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McNamara, G. and Vieira da Silva, G., 2023. The coastline paradox: A new perspective. Journal of Coastal Research, 39(1), 45–54. Charlotte (North Carolina), ISSN 0749-0208. The coastline paradox, which suggests that coastlines have indefinite lengths, is a widespread and misleading concept that has endured in scientific literature for over 50 years. This paper argues that the length of a coastline is real and finite. The measurement of coastlines allows for the quantification of coastline dynamics and engineering responses to these changes. The real difficulties in measuring sometimes complex coastal shapes have taken the appearance of an unreal impossibility. The paradox is resolved using three methods. The first examines definitions used to establish the features to which "coastline" refers. The second applies these definitions to the measurement of real coastlines. Finally, a geometrical analysis is carried out to resolve the paradox mathematically. The purpose of this paper is to help resolve the paradox and reduce confusion surrounding the topic, which will be of direct use for coastal communities and planners to assess and respond to coastline changes and sea-level rise. [ABSTRACT FROM AUTHOR]

Skinner, W.K., 2024. Coastal hazard assessment from multidecadal profile response incorporating climate patterns and sea-level rise. Journal of Coastal Research, 40(3), 511–526. Charlotte (North Carolina), ISSN 0749-0208. A new method for coastal hazard assessment is described and demonstrated by reference to a 40-year cross-shore profile record in Papamoa, New Zealand. It is based on a mathematical interpretation of the envelope within which long-term historic cross-shore profiles vary and from which, for the required assessment period, the statistically significant fully accreted-state and fully eroded-state profiles can be determined. The Monte Carlo method is used to derive stochastic outcomes for long-term trend (LTT) and sea-level rise (SLR) on the basis of correlations with, and a long term proxy for, a decadal-scale climate pattern, which in the example case is the Interdecadal Pacific Oscillation. Sediment volumes for short-term fluctuation and the LTT are determined and conserved to reflect a consistent wave climate over the assessment period when appraising the effect of SLR. Dune biomass is accounted for when determining erosion scarp stability and hence the final extent of the current and future hazard zones. Results are presented in schematic form as excursions relative to a land benchmark and also as full end-state profiles extending from the dune backshore to the closure depth, with the latter determined by bar volume and profile. Various scenarios are appraised, including those that incorporate SLR predictions of the climate models of the Intergovernmental Panel on Climate Change. The relative risk of various scenarios is benchmarked to the probalistic expected outcome to produce a risk-based, site-specific assessment of coastal hazards. [ABSTRACT FROM AUTHOR]

Long, S.A.; Mango-Mutiti, C.; Mutiti, S., and Weese, D.A., 2023. Investigating the effects of increasing water salinity on an endemic crayfish. Journal of Coastal Research, 39(5), 816–822. Charlotte (North Carolina), ISSN 0749-0208. The greatest diversity of freshwater crayfish is found in the southeastern United States, home to nearly 75% of the world's known crayfish species. Many of the freshwater habitats for these crayfish are threatened by human activities and face degradation from multiple fronts, one being climate-related sea-level rise. This threat is significant for island populations that are unable to disperse to favorable locations. The goal of this study was to investigate the salinity tolerance of Procambarus lunzi (Hobbs 1940b), a species endemic to a small coastal region in the southeastern United States, to predict how sea-level rise might affect vulnerable coastal populations. A total of 171 crayfish was collected from a barrier island in Georgia and exposed to three treatments: freshwater, a slow salinity increase (salinity raised by 1.5‰ weekly), and a fast salinity increase (salinity raised by 3‰ weekly). Weekly mortalities were recorded and used to compute percent survivorship. Individual body masses were also monitored weekly and the average change in body mass between treatment groups was compared using one-way analysis of variance. Regression analysis was used to assess the relationship between initial body mass and the salinity level tolerated before mortality occurred. There was no significant difference in body mass change between the control group and the salinity treatment groups. The salinity level tolerated before mortality occurred was not correlated with individuals' body mass at the start of the treatments. The first mortality occurred at 30‰ salinity and 50% mortality occurred when salinity was >39‰. These results indicate a high tolerance to salinity that was unexpected for a freshwater species. The implication is that P. lunzi may be able to withstand habitat degradation due to sea-level rise given its relatively high tolerance to increases in salinity. [ABSTRACT FROM AUTHOR]

Lim, H.S.; Lee, H.J.; Kim, D., and Hong, S., 2023. Beach erosion along the eastern coast of Korea: A brief review. Journal of Coastal Research, 39(1), 181–190. Charlotte (North Carolina), ISSN 0749-0208. Most of the beaches on the eastern coast of Korea are eroding at an alarming rate, triggered by combined natural and artificial causes. In this review, each of the major causes of beach erosion is addressed briefly. A few protection measures such as breakwaters and nourishments are also discussed, with the emphasis on the unexpected or undesirable outcomes. Finally, some of the essential requirements for the field measurements in a beach are mentioned. Global warming has induced the chief natural causes of the beach erosion in Korea, including a gradual increase in wave energies and sea level. An estimation in this review suggests the rates of shoreline of 1 m/10 yrs on the eastern coast by sea-level rise alone. By comparison, artificial beach erosion is most likely to occur upon emplacing structures nearby. A variety of the artificially erosional cases by beach developments are described in the review. Storms and typhoons play a critical role in eroding beaches and changing local morphologies in a short period of time and thus should be observed hydrodynamically. However, the diminishing run-off of rivers and streams should be regarded as the primary reason for the nationwide artificial erosion of beaches. The scanty supply of stream sands to the beaches, together with the influence of global warming, would have the beaches eroded continuously without any coastal developments. [ABSTRACT FROM AUTHOR]