Recent research suggests that slowing the circulation of the ocean as a result of climate change could increase the level of extreme cold weather in the United States.
All over the world, there is a conveyor belt of water.
Its vibraent is driven by fluctuation in temperature and salt water, and weather patterns around the world are regulated by its activity.
A pair of researchers investigated the Atlantic portion of this conveyor belt known as Atlantic Meridional Overturning Circulation (AMOC) and found that winter weather in the United States is essentially dependent on it.
As the AMOC slows as a result of climate change, the US will endure more extreme cold in winter.
Here is the functioning of the AMOC: Warm water moves north in the upper Atlantic Ocean and releases warmth into the atmosphere at high latitudes.
Climate models assume that the climate will be even weaker as a reaction to the increased levels of greenhouse gases in the atmosphere.
The difference between that the role of AMOCs in extremely cold weather.