Article,
Projected changes in wave climate from a multi-model ensemble
Nature Clim. Change, 3 (5): 471--476 (May 13, 2013)
DOI: 10.1038/nclimate1791
Abstract
Future changes in wind-wave climate have broad implications for the operation and design of coastal, near- and off-shore industries and ecosystems, and may further exacerbate the anticipated vulnerabilities of coastal regions to projected sea-level rise. However, wind waves have received little attention in global assessments of projected future climate change. We present results from the first community-derived multi-model ensemble of wave-climate projections. We find an agreed projected decrease in annual mean significant wave height (H\_S) over 25.8\% of the global ocean area. The area of projected decrease is greater during boreal winter (January–March, mean; 38.5\% of the global ocean area) than austral winter (July–September, mean; 8.4\%). A projected increase in annual mean H\_S is found over 7.1\% of the global ocean, predominantly in the Southern Ocean, which is greater during austral winter (July–September; 8.8\%). Increased Southern Ocean wave activity influences a larger proportion of the global ocean as swell propagates northwards into the other ocean basins, observed as an increase in annual mean wave period (T\_M) over 30.2\% of the global ocean and associated rotation of the annual mean wave direction (θ\_M). The multi-model ensemble is too limited to systematically sample total uncertainty associated with wave-climate projections. However, variance of wave-climate projections associated with study methodology dominates other sources of uncertainty (for example, climate scenario and model uncertainties).
