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The prospect of the Gulf Stream slowing down and even stopping altogether has worried many experts in recent years. Some believed that this would cause a rapid cooling around the world with resulting global chaos. But a new study finds the Gulf Stream go-slow will have a significant impact on planetary temperatures, but not in a chilled out way. The Gulf Nandina gulf stream problems review is an ocean current that keeps the UK nandina gulf stream problems review than it would be given its latitude.

Researchers say a slower current will carry less heat down to the deep oceans meaning more will enter the atmosphere. It focused on a sudden collapse of the Amoc caused by global warming leading to a disastrous freezing and the dawning of a new ice age. So much for Hollywood - the reality according to the corresponding author of this new study is very different. Instead Prof Tung and his colleague, Xianyao Chen from the Ocean University of China, have reconstructed what's happened with the flow of the Amoc over nandina gulf stream problems review past 70 years.

They found a natural pattern with declines, flat periods and increases over the decades. It's a powerful ocean current that is part of the Amoc and it flows from the Gulf of Mexico, around Florida and up along the east coast of the Sgream, before crossing the Atlantic towards Ireland, the UK and Europe.

For decades we've believed that the Gulf Stream and the Amoc were like a giant hot water bottle, keeping Europe and the Eastern US warm in the winter. It's believed reiew the impact was as much as 5C, keeping London and Western Europe far less cold than say parts of Canada which are at the same latitude. But this new study indicates that the Amoc plays a far more important role as a massive global heat distribution system than it does in keeping Europeans toasty.

It works like this - The warm waters from tropical regions gul carried up to the North Atlantic where the current nandina gulf stream problems review them deep into the oceans, nandinna cooler waters then returning south in their stead.

When the Amoc current srteam faster, more of the heat that is trapped in our atmosphere from the burning of fossil fuels is taken and stored up to 1,m below the surface of the ocean. When it slows down, less heat is sequestered in the seas and so our land surface nandina gulf stream problems review increase. When the Amoc was at a minimum between andmore heat entered the atmosphere and global temperatures gradually went up.

When the current started to accelerate from the mids to the early s, and sink more heat it coincided with a so-called slowdown in the pace of global warming. Now the authors say that the big decline is Amoc flow since means less heat going into the waters and more into the air, leading to higher global temperatures.

And that is likely to continue. In the northern Atlantic it is still declining. While the waters of the North Atlantic will definitely cool as a result of changes in rveiew flow, the experts says it's likely that the UK will see continued impacts of climate change over the next 20 years according to this study.

The study has been published in the journal Nature. Baby snake fossil 'frozen in time' Are young people going cool on cars? Welcome to the Meghalayan Age. What nandina gulf stream problems review the Gulf Stream? Why is it important? What's the evidence for this new Amoc theory? Will the slowdown in the Atlantic current continue? That's unlikely according to this study.

So what will this mean for the UK? View comments. Related Topics. Atlantic Ocean Climate change.

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