Heat trapped by greenhouse gases is raising ocean temperatures faster than previously thought, according to a study which provides further evidence that earlier claims of a 'hiatus' in global warming over the past 15 years were unfounded.
"If you want to see where global warming is happening, look in our oceans," said Zeke Hausfather, a graduate student at the University of California, Berkeley in the U.S.
"Ocean heating is a very important indicator of climate change, and we have robust evidence that it is warming more rapidly than we thought," Hausfather said.
Ocean heating is critical marker of climate change because an estimated 93 per cent of the excess solar energy trapped by greenhouse gases accumulates in the world's oceans.
Unlike surface temperatures, ocean temperatures are not affected by year-to-year variations caused by climate events like El Nino or volcanic eruptions.
The new analysis, published in the journal Science, shows that trends in ocean heat content match those predicted by leading climate change models, and that overall ocean warming is accelerating.
Assuming a 'business-as-usual' scenario in which no effort has been made to reduce greenhouse gas emissions, the Coupled Model Intercomparison Project 5 (CMIP5) models predict that the temperature of the top 2,000 metres of the world's oceans will rise 0.78 degrees Celsius by the end of the century, researchers said.
The thermal expansion caused by this bump in temperature would raise sea levels 30 centimeters on top of the already significant sea level rise caused by melting glaciers and ice sheets.
Warmer oceans also contribute to stronger storms, hurricanes and extreme precipitation.
"While 2018 will be the fourth warmest year on record on the surface, it will most certainly be the warmest year on record in the oceans, as was 2017 and 2016 before that," said Hausfather.
Four studies, published between 2014 and 2017, provide better estimates of past trends in ocean heat content by correcting for discrepancies between different types of ocean temperature measurements and by better accounting for gaps in measurements over time or location.