Anthropogenic controls on overwash deposition: Evidence and consequences

被引:61
作者
Rogers, Laura J. [1 ]
Moore, Laura J. [1 ]
Goldstein, Evan B. [1 ]
Hein, Christopher J. [2 ]
Lorenzo-Trueba, Jorge [3 ]
Ashton, Andrew D. [4 ]
机构
[1] Univ N Carolina, Dept Geol Sci, Chapel Hill, NC USA
[2] Virginia Inst Marine Sci, Coll William & Mary, Dept Phys Sci, Gloucester Point, VA 23062 USA
[3] Montclair State Univ, Dept Earth & Environm Studies, Montclair, NJ USA
[4] Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA
关键词
SEA-LEVEL RISE; AIRBORNE TOPOGRAPHIC LIDAR; BARRIER ISLANDS; ATLANTIC COAST; NORTH-CAROLINA; CLIMATE; BEACHES; IMPACTS; SCALE; FIRE;
D O I
10.1002/2015JF003634
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Accelerated sea level rise and the potential for an increase in frequency of the most intense hurricanes due to climate change threaten the vitality and habitability of barrier islands by lowering their relative elevation and altering frequency of overwash. High-density development may further increase island vulnerability by restricting delivery of overwash to the subaerial island. We analyzed pre-Hurricane Sandy and post-Hurricane Sandy (2012) lidar surveys of the New Jersey coast to assess human influence on barrier overwash, comparing natural environments to two developed environments (commercial and residential) using shore-perpendicular topographic profiles. The volumes of overwash delivered to residential and commercial environments are reduced by 40% and 90%, respectively, of that delivered to natural environments. We use this analysis and an exploratory barrier island evolution model to assess long-term impacts of anthropogenic structures. Simulations suggest that natural barrier islands may persist under a range of likely future sea level rise scenarios (7-13mm/yr), whereas developed barrier islands will have a long-term tendency toward drowning.
引用
收藏
页码:2609 / 2624
页数:16
相关论文
共 65 条
[1]  
[Anonymous], 2015, NAT CLIM CHANGE, DOI DOI 10.1038/nclimate2474
[2]  
[Anonymous], 2013, AL182012
[3]   Quantifying overwash flux in barrier systems: An example from Martha's Vineyard, Massachusetts, USA [J].
Carruthers, Emily A. ;
Lane, D. Philip ;
Evans, Rob L. ;
Donnelly, Jeffrey P. ;
Ashton, Andrew D. .
MARINE GEOLOGY, 2013, 343 :15-28
[4]   Investigating the role of complex sandbar morphology on nearshore hydrodynamics [J].
Cohn, N. ;
Ruggiero, P. ;
Ortiz, J. ;
Walstra, D. J. .
JOURNAL OF COASTAL RESEARCH, 2014, :53-58
[5]  
Criss RE, 2001, GEOLOGY, V29, P875, DOI 10.1130/0091-7613(2001)029<0875:FETFC>2.0.CO
[6]  
2
[7]   A numerical model of coastal overwash [J].
Donnelly, C. ;
Larson, M. ;
Hanson, H. .
PROCEEDINGS OF THE INSTITUTION OF CIVIL ENGINEERS-MARITIME ENGINEERING, 2009, 162 (03) :105-114
[8]  
Donnelly C., 2007, Proceedings of Coastal Sediments, V07, P2061, DOI [DOI 10.1061/40926(239)162, 10.1061/40926(239)162.]
[9]   State of knowledge on measurement and modeling of coastal overwash [J].
Donnelly, Chantal ;
Kraus, Nicholas ;
Larson, Magnus .
JOURNAL OF COASTAL RESEARCH, 2006, 22 (04) :965-991
[10]   Downscaling CMIP5 climate models shows increased tropical cyclone activity over the 21st century [J].
Emanuel, Kerry A. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2013, 110 (30) :12219-12224