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Climate Change Driven Ocean Warming is Making Waves Larger: Why it Matters
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Climate Change Driven Ocean Warming is Making Waves Larger: Why it Matters
Since 1948, ocean wave energy has increased by 0.4% per year, due to overall global warming increasing sea surface temperatures and wind speeds.
Also, ocean waves can be 4x steeper than previously thought, when wave models are in 3D versus the more commonly used 2D models. This has been verified by direct observations in a wave tank at the University of Edinburgh.
This means that so-called rogue waves that occurred in the real “Perfect Storm” in 1991 sinking a fishing boat (portrayed in Hollywood Movie The Perfect Storm), sinking the Ocean Ranger oil rig, and the Draupner Wave will be more likely with global warming causing increased ocean warming.
Links:
Extreme 3D ocean waves can reach heights 4x steeper than previously thought
Peer-reviewed paper: Three-dimensional wave breaking
Wave illustrations
Ocean warming is making waves stronger—and that’s a problem
A recent increase in global wave power as a consequence of oceanic warming
Abstract
Wind-generated ocean waves drive important coastal processes that determine flooding and erosion. Ocean warming has been one factor affecting waves globally. Most studies have focused on studying parameters such as wave heights, but a systematic, global and long-term signal of climate change in global wave behavior remains undetermined. Here we show that the global wave power, which is the transport of the energy transferred from the wind into sea-surface motion, has increased globally (0.4% per year) and by ocean basins since 1948. We also find long-term correlations and statistical dependency with sea surface tempera- tures, globally and by ocean sub-basins, particularly between the tropical Atlantic tempera- tures and the wave power in high south latitudes, the most energetic region globally. Results indicate the upper-ocean warming, a consequence of anthropogenic global warming, is changing the global wave climate, making waves stronger. This identifies wave power as a potentially valuable climate change indicator.
Laboratory recreation of the Draupner wave and the role of breaking in crossing seas
Abstract
Freak or rogue waves are so called because of their unexpectedly large size relative to the population of smaller waves in which they occur. The 25.6 m high Draupner wave, observed in a sea state with a significant wave height of 12 m, was one of the first confirmed field measurements of a freak wave. The physical mechanisms that give rise to freak waves such as the Draupner wave are still contentious. Through physical experiments carried out in a circular wave tank, we attempt to recreate the freak wave measured at the Draupner platform and gain an understanding of the directional conditions capable of supporting such a large and steep wave. Herein, we recreate the full scaled crest amplitude and profile of the Draupner wave, including bound set-up. We find that the onset and type of wave breaking play a significant role and differ significantly for crossing and non-crossing waves. Crucially, breaking becomes less crest-amplitude limiting for sufficiently large crossing angles and involves the formation of near-vertical jets. In our experiments, we were only able to reproduce the scaled crest and total wave height of the wave measured at the Draupner platform for conditions where two wave systems cross at a large angle.
Wikipedia: List of Rogue Waves
Hollywood: The Poseidon Adventure
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