Create a list of articles to read later. You will be able to access your list from any article in Discover.
You don't have any saved articles.
The northern lights, also called the aurora borealis, have transfixed humans for thousands of years.
Discover the best time and place to see this natural phenomenon as well as the science behind how we forecast it.
The northern lights is the name given to the colourful lights that can appear in the night sky over the northern hemisphere. When they appear in the southern hemisphere, they’re called the southern lights instead.
This phenomenon is known as an aurora. The northern lights are more formally known as the aurora borealis because borealis means north in Latin. The southern lights, meanwhile, are called the aurora australis.
Auroras don’t just happen on Earth. Scientists have also seen them on other planets, including Mars, Jupiter and Saturn, as well as on comets and even dwarf stars far beyond our solar system.
The northern lights are caused by the interaction between the magnetic fields of the Sun and Earth. Dr Geoff Vasil, who studies the Sun’s workings at the University of Edinburgh’s School of Mathematics, explains how this creates an aurora.
“The Sun is a nuclear furnace, squeezing atoms together at its heart to release energy,” Geoff explains. “Ultimately, that’s where the power behind the northern lights comes from.”
“Over time, this energy gradually emerges from the core and leaks to the outside, where it starts to cause convection currents in the Sun’s upper layers. These currents generate the Sun’s magnetic field.”
“While we’re not exactly sure how everything works, the intense heat and magnetism is enough to launch energetic charged particles into space as the solar wind.”
These charged particles are released in all directions, with some heading towards Earth.
Earth generates its own magnetic field due to currents in its metallic outer core, and this helps to deflect most of the charged particles.
But not all the particles are deflected. Instead, some are funnelled towards the planet’s poles and into the atmosphere. It’s these charged particles that are responsible for auroras such as the northern lights.
The colours of the northern lights result from the charged particles hitting different atoms and molecules in Earth’s upper atmosphere. Some of the energy from the charged particles is passed on during the collision, but the atoms and molecules can’t store it for very long.
Instead, this excess energy is released as light, and each element emits different colours:
The strength of the northern lights varies for many different reasons, including how active the Sun is. Our star goes through an 11-year-long solar cycle during which the strength of its magnetic field changes.
When the solar cycle peaks, known as the solar maximum, the Sun’s magnetic field is at its strongest. This leads to stronger solar storms and more of them, including events such as solar flares and coronal mass ejections.
These can throw large amounts of charged particles out into space towards Earth. This causes geomagnetic storms that increase the chance of the northern lights occurring and make it more likely that the lights will be strong.
“When the magnetic fields of the Sun reach our planet, they can push Earth’s magnetic field out behind it,” explains Geoff. “Once it is stretched out far enough, Earth’s magnetic field snaps back like an elastic band.”
“This is known as reconnection and releases a large amount of particles into the upper atmosphere. This causes the northern lights to grow bigger and brighter.”
The best place to see the northern lights changes depending on the solar cycle, the time of year and a variety of other factors. Generally, however, northern lights visibility is normally better the closer you are to magnetic north.
“The location of the northern lights can change depending on the solar wind,” Geoff says. “They tend to happen nearer the poles where particles can enter the atmosphere more easily, but the aurora can move closer to the equator depending on the conditions.”
The region where the northern lights are most common is known as the annulus. This is a ring-shaped region centred on the northern magnetic pole that’s around 3,000 kilometres across.
Countries inside the annulus, including Finland, Iceland and Canada, are generally the best places to see the northern lights.
When solar activity is strong enough, however, the annulus can expand and reach more southerly nations, such as the UK and USA. This is most common around the time of the solar maximum.
The best time to see the northern lights is generally during March and April as well as later in the year during September and October. It’s particularly common around the spring and autumn equinoxes, the two occasions each year when day and night are roughly the same length.
This is often known as the Russell-McPherron effect, named after the two scientists who noticed that auroras tend to get stronger around the equinoxes. Their explanation for this is based on the way the Sun’s and Earth’s magnetic fields interact.
Like all magnets, their magnetic fields have a north and a south pole. The polarity of these magnetic fields changes over the year. Around the equinoxes, the polarity of the Sun’s and Earth’s magnetic fields line up in opposite directions.
This allows more particles from the solar wind to get into Earth’s atmosphere, causing more intense northern lights. The magnetic poles are also at a right angle to the flow of the solar wind around the equinoxes, which further enhances the aurora.
The effect of equinoxes is just one of the factors scientists consider when forecasting the northern lights.
Northern lights forecasts attempt to predict when and where auroras will take place. Forecasters combine information about conditions on Earth and the Sun to predict how visible the northern lights will be, but it’s a tricky process.
“We know what happens in almost every stage of the process of the northern lights forming, but the whys are mysterious,” explains Geoff. “The stages on Earth are much better understood than those in the Sun.”
“As we don’t fully understand how the Sun works, solar forecasting currently attempts to model what our star might do based on previous observations. For example, the size and position of sunspots can be used to suggest when they might erupt.”
“At the moment, our short-term forecasts are more accurate than the longer-term predictions, which will need us to have a better idea of what’s happening in the Sun.”
The likelihood of seeing the northern lights tonight depends on a variety of factors, including the time of year, the weather and levels of light pollution.
It’s worth checking the websites of organisations such as the Space Weather Prediction Center or AuroraWatch UK to see when the northern lights are likely to be visible in your area.
To maximise your chances, find an area of high ground where the skies are clear and dark away from the lights of towns and cities.
The northern lights are most visible around the spring months of March and April and the autumn months of September and October. The aurora is generally at its strongest between 23.00 and 02.00 at night, but this can vary depending on the conditions.
Photographing the northern lights can be difficult but it’s not impossible. To give yourself the best chance of capturing them on camera, first find an area with clear, dark skies away from non-natural light sources.
To capture the ethereal glow of the northern lights as they flicker and glow above you, set your camera to a long exposure time. You’ll also need to keep your camera as still as possible, so it’s worth using a tripod if you have one.
If you’re using a smartphone, make sure your flash is off and set the camera to night mode if your phone has one. Increase the exposure time and hold your phone as steady as you can.
You may need to experiment with different settings to get the best pictures.