{"id":68264,"date":"2021-02-15T10:04:29","date_gmt":"2021-02-15T09:04:29","guid":{"rendered":"https:\/\/www.sonnenseite.com\/?p=68264"},"modified":"2021-02-15T10:04:30","modified_gmt":"2021-02-15T09:04:30","slug":"marine-heatwaves-becoming-more-intense-more-frequent","status":"publish","type":"post","link":"https:\/\/www.sonnenseite.com\/en\/future\/marine-heatwaves-becoming-more-intense-more-frequent\/","title":{"rendered":"Marine Heatwaves Becoming More Intense, More Frequent"},"content":{"rendered":"\n

Thinning surface layer of ocean leaves waters more susceptible to extreme warming events.<\/p>\n\n\n\n

When thick, the surface layer of the ocean acts as a buffer to extreme marine heating\u2014but a new study from CU Boulder shows this \u201cmixed layer\u201d is becoming shallower each year. The thinner it becomes, the easier it is to warm. The new work could explain recent extreme marine heatwaves, and points at a future of more frequent and destructive ocean warming events as global temperatures continue to climb.<\/p>\n\n\n\n

\u201cMarine heatwaves will be more intense and happen more often in the future,\u201d said Dillon Amaya, a CIRES Visiting Fellow<\/a> and lead author on the study<\/a> out this week in the Bulletin of the American Meteorological Society<\/em>\u2019s Explaining Extreme Events<\/a>. \u201cAnd we are now understanding the mechanics of why. When the mixed layer is thin, it takes less heat to warm the ocean more.\u201d<\/p>\n\n\n\n

The mixed layer\u2014the water in which temperature remains consistent\u2014blankets the top 20-200 meters of the ocean. Its thickness is responsible for heat events: the thicker it is, the more the layer can act as a buffer to shield the waters below from incoming hot air. But as this armor thins, the mixed layer becomes more susceptible to rapid swings in temperature.<\/p>\n\n\n\n

\u201cThink of the mixed layer as boiling a pot of water,\u201d said Amaya. \u201cIt will take no time at all for an inch of water to come to a boil, but much longer for a pot filled to the brim to heat through.\u201d<\/p>\n\n\n\n

Amaya and his team from NOAA, NCAR and CU Boulder used a combination of ocean observations and models to estimate the depth of the mixed layer back to 1980, and also project out into the future. They determined that over the last 40 years, the layer has thinned by nearly 3 meters (9 feet) in some regions of the North Pacific. And by 2100, the mixed layer will be 4 meters (12 feet) thinner\u201430 percent less than what it is today. This thin mixed layer combined with warmer global temperatures will set the stage for drastic swings in ocean temperatures, leading to much more frequent and extreme heating events, the researchers say.<\/p>\n\n\n\n

And it\u2019s already happening. Take the 2019 heatwave<\/a> in the Northeast Pacific. Weakened winds and higher air temperatures came together to warm Pacific Ocean waters by about 3 degrees C (5.5 F). A thinning mixed layer most likely contributed to this surge of warm waters, the authors found. And it will get worse.<\/p>\n\n\n\n

\u201cIf you take the same wind and ocean conditions that occurred in 2019 and you apply them to the estimated mixed layer in 2100, you get a marine heatwave that is 6.5 degrees C (12 F) warmer than what we say in 2019,\u201d said Amaya. \u201cAn event like that would absolutely devastate sensitive marine ecosystems along the U.S. west coast.\u201d<\/p>\n\n\n\n

Amaya also points out that, as climate continues to warm and the mixed layer continues to thin, scientists might start to lose the ability to predict year-to-year ocean surface temperatures. Without the ability to accurately forecast ocean temperatures, fisheries and other coastal operations could be in danger.<\/p>\n\n\n\n

Other studies also suggest marine heatwaves will become more common in the future, but not many have explored the root cause: ocean dynamics and physics. \u201cIn order to simulate these events in models and help predict them, we must understand the physics of why that\u2019s happening,\u201d said Amaya.<\/p>\n\n\n\n

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