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The Gulf Stream is a strong,
warm, fast moving ocean current that flows into the Atlantic Ocean and is often
referred as originating in the Gulf of Mexico.
It makes up a portion of the North Atlantic
Subtropical Gyre.
The Gulf Stream results in the
climate of Western and Northern Europe being warmer than it would be otherwise
due to the North Atlantic Drift, one of the branches from the tail of the Gulf
Stream.
The waters that feed
into the Gulf Stream flow from the west coast of Northern Africa. The Atlantic
North Equatorial Current flows from that continent across the Atlantic Ocean. The
current splits into two currents when it reaches Eastern South America. One of
these currents is the Antilles current which is funnelled through the islands of
the Caribbean and between Mexico and Cuba.
The northern stream crosses to
Northern Europe, whilst the southern stream recirculates off West Africa. Because these areas are often very narrow, the current is
able to compress and gather strength. As it does so, it begins circulating in
the Gulf of Mexico’s warm waters. It is here that the Gulf Stream becomes
officially visible on satellite images so it
is said that the current originates in this area.
Once it gains
enough strength after circulating in the Gulf of Mexico, the Gulf Stream then
moves east. It rejoins the Antilles
Current and exits the area through the Straits of Florida. Here, the Gulf
Stream is a powerful underwater river that transports water at a rate of 30
million cubic meters per second.
It then flows
parallel to the east coast of the United States and later flows into the open
ocean near Cape Hatteras but continues moving north. In this deeper ocean water
the Gulf Stream is its most powerful and splits into several currents, the
largest of which is the North Atlantic Current.
The North
Atlantic Current then flows further north and feeds the Norwegian Current and
moves the relatively warm water along the west coast of Europe. The rest of the
Gulf Stream flows into the Canary Current which moves along the eastern side of
the Atlantic Ocean and back south to the equator.
The northern
branch of the Gulf Stream, the North Atlantic Current, is deeper and is caused
by thermohaline circulation resulting from density differences in the water.
Because ocean currents circulate water of different
temperatures all over the globe, they often have a significant impact on the
world’s climate and weather patterns. The Gulf Stream is one of the most
important currents in this regard since it gathers all of its water from the
warm tropical waters of the Caribbean and the Gulf of Mexico. As such, it keeps
sea surface temperatures warm, causing the areas around it to be warm and more
hospitable. Florida and much of the South-eastern United States for instance is
mild all year round.
The greatest
impact the Gulf Stream has on climate is found in Europe. Since it flows into
the North Atlantic Current, it too is warmed (though at this latitude the sea
surface temperatures are cooled considerably), and it is believed that it helps
keep places like Ireland and England much warmer than they would otherwise be
at such a high latitude. For example, the average low in London in December is
42°F (5°C) while in St. John’s, Newfoundland, the average is 27°F (-3°C). The
Gulf Stream and its warm winds are also responsible for keeping northern
Norway’s coast free of ice and snow.
As well as
keeping many places mild, the Gulf Stream’s warm sea surface temperatures also
aid in the formation and strengthening of many of the hurricanes that move through the Gulf of Mexico. Additionally, the
Gulf Stream is important to the distribution of wildlife in the Atlantic. The
waters off of Nantucket, Massachusetts for example are incredibly bio diverse
because the presence of the Gulf Stream makes it the northern limit for
southern species varieties and the southern limit for northern species.
Although there are no definitive answers, it is
believed that the Gulf Stream could be in the future or is already being
impacted by global warming and the melting of glaciers.
Some studies suggest that with the melting of ice in places like Greenland,
cold, dense water will flow into the ocean and disrupt the flow of the Gulf
Stream and other currents that are part of the Global Conveyor Belt. If this
were to happen, weather patterns worldwide could change.
Recently, there
has been evidence that the Gulf Stream is weakening and slowing and there is
growing concern about what impacts such a change would have on the world’s
climate. Some reports suggest that without the Gulf Stream, temperatures in
England and north=western Europe could drop by 4-6°C.
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