Space plasma

Stars like our Sun are made of ionised gas known as plasma. In fact, space is dominated by plasma – space scientists (astrophysicists) believe that about 99% of matter in the universe is plasma.

The Sun

Astrophysicists classify the Sun as a star of average size, temperature and brightness. It consists mainly of hydrogen (71% by mass) and helium (27% by mass). Due to the very high temperatures found within the Sun, these elements exist not in the gaseous state but as plasma.

The vast amounts of energy emitted by the Sun come from thermonuclear fusion reactions occurring within the core that convert hydrogen nuclei into helium nuclei. It has been calculated that the energy output of the Sun is 3.86 x 10²³ kJ per second.

Solar wind

The outer atmosphere of the Sun is known as the corona. Temperatures within this region are extremely high, giving some of the charged particles present sufficient energy to escape from the strong gravitational pull of the Sun. This stream of charged particles emanating from the Sun in all directions at speeds of about 400 km/s is called the solar wind. It is rapidly moving plasma that pushes out to the edge of the solar system

Rights: The University of Waikato Te Whare Wānanga o Waikato

Solar wind plasma and the magnetosphere

Interaction of the Earth’s magnetosphere with the solar wind plasma. Although the solar wind is always directed away from the Sun, its intensity and speed are dependent on the Sun’s activity.

The solar wind is not uniform. Although it is always directed away from the Sun, its intensity and speed are dependent on the activity of the Sun. For example, major solar eruptions known as coronal mass ejections (CMEs) can increase the plasma density and speed of the solar wind. This can impact on the Earth’s magnetic field, causing increased auroral activity and, in extreme cases, geomagnetic storms that can disrupt communication systems and cause power surges on electrical transmission grids. Read about the event in March 2022 when two solar flares hurled charged particles at Earth.

Ionosphere

In the uppermost region of the Earth’s atmosphere, the intense incoming solar radiation causes the ionisation of gaseous atoms. Ionisation is the process in which neutral atoms or molecules gain or lose electrons to become electrically charged. This creates a mix of neutral atoms, electrons and positive ions called plasma.

The term ‘ionosphere’ is used to describe this region of near-Earth space that extends mostly within the altitude range of 85–600 km. On descending through the ionosphere, the more energetic solar radiation is absorbed, resulting in a drop-off in the degree of ionisation. In addition, the ratio of plasma/gas mix changes until, at an altitude of about 50 km, only gas exists.

Rights: The University of Waikato Te Whare Wānanga o Waikato

Layers of the ionosphere

The layers of the ionosphere change from daytime to night-time. This alters the way in which radio waves reflect off the ionosphere and back to Earth.

Various regions within the ionosphere based on electron density have been described. These vary from daytime to night-time and play a key role in absorbing harmful radiation from the Sun and outer space. In addition, the ionosphere influences radio wave propagation. It can be used to ‘bounce’ certain types of radio wave signals down to the ground, allowing for communication over very large distances.

Auroras

An aurora is a luminous glow in the E-region of the ionosphere seen mainly in high latitudes close to the poles. They are visual reminders of the solar wind – the more intense the solar wind, the more spectacular the aurora’s display of coloured lights.

Auroras are caused by high-energy charged particles from the solar wind becoming trapped in the Earth’s magnetic field. As these particles spiral back and forth along the magnetic field lines, they come down into the ionosphere near the North and South Magnetic Poles where the magnetic field lines disappear into the body of the Earth.

Rights: Fraser Gunn

Aurora Australis over Lake Tekapo

The colours of the Aurora Australis are caused by the reaction of the gases in our atmosphere with the solar winds that are emitted by the Sun.

As these high-energy charged particles collide with oxygen and nitrogen atoms in the ionosphere, they excite them to higher energy levels. On returning to their normal resting levels, the atoms emit the energy gained in the form of visible light. It is this light in shades of green and red that we see in the aurora. In the northern hemisphere, we see the Aurora Borealis, and in the southern hemisphere, we see the Aurora Australis.