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The variety of socio-technical networks that marine professionals perform their work in, as well as the multiple points of stress that may be experienced by these networks, have made the comparative study of socio-technical networks difficult (Frantzis, 2006 ²¹⁸⁹ ). These networks operate in a range of contexts, ranging from blue growth in support of renewable energy sources (Frantzis, 2006 ²¹⁹⁰ ), to disaster risk management through emergency response (Frantzis et al., 2007 ²¹⁹¹ ), to coastal adaptation by increasing the resistance to storms and waves (Frantzis et al., 2011 ²¹⁹² ). In all of these cases, the socio-technical networks can be measured according to their characteristics and their effects on the development of different types of threats to the sustainability of marine ecosystems. The socio-technical network concepts outlined in these works (e.g., vulnerability, resilience, adaptive capacity, resilience capacity and adaptive potential) can also be used to represent the marine systems that they describe. In this study, an understanding of the changing vulnerability of near-shore ecosystems requires an analysis of the social-ecological interactions in a range of marine landscapes, which is relevant to all socio-technical networks with the potential to affect coastal resource management and the local response to SLR.

Independent of uncertainties in the onset and duration of RSL sea-level fall, it is clear that an estimate of current sea level is required for initiating, managing and evaluating sea-level projections. Asynchronised network of satellites, tide gauges, the GRACE Gravity Recovery and Climate Experiment (GRACE) and other global gravity measurement systems now gives us the opportunity to provide a global sea-level estimate of unprecedented accuracy. This is achieved by combining observations from different instruments, with a consistent interpretation of the available gravity data. GRACE data will be available at the time of writing, but there is still plenty of uncertainty in the data analyses and there are still details to iron out in this area. In particular, there is some debate about the way in which GRACE observations are combined with tide gauge information. GRACE has more limited usefulness in regional seas. Since it estimates tidal signals by superimposing a linear sea-level signal, it can in most cases not be used to measure any changes in tide that are too small to be measured by tide gauges. Similarly, due to the coarse temporal sampling (∼ three years in the Australian regional record) GRACE tide gauge data is of limited utility in local areas. However, tidal-based methods can be used in regional seas. In the Pacific, tidal measurements combined with GRACE GRAD data can be used to estimate changes in tidal potential.

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