STORMS
It deepens the lows
Over an area of low pressure the jet stream can act like a vacuum cleaner, drawing air out of the top. The pressure falls further and the weather turns stormier.
Check the jetWHAT THE METEOROLOGISTS SAY
You cannot see it, but it steers our weather.
Around 5 to 7 miles up, the jet stream blows from west to east. The Met Office says its position is often the driving force behind the weather we get in the UK, from winter storms to a dull July.
Check the jet Read the short answer
THE SHORT ANSWER
The jet stream works like a conveyor belt high overhead.
It moves, strengthens and sometimes stalls weather systems.
STORMS
Over an area of low pressure the jet stream can act like a vacuum cleaner, drawing air out of the top. The pressure falls further and the weather turns stormier.
Check the jetSEASONS
In winter the temperature contrast is bigger, so the jet is stronger and often sits over the UK. In summer it usually shifts north, giving calmer, drier weather.
See the numbersFLIGHTS
The jet flows at about the height transatlantic aircraft fly. Flying with it can cut flight times and fuel; flying against it can bring delays.
Reading the forecastA QUICK JET CHECK
Pick where the jet stream is in the forecast to see the kind of weather the Met Office links with it. The bar shows how unsettled the UK weather tends to be.
A general guide based on Met Office explainers. Real weather depends on many factors, so always use the actual forecast and warnings.
TWO NUMBERS WORTH KNOWING
One figure on how high the jet stream blows,
one on how fast its core can get.
HEIGHT · MET OFFICE
Height of the jet stream
5–7 miles up
The Met Office describes the jet stream as a core of strong winds around 5 to 7 miles above the Earth's surface. NOAA gives a typical height of about 30,000 feet.
SPEED · NOAA
Top speeds in the core
275+ mph
NOAA says jet streams can reach speeds of more than 275 mph (442 km/h). The Met Office says the jet stream can reach speeds of over 200 mph.
NOAA describes two main jets in each hemisphere: the polar jet between about 50° and 60° latitude and the subtropical jet near 30°. Both follow the boundaries between hot and cold air.

FOUR THINGS TO LISTEN FOR
Forecasters often mention the jet stream when the weather changes. These four ideas help you follow what they mean.
WHY IT EXISTS
The jet stream exists because of the temperature difference between the equator and the poles. In the northern hemisphere cold polar air lies to the north of it and warmer air to the south, and that contrast drives the high-level winds.
The Earth's rotation turns the flow eastwards. NOAA explains that air moving away from the equator keeps its eastward momentum while the ground beneath it moves more slowly, so the wind runs from west to east. This is the Coriolis effect.

QUESTIONS PEOPLE ASK
The Met Office describes it as a core of strong winds around 5 to 7 miles above the Earth's surface, blowing from west to east. NOAA calls jet streams relatively narrow bands of strong wind in the upper atmosphere, or rivers of air.
Yes. NOAA describes a polar jet between about 50° and 60° latitude and a subtropical jet around 30°, in both hemispheres. They can meander, split and even disappear for a while.
In winter the temperature difference between the equator and the poles is larger, so the jet stream is stronger and often flows over the UK. The Met Office says this is why we tend to see wetter, windier weather then.
No. The Met Office says a Caribbean jet stream is not a meteorological term. Warm spells come from where the air mass is drawn from, such as the Azores, helped by small shifts in the jet stream.
It can. The Met Office says it flows at about the height of transatlantic aircraft: flying with it saves time and fuel, flying against it costs both, and it can bring turbulence where the wind changes speed.
SOURCES
Each figure on this page comes from the sources below. Check them for the full detail and context.