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Abstract
Historical trends in the direction and magnitude of ocean surface wave height, period, or direction are debated due to diverse data, time-periods, or methodologies. Using a consistent community-driven ensemble of global wave products, we quantify and establish regions with robust trends in global multivariate wave fields between 1980 and 2014. We find that about 30–40% of the global ocean experienced robust seasonal trends in mean and extreme wave height, period, and direction. Most of the Southern Hemisphere exhibited strong upward-trending wave heights (1–2 cm per year) and periods during winter and summer. Ocean basins with robust positive trends are far larger than those with negative trends. Historical trends calculated over shorter periods generally agree with satellite records but vary from product to product, with some showing a consistently negative bias. Variability in trends across products and time-periods highlights the importance of considering multiple sources when seeking robust change analyses.
In about 30 to 40% of the global ocean, including most of the Southern Hemisphere, mean and extreme wave heights have increased in magnitude between 1980 and 2014, according to a multiproduct ensemble of historical global wave climate assessments.
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1 Pacific Coastal and Marine Science Center, US Geological Survey (USGS), Santa Cruz, USA (GRID:grid.513147.5)
2 Pacific Coastal and Marine Science Center, US Geological Survey (USGS), Santa Cruz, USA (GRID:grid.513147.5); University of Central Florida, Orlando, USA (GRID:grid.170430.1) (ISNI:0000 0001 2159 2859); Commonwealth Scientific and Industrial Research Organisation (CSIRO) Oceans and Atmosphere, Hobart, Australia (GRID:grid.1016.6) (ISNI:0000 0001 2173 2719)
3 Commonwealth Scientific and Industrial Research Organisation (CSIRO) Oceans and Atmosphere, Hobart, Australia (GRID:grid.1016.6) (ISNI:0000 0001 2173 2719)
4 University of Melbourne, Department of Infrastructure Engineering, Melbourne, Australia (GRID:grid.1008.9) (ISNI:0000 0001 2179 088X)
5 Environment and Climate Change Canada, Climate Research Division, Toronto, Canada (GRID:grid.410334.1) (ISNI:0000 0001 2184 7612)
6 University of Bologna, Department of Physics and Astronomy Augusto Righi, Bologna, Italy (GRID:grid.6292.f) (ISNI:0000 0004 1757 1758)
7 Kyoto University, Disaster Prevention Research Institute, Kyoto, Japan (GRID:grid.258799.8) (ISNI:0000 0004 0372 2033)
8 Department of Water Science and Engineering, IHE-Delft, Delft, The Netherlands (GRID:grid.258799.8)
9 University of Hawai’i, Department of Ocean and Resources Engineering, Honolulu, USA (GRID:grid.410445.0) (ISNI:0000 0001 2188 0957)
10 P.P. Shirshov Institute of Oceanology of the Russian Academy of Sciences, Moscow, Russia (GRID:grid.426292.9) (ISNI:0000 0001 2295 4196)
11 Norwegian Meteorological Institute, Department of Research and Development, Oslo, Norway (GRID:grid.82418.37) (ISNI:0000 0001 0226 1499)
12 European Centre for Medium-Range Weather Forecasts, Reading, UK (GRID:grid.42781.38) (ISNI:0000 0004 0457 8766)
13 Norwegian Meteorological Institute, Department of Research and Development, Oslo, Norway (GRID:grid.82418.37) (ISNI:0000 0001 0226 1499); University of Bergen, Bergen, Norway (GRID:grid.7914.b) (ISNI:0000 0004 1936 7443)
14 National Oceanography Centre, Liverpool, UK (GRID:grid.418022.d) (ISNI:0000 0004 0603 464X)
15 Institute of Hydraulics Cantabria, Santander, Spain (GRID:grid.258799.8)
16 National Autonomous University of Mexico, Mexico City, Mexico (GRID:grid.9486.3) (ISNI:0000 0001 2159 0001)
17 Deltares, Delft, The Netherlands (GRID:grid.6385.8) (ISNI:0000 0000 9294 0542)
18 Helmholtz-Zentrum Hereon, Geesthacht, Germany (GRID:grid.24999.3f) (ISNI:0000 0004 0541 3699)
19 Tokyo Institute of Technology, Tokyo, Japan (GRID:grid.32197.3e) (ISNI:0000 0001 2179 2105)