in the beginning this yr , we discovered that ocean circulation is ata 1,500 - yr low . Now , research publish in the journalNaturesuggests that it is not because of world-wide heating , as antecedently suppose , but is rather part of a regular and decades - long   cycle . That is not to say it wo n’t have major implications on our climate in the come up years – or that this rude phenomenon wo n’t be exacerbated by climate change .

“ We have about one cycle of watching at depth , so we do not know if it ’s occasional , but free-base on the open phenomenon we think it ’s very likely that it ’s periodical , ” Ka - Kit Tung , a prof of employ mathematics at the University of Washington and co - writer of the theme , said in astatement .

It all comes down to something called the   Atlantic Meridional Overturning Circulation ( AMOC ) , the large organisation of currents that sends the oceans ' surface H2O northwards to the Atlantic Ocean . Here , the heavier ( and salty ) pee sinks to the bottom and retreats to the south , where it rises to the surface and flow north once again .

In April , a paperconfirmed the AMOC had slowed by roughly 15 percent in the last few decades , invest it at its modest pace in 1,500 years . At the time , the researchers ask that this was the culmination of   150 years of greenhouse   flatulence discharge and rising global temperatures   – but a newfangled study suggests otherwise .

Tung and atomic number 27 - source Xianyao Chen have retool this hypothesis with their report , published last calendar week . After analyzing   data point from Argo float , tidal records , ship - establish temperature measurements ,   satellite range of sea - surface stature , and gamy - tech trailing of the AMOC , they say the grounds points to it being part of a regular and periodic cycle of accelerate and slow down currents , which happen on a 60 to 70 - year basis . This means we do not have to panic about an apocalypticDay After Tomorrow - type scenario , where we are suddenly plunged into a new ice age .

When the AMOC is in a " fast phase " , you have more quick and piquant water from the tropical zone pour into the North Atlantic . Gradually , this do more glacier to thawing so that the fresh water from the chalk lightens the aerofoil water , abridge the swiftness at which it sink , slowing the current and introducing a " slow phase " . At this decimal point , the North Atlantic gets chillier and ice melt starts to slow . Over clip , the amount of fresh water on the surface will drop and the salty ( and , therefore , heavier ) water can sink , sound off off the whole process once again .

Tung and Chen say the AMOC is notcollapsing – it ’s simplytransitioningfrom one phase angle to another as part of a natural wheel .   But ( and it ’s a big but ) that is not to say that   the upshot wo n’t be exacerbated by climate change .

Between 1975 and 1998 , the AMOC was experiencing a ho-hum phase , which meant that there was a noticeable heating of surface temperature . But from 2000 onwards , this warming plateaued .   Tung and Chen think that this is because the AMOC was in a fast phase and some of this excess heat sunk with the heavy water to the bottom of the sea , where it is still stored . Now , the AMOC is   speed up   – and that means we can expect surface warming to accelerate too .

“ The well news is the indicators show that this retardation of the Atlantic overturning circulation is ending , and so we should n’t be alarmed that this current will collapse any time soon , ” Tung impart .

“ The defective news is that surface temperatures are likely to bulge rising more quickly in the come decades . ”