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c 2017 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access
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article distributed under the terms and conditions of the Creative Commons Attribution
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(CC BY) license (http://creativecommons.org/licenses/by/4.0/).
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Journal of
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Marine Science
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and Engineering
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Article
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South Florida’s Encroachment of the Sea and
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Environmental Transformation over the 21st Century
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Joseph Park 1,*
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ID , Erik Stabenau 1 ID , Jed Redwine 2 ID and Kevin Kotun 1
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1 Physical Resources, South Florida Natural Resources Center, National Park Service, Homestead, FL 33030,
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USA; Erik_Stabenau@nps.gov (E.S.); Kevin_Kotun@nps.gov (K.K.)
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2 Biological Resources, South Florida Natural Resources Center, National Park Service, Homestead, FL 33030,
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USA; Jed_Redwine@nps.gov
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* Correspondence: Joseph_Park@nps.gov; Tel.: +1-305-224-4250
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Received: 12 April 2017; Accepted: 18 July 2017; Published: 28 July 2017
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Abstract: South Florida encompasses a dynamic confluence of urban and natural ecosystems strongly
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connected to ocean and freshwater hydrologic forcings. Low land elevation, flat topography and
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highly transmissive aquifers place both communities at the nexus of environmental and ecological
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transformation driven by rising sea level. Based on a local sea level rise projection, we examine
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regional inundation impacts and employ hydrographic records in Florida Bay and the southern
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Everglades to assess water level exceedance dynamics and landscape-relevant tipping points. Intrinsic
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mode functions of water levels across the coastal interface are used to gauge the relative influence and
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time-varying transformation potential of estuarine and freshwater marshes into a marine-dominated
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environment with the introduction of a Marsh-to-Ocean transformation index (MOI).
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Keywords: South Florida; sea level rise; inundation; coastal impacts; water level exceedance
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1. Introduction
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Sea level rise is not evenly distributed around the globe, and the response of a regional coastline
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is highly dependent on local natural and human settings [1]. This is particularly evident at the
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southern end of the Florida peninsula where low elevations and exceedingly flat topography provide
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