No abstract

Strategic environmental assessment (SEA) is used to identify the potential impacts of plans and policies such as maritime spatial planning (MSP). Studies have demonstrated ambiguity in SEA objectives and substantial knowledge gaps in existing and emerging SEA practices for MSP. The aim of this paper is to support a methodology for the development, implementation, and monitoring of SEA for MSP plans based on a stepwise, participatory mapping exercise by experts, using indicators to evaluate areas of conflicts/synergies in possible future scenarios. An overview of 16 proposed indicators identified a representative criterion. Participatory sector analyses were performed in three scenarios. Most conflicts focused on coastal areas, indicating that coastal planning should be a priority in all possible scenarios. The methodology developed in this paper uses GES indicators to perform the assessment of the three different scenarios and makes the development of a participatory mapping approach with experts in the very early stages of the process a more feasible alternative for a first assessment. This methodology was efficient in a collaborative SEA evaluation of MSPs to facilitate an ecosystem approach in an Azorean case study.

No abstract

Gomes et al.: Wave energy off the Brazilan coast 220Evaluating the gravity wave energy potential off the Brazilian coast The wave energy potential on the Brazilian coast is estimated using in-situ buoy data and model data. The results present a greater potential on the southern-southeastern coast than on the northeastern coast, but the variance is also larger. These seem to be associated with the different atmospheric regimes. While in the northeastern portion the trade winds determine the wave regime, in the south the passage of cold front systems plays a major role. For almost all regions and throughout the year, the energy potential oscillates between 10 and 30 kW/m, the most efficient range to implement wave energy converters. The occurrence of sea states is also assessed, showing that the passage of cold front systems also creates different sea states in the S-SW area. Finally, the most common sea states and energy flux are estimated, showing a shift towards longer periods and higher waves for the latter. On the S-SW coast, although the most frequent sea states have waves with periods around 8 s, the energy flux has a more balanced distribution between these and the waves with periods around 11s, the common period for waves generated by cold front systems. This result shows that the most common sea state is not necessarily the one that should be considered when planning wave energy converters for the region. AbstrAct

No abstract