- ues ecosystem services provided by marshes at $10,000/ha Ecosystem resiliency is determined by responses to a com- (Barbier and Hacker 2011). Human populations on bar- bination of long-term press and short-term pulse distur- rier islands are more dense than in their mainland states bances. The interplay can be complex, where pulse (Zhang and Leatherman 2011) and have grown at an disturbances can either accelerate ecosystem change, or accelerated rate that is faster than the rest of the nation else enhance resiliency to long-term stresses. Coastal (Culliton 1998). As low-lying coastal landforms, climate ecosystems such as barrier islands and salt marshes face change threatens barrier-marsh systems, including the both long-term stresses associated with sea level rise that effects of sea level rise (Sallenger et al. 2012; IPCC 2014) threaten to drown low-lying coastal landscapes, as well as and storms (Bender et al. 2010). The response of barrier short-term disturbances from storms that result in pulses island systems to climate change is also closely linked to of inundation, erosion, and deposition. Climate change is human impacts (McNamara et al. 2011; Kirwan and projected to increase hurricane intensity as well as the Megonigal 2013), through processes such as shoreline rate of sea level rise (Vermeer and Rahmstorf 2009; IPCC hardening and artificial dune-building which alter natural 2014), making the interplay between these drivers com- sedimentation processes. This creates a two-way coupling plex and important to landscape evolution and ecosystem whereby human behavior in response to coastal flooding function. and erosion can reduce ecosystem resiliency, thus dimin- Barrier islands and the marshes behind them play an ishing the very ecosystem services that protect the human important role in protecting valuable coastal property systems from flooding and erosion. 2948 ª 2016 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. D. C. Walters & M. L. Kirwan Optimal Hurricane Overwash Thickness Traditional approaches study the response of barrier climate change will influence the coupled marsh-barrier islands and marshes to climate change separately. How- system. We find that shallow burial leads to enhanced ever, recent numerical modeling proposes a fundamental plant productivity, but that deep burial leads to reduced coupling between the behavior of marshes and barriers growth and mortality, so that subtle changes in the fre- (Lorenzo-Trueba and Ashton 2014; Walters et al. 2014). quency and magnitude of hurricane overwash will For example, backbarrier fringe marshes provide a plat- impact the resilience of marshes and barrier islands to form for barrier islands to migrate over that reduces the long-term sea level rise. rate of island migration, while sand from the island helps to maintain narrow fringe marshes under condi- Materials and Methods tions of suspended sediment supply and sea level rise that they would otherwise not be able to survive (Wal- Site description ters et al. 2014). Overwash, the transport of sand from the beach and dune to the backbarrier environment dur- We measured the response of marsh productivity to bur- ing storms, is the key process that links barrier islands ial by experimental overwash at Hog Island, Virginia and marshes. While episodic overwash provides an (USA) (Fig. 1). Hog Island is part of the VCR (Virginia important source of sediment to build the backbarrier Coast Reserve), an approximately 150 km barrier island vertically (Dolan and Godfrey 1973), burial can also lead coastline that evolves largely without human alteration. À to plant mortality and decades-long recovery (Osgood Local relative sea level rise rates exceed 3.0 mm year 1, et al. 1995; Wang and Horwitz 2007). Although storms where land subsidence and proximity to the Gulf Stream typically deposit sediment on marshes (Cahoon 2006; result in a mid-Atlantic hot spot of accelerated sea level Tweel and Turner 2012), they can also cause substantial rise (Sallenger et al. 2012). Overwash of nutrient poor erosion (Cahoon 2006; Nikitina et al. 2014). Alterna- barrier island sand frequently buries adjacent tidal tively, the subsidy of sediment provided by overwash marshes and, in some cases, leads to vegetation mortality could add nutrients and help stave off the negative and re-establishment that resembles primary succession impacts of sea level rise on backbarrier marsh vegeta- (Osgood et al. 1995). Our experiments are located in or tion, thus leading to enhanced productivity (Men- near a backbarrier fringe marsh that developed on an delssohn and Kuhn 2003). Here, we study the impact of overwash fan associated with a storm in 1962 (Walsh experimental hurricane overwash on marsh plant growth 1998), and immediately adjacent to long-term marsh bio- along an inundation gradient representative of sea level mass sampling sites associated with the VCR Long Term rise in an effort to understand how interacting facets of Ecological Research site (Fig. 1C). (A) Figure 1. (A) Location of Hog Island study site on the Atlantic coast of Virginia (USA). (B) Google Earth photography illustrates extensive marsh behind a sandy barrier island with vegetated dunes and (C) the location of experimental plots relative to long-term end of (B) (C) year biomasssampling transects. ª 2016 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd. 2949 Optimal Hurricane Overwash Thickness D. C. Walters & M. L. Kirwan To explore the combined influences of overwash and wooden stakes so that approximately 1 cm of the bucket sea level rise, we conducted our experiment at a pair of was buried below the marsh surface, thus varying the low and high elevation marsh sites that are subject to dif- height of the bucket above the surface (Fig. 2). Experi- ferent periods of tidal inundation and different rates of ments began prior to the growing season in March, ambient plant productivity. Solinst Levelogger © pressure 2014 to simulate
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