Study: As the Oceans Warm, Wave Intensity May Increase
[By Thomas Mortlock, Itxaso Oderiz, Nobuhito Mori and Rodolfo Silva]
Sea level rise isn’t the only way climate change will devastate the coast. Our research, published June 8, found it is also making waves more powerful, particularly in the Southern Hemisphere.
We plotted the trajectory of these stronger waves and found the coasts of South Australia and Western Australia, Pacific and Caribbean Islands, East Indonesia and Japan, and South Africa are already experiencing more powerful waves because of global warming.
This will compound the effects of sea level rise, putting low-lying island nations in the Pacific — such as Tuvalu, Kiribati and the Marshall Islands — in further danger, and changing how we manage coasts worldwide. But it’s not too late to stop the worst effects — that is, if we drastically and urgently cut greenhouse gas emissions.
An energetic ocean
Since the 1970s, the ocean has absorbed more than 90 percent of the heat gained by the planet. This has a range of impacts, including longer and more frequent marine heatwaves, coral bleaching, and providing an energy source for more powerful storms.
But our focus was on how warming oceans boost wave power. We looked at wave conditions over the past 35 years, and found global wave power has increased since at least the 1980s, mostly concentrated in the Southern Hemisphere, as more energy is being pumped into the oceans in the form of heat.
And a more energetic ocean means larger wave heights and more erosive energy potential for coastlines in some parts of the world than before. Ocean waves have shaped Earth’s coastlines for millions of years. So any small, sustained changes in waves can have long-term consequences for coastal ecosystems and the people who rely on them.
Mangroves and salt marshes, for example, are particularly vulnerable to increases in wave energy when combined with sea level rise. To escape, mangroves and marshes naturally migrate to higher ground. But when these ecosystems back onto urban areas, they have nowhere to go and die out. This process is known as “coastal squeeze”.
These ecosystems often provide a natural buffer to wave attack for low-lying coastal areas. So without these fringing ecosystems, the coastal communities behind them will be exposed to more wave energy and, potentially, higher erosion.
So why is this happening?
Ocean waves are generated by winds blowing along the ocean surface. And when the ocean absorbs heat, the sea surface warms, encouraging the warm air over the top of it to rise (this is called convection). This helps spin up atmospheric circulation and winds.
In other words, we come to a cascade of impacts: warmer sea surface temperatures bring about stronger winds, which alter global ocean wave conditions.
Our research shows, in some parts of the world’s oceans, wave power is increasing because of stronger wind energy and the shift of westerly winds towards the poles. This is most noticeable in the tropical regions of the Atlantic and Pacific Oceans, and the subtropical regions of the Indian Ocean.
But not all changes in wave conditions are driven by ocean warming from human-caused climate change. Some areas of the world’s oceans are still more influenced by natural climate variability — such as El Niño and La Niña — than long-term ocean warming.
In general, it appears changes to wave conditions towards the equator are more driven by ocean warming from human-caused climate change, whereas changes to waves towards the poles remain more impacted by natural climate variability.
How this could erode the coasts
While the response of coastlines to climate change is a complex interplay of many processes, waves remain the principal driver of change along many of the world’s open, sandy coastlines.
So how might coastlines respond to getting hit by more powerful waves? It generally depends on how much sand there is, and how, exactly, wave power increases.
For example, if there’s an increase in wave height, this may cause increased erosion. But if the waves become longer (a lengthening of the wave period), then this may have the opposite effect, by transporting sand from deeper water to help the coast keep pace with sea level rise.
For low-lying nations in areas of warming sea surface temperatures around the equator, higher waves - combined with sea level rise - poses an existential problem.
People in these nations may experience both sea level rise and increasing wave power on their coastlines, eroding land further up the beach and damaging property. These areas should be regarded as coastal climate hotspots, where continued adaption or mitigation funding is needed.
It’s not too late
It’s not surprising for us to find the fingerprints of greenhouse warming in ocean waves and, consequentially, along our coastlines. Our study looked only at historical wave conditions and how these are already being impacted by climate change.
But if warming continues in line with current trends over the coming century, we can expect to see more significant changes in wave conditions along the world’s coasts than uncovered in our backward-looking research.
However, if we can mitigate greenhouse warming in line with the 2? Paris agreement, studies indicate we could still keep changes in wave patterns within the bounds of natural climate variability.
Still, one thing is abundantly clear: the impacts of climate change on waves is not a thing of the future, and is already occurring in large parts of the world’s oceans. The extent to which these changes continue and the risk this poses to global coastlines will be closely linked to decarbonization efforts over the coming decades.
Thomas Mortlock is a Senior Risk Scientist at Risk Frontiers and an Adjunct Fellow at Macquarie University.
Itxaso Odériz is a research assistant at Universidad Nacional Autónoma de México (UNAM).
Nobuhito Mori is a professor at Kyoto University.
Rodolfo Silva is a professor at Universidad Nacional Autónoma de México (UNAM).
This article appears courtesy of The Conversation and may be found in its original form here.
The opinions expressed herein are the author's and not necessarily those of The Maritime Executive.