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2D Aurora Borealis: Solar Wind & Magnetic Field Lines

A dynamic display of Earth’s magnetic field interacting with charged particles from the Sun to create the mesmerizing auroral displays in polar regions.

mysimulator teamUpdated June 2026≈ 4 min read▶ Open the simulation

What the 2D Aurora Borealis Is

The 2D Aurora Borealis is a simplified representation of the complex interaction between Earth’s magnetic field and charged particles from the Sun. This simulation models how solar wind, consisting primarily of electrons and protons, interacts with Earth's magnetosphere to create the auroral displays observed in polar regions.

In this model, charged particles stream along the lines of Earth’s magnetic field into the atmosphere where they collide with atmospheric gases such as oxygen and nitrogen, exciting these atoms and causing them to emit light. The resulting patterns mimic the green, red, and purple curtains seen during an auroral display.

Why It Happens

The 2D Aurora Borealis occurs due to the interaction between Earth’s magnetic field and charged particles from the Sun. When solar wind reaches Earth, it encounters our planet's magnetosphere, a region of space around Earth where the influence of its magnetic field dominates over that of the solar wind.

As these charged particles are guided along the lines of Earth’s magnetic field towards regions near the poles, they collide with atmospheric gases. These collisions excite the gas atoms and molecules, causing them to emit light in a process known as chemiluminescence.

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How It Affects Different Gases

The colors of the aurora are determined by which gases are present in the atmosphere. In this simulation, nitrogen and oxygen play key roles. Oxygen typically produces green and red light when excited, while nitrogen tends to emit blue or purple hues.

By adjusting the ratio of nitrogen to oxygen in the model, you can see how different gas compositions affect the overall coloration of the aurora.

Impact on Earth’s Atmosphere

The 2D Aurora Borealis simulation helps us understand the impact of solar wind on Earth's atmosphere. Auroras are not just beautiful natural phenomena; they can also affect satellite communications, power grids, and even GPS systems due to their magnetic field interactions.

Studying auroras provides insights into space weather and helps predict geomagnetic storms that could disrupt technology and infrastructure.

Frequently asked questions

What causes the different colors in the aurora borealis?

The colors of the aurora are caused by the excitation of atmospheric gases like oxygen and nitrogen. Oxygen typically produces green and red light, while nitrogen tends to emit blue or purple hues.

How do solar flares affect the aurora borealis?

Solar flares can increase the intensity and frequency of charged particles streaming from the Sun, leading to more vibrant and extensive auroral displays. Strong solar activity can cause geomagnetic storms that enhance the aurora.

Can we see auroras at any latitude on Earth?

Auroras are most commonly seen near the polar regions but can be observed at lower latitudes during strong solar activity. The auroral oval expands and contracts based on geomagnetic conditions.

What is chemiluminescence in the context of the aurora borealis?

Chemiluminescence refers to the process by which excited atoms or molecules release energy in the form of light. In the case of the aurora, this occurs when charged particles from the solar wind collide with atmospheric gases and excite them, leading to the emission of light.

Try it live

Everything above runs in your browser — open 2D Aurora Borealis: Solar Wind & Magnetic Field Lines and change the parameters while it is running. Nothing is installed, nothing is uploaded, the whole model lives in one tab.

▶ Open 2D Aurora Borealis: Solar Wind & Magnetic Field Lines simulation

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