Global distribution of nearshore slopes with implications for coastal retreat

被引:63
作者
Athanasiou, Panagiotis [1 ,2 ]
van Dongeren, Ap [1 ,5 ]
Giardino, Alessio [1 ]
Vousdoukas, Michalis [3 ,4 ]
Gaytan-Aguilar, Sandra [1 ]
Ranasinghe, Roshanka [1 ,2 ,5 ]
机构
[1] Deltares, Delft, Netherlands
[2] Univ Twente, Fac Engn Technol, Water Engn & Management, Enschede, Netherlands
[3] European Commiss, Joint Res Ctr, Ispra, Italy
[4] Univ Aegean, Dept Marine Sci, Mitilini, Greece
[5] IHE Delft Inst Water Educ, Delft, Netherlands
基金
欧盟地平线“2020”;
关键词
SEA-LEVEL RISE; CLIMATE-CHANGE; EROSION; VARIABILITY; UNCERTAINTY; BEACHES; MODEL; TIME;
D O I
10.5194/essd-11-1515-2019
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Nearshore slope, defined as the cross-shore gradient of the subaqueous profile, is an important input parameter which affects hydrodynamic and morphological coastal processes. It is used in both local and large-scale coastal investigations. However, due to unavailability of data, most studies, especially those that focus on continental or global scales, have historically adopted a uniform nearshore slope. This simplifying assumption could however have far-reaching implications for predictions/projections thus obtained. Here, we present the first global dataset of nearshore slopes with a resolution of 1 km at almost 620 000 points along the global coastline. To this end, coastal profiles were constructed using global topo-bathymetric datasets. The results show that the nearshore slopes vary substantially around the world. An assessment of coastline recession driven by sea level rise (SLR) (for an arbitrary 0.5 m SLR) with a globally uniform coastal slope of 1: 100, as carried out in previous studies, and with the spatially variable coastal slopes computed herein shows that, on average, the former approach would underestimate coastline recession by about 40 %, albeit with significant spatial variation. The final dataset has been made publicly available at https://doi .org/10.4121/uuid:a8297dcd-c34e-4e6d-bf66-9fb8913d983d (Athanasiou, 2019).
引用
收藏
页码:1515 / 1529
页数:15
相关论文
共 44 条
[1]   Downscaling Changing Coastlines in a Changing Climate: The Hybrid Approach [J].
Antolinez, Jose Antonio A. ;
Murray, A. Brad ;
Mendez, Fernando J. ;
Moore, Laura J. ;
Farley, Graham ;
Wood, James .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2018, 123 (02) :229-251
[2]  
Athanasiou P, 2019, GLOBAL DISTRIBUTION, DOI [10.4121/uuid:a8297dcd-c34e-4e6d-bf66-9fb8913d983d, DOI 10.4121/UUID:A8297DCD-C34E-4E6D-BF66-9FB8913D983D]
[3]   Erosion consequences on beach functions along the Maresme coast (NW Mediterranean, Spain) [J].
Ballesteros, Caridad ;
Jimenez, Jose A. ;
Valdemoro, Herminia I. ;
Bosom, Eva .
NATURAL HAZARDS, 2018, 90 (01) :173-195
[4]   Development of the Coastal Storm Modeling System (CoSMoS) for predicting the impact of storms on high-energy, active-margin coasts [J].
Barnard, Patrick L. ;
van Ormondt, Maarten ;
Erikson, Li H. ;
Eshleman, Jodi ;
Hapke, Cheryl ;
Ruggiero, Peter ;
Adams, Peter N. ;
Foxgrover, Amy C. .
NATURAL HAZARDS, 2014, 74 (02) :1095-1125
[5]   Incorporating climate change and morphological uncertainty into coastal change hazard assessments [J].
Baron, Heather M. ;
Ruggiero, Peter ;
Wood, Nathan J. ;
Harris, Erica L. ;
Allan, Jonathan ;
Komar, Paul D. ;
Corcoran, Patrick .
NATURAL HAZARDS, 2015, 75 (03) :2081-2102
[6]  
Battjes J. A., 1974, COAST ENG P, V1, P26, DOI [10.9753/icce.v14.26, DOI 10.9753/ICCE.V14.26]
[7]   FIELD DATA ON SEAWARD LIMIT OF PROFILE CHANGE [J].
BIRKEMEIER, WA .
JOURNAL OF WATERWAY PORT COASTAL AND OCEAN ENGINEERING-ASCE, 1985, 111 (03) :598-602
[8]  
Brutsche K. E, 2016, CHETNVI45 ERDCCHL US
[9]  
Bruun P., 1962, J. Waterw. Harb. Div., V88, P117, DOI [10.1061/JWHEAU.0000252, DOI 10.1061/JWHEAU.0000252]
[10]   Sea-level rise and shoreline retreat: time to abandon the Bruun Rule [J].
Cooper, JAG ;
Pilkey, OH .
GLOBAL AND PLANETARY CHANGE, 2004, 43 (3-4) :157-171