A Coastal Susceptibility Index Assessment of KwaZulu-Natal, East Coast of South Africa

The KwaZulu-Natal coastline on the east coast of South Africa is one of the most densely populated coastlines in Africa and has been subjected to human developments over the last 18 years. In recent years, extreme coastal events, due to a rapidly changing climate have caused much damage along the coast and are predicted to increase in intensity and frequency with the rise in eustatic sea-level. Therefore, assessing the coastal susceptibility in KwaZulu-Natal (KZN) attempts to identify the most sensitive locations along the coast to anticipated sea-level rise and related coastal hazards. This study discusses the application of the Coastal Susceptibility Index, which incorporates and ranks six physical variables, namely: geomorphology, coastal slope, historical shoreline change rate, significant wave height, mean tide range, and relative sea-level rise, to calculate the CSI. This information was displayed based on quartiles, indicating sections of the coastline with a very high, high, moderate or low susceptibility. The majority (34.33%) of the studied KZN is ranked as high susceptibility. More than half the coast (56.72%) is characterized as highly and very highly sensitive, primarily due to the susceptible geological landforms, low lying topography, high erosion rates and a highly significant wave height. The study provides a framework for decision-makers to prioritize coastal zones that require enhanced natural resilience and adopt appropriate management strategies within the study area.

[1]  E. Robert Thieler,et al.  The Digital Shoreline Analysis System (DSAS) Version 4.0 - An ArcGIS extension for calculating shoreline change , 2009 .

[2]  A. Smith,et al.  Coastal dynamics on a soft coastline from serendipitous webcams: KwaZulu-Natal, South Africa , 2014 .

[3]  A. Mather,et al.  A Perspective on Sea Level Rise and Coastal Storm Surge from Southern and Eastern Africa: A Case Study Near Durban, South Africa , 2012 .

[4]  A. Smith,et al.  Combined marine storm and Saros spring high tide erosion events along the KwaZulu-Natal coast in March 2007 , 2007 .

[5]  J. Cooper Geomorphological variability among microtidal estuaries from the wave-dominated South African coast , 2001 .

[6]  C. Musekiwa,et al.  An assessment of coastal vulnerability for the South African coast , 2015 .

[7]  E. Robert Thieler,et al.  National assessment of coastal vulnerability to sea-level rise; U.S. Atlantic Coast , 1999 .

[8]  W. Davies Applying a Coastal Vulnerability Index (CVI) to the Westfjords, Iceland : a preliminary assessment , 2012 .

[9]  P. E. Dunaiski,et al.  The effect of parameters on the end buffer impact force history of the crane : technical paper , 2012 .

[10]  A. Smith,et al.  Forecasting cyclic coastal erosion on a multi-annual to multi-decadal scale: Southeast African coast , 2014 .

[11]  A. Mather,et al.  Southern African sea levels: corrections, influences and trends , 2009 .

[12]  J. Shaji Coastal sensitivity assessment for Thiruvananthapuram, west coast of India , 2014, Natural Hazards.

[13]  Colin D. Woodroffe,et al.  Assessing vulnerability to sea-level rise using a coastal sensitivity index: a case study from southeast Australia , 2010 .

[14]  A. Smith,et al.  Contrasting styles of swell-driven coastal erosion: examples from KwaZulu-Natal, South Africa , 2010, Geological Magazine.

[15]  A. Mather Linear and nonlinear sea-level changes at Durban, South Africa , 2007 .

[16]  Christos Chalkias,et al.  Assessment of the sensitivity of the southern coast of the Gulf of Corinth (Peloponnese, Greece) to sea-level rise , 2012 .