Wave height and path spied from space
A new study from the Australian National University will improve the models and maps of ocean currents, wave heights and tides, plotting the incredibly long process that ends with waves crashing on the shore.
Research led by ANU Vice-Chancellor Professor Ian Young will allow oceanographers and meteorologists to better predict the rate at which ocean swells decay, or deteriorate, as they travel across the globe.
“Ocean cargo shipping, offshore oil and gas production, and even recreational activities such as surfing, are all dependent on wave action,” says Professor Young.
“It is therefore critical that we are able to predict swell.”
It is estimated that 75 per cent of waves across the world are not actually generated by local winds. Instead, they are driven by distant storms which generate swells.
“Imagine you drop a rock in a pond. Waves radiate out from the rock. You don’t need anything to push the waves. Once generated, they propagate by themselves.
“So, for most of the Indian, Pacific and South Atlantic oceans, it is actually the weather in the Southern Ocean thousands of kilometres away that dominates the wave conditions,” explains Professor Young.
“The Southern Ocean is dominated by big low pressure systems that move across it year round. These systems generate waves that then grow and can travel tens of thousands of kilometres from where they were actually formed, to crash on a beach in Australia.”
The researchers used satellites to track swells generated in the Southern Ocean, measuring the rate of decay as they travelled north towards Australia. They found that the decay of the swell depends on how steep the wave is.
“Steep waves decay very quickly. However, typical swell is not very steep and can travel across oceanic basins with only a relatively small loss of energy,” Prof Young said
“What we were able to do is track the swell from the satellite as it moved from the south to the north, some 1400 kilometres. We only chose cases where there was no wind so that we could be confident that all we were measuring was the swell decay.
“We can take these results and put them into a mathematical formula that can be put straight into computer models used by national weather bureaus.
“This will increase our ability to better predict wave action. As 70 per cent of the world’s oceans are dominated by swell, it’s extremely important to be able to predict them accurately.”
Full details from the report are available from the Journal of Physical Oceanography.