Abstract

Sea-level rise (SLR) poses a particularly ominous threat to human habitations and infrastructure in the coastal zone because 10% of the world's population lives in low-lying coastal regions within 10m elevation of present sea level. There has been much discussion about projected (and the sources of projection) vs. measured SLR rates. Which rates should coastal scientists and managers apply in their studies, and what is the degree of confidence of such forecasts, are still open questions.This paper reviews the patterns and effects of relative SLR (RSLR) in coastal lagoons. Three main components are presented in the review: (a) a summary of the main approaches used in predicting medium- to long-term trends in RSLR, (b) a summary of the main evolutionary trends of coastal lagoons and the tools used to examine such trends, and (c) an identification of future research needs.The review reveals that the major source of uncertainty is how and when RSLR will manifest itself at different spatio-temporal scales in coastal lagoon systems, and how its effects can be mitigated. Most of the studies reviewed herein articulate a natural ‘defence’ mechanism of barriers in coastal lagoons by landward barrier retreat through continuous migration, and a gradual change in basin hypsometry during the retreat process. So far, only a relatively small number of detailed studies have integrated and quantified human impacts and coastal lagoon evolution induced by RSLR. We conclude that much more research about adaptation measures is needed, taking into consideration not only the physical and ecological systems but also social, cultural, and economic impacts. Future challenges include a downscaling of SLR approaches from the global level to regional and local levels, with a detailed application of coastal evolution prediction to individual coastal lagoon systems.

Highlights

  • Sea-level rise (SLR) is among the most important yet complex and often misunderstood aspects of climate change

  • The present review shows that the level of knowledge regarding the potential severity of the consequences of climate change on coastal zones is still insufficient

  • It should be borne in mind that because of regional differences in SLR, the occurrence of and response to the effects of climate change will not be uniform worldwide

Read more

Summary

Introduction

Sea-level rise (SLR) is among the most important yet complex and often misunderstood aspects of climate change. What matters most to the coastal morphological equilibrium is not the global-mean projected SLR rate itself, but the local change in the observed relative sea-level rise (RSLR). Geological observations reveal that many barrier systems worldwide have been able to keep pace with RSLR for thousands of years (McBride et al, 2013) These systems can have spatially distinct responses to RSLR, as in the case of the Gulf of Mexico, which is composed of several bay/lagoon stretches and barriers, where previous studies (e.g., Troiani et al, 2011) have reported rapid and dramatic morphological changes resulting from RSLR and spatial differences in the response. Those authors estimate that 145 million people live within 1 m of present-day mean sea level. Three foci to the review are presented: (a) summarizing the main approaches used in predicting medium- to long-term trends in SLR; (b) identifying the main evolutionary trends of coastal lagoons and the tools used to examine such trends; and (c) highlighting the aspects that require further research

SLR scenarios and key uncertainties
Time scales and length scales of coastal evolution
Morphological effects of RSLR in coastal lagoons
RSLR and the evolution of barriers and inlets
RSLR and salt marsh evolution
Modelling the evolution of coastal lagoons under RSLR scenarios
The economic and social consequences of RSLR for coastal lagoons
Future challenges
Findings
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call