What are ionospheric currents?

The ionospheric currents are a highly variable part of the coupled Magnetosphere – Ionosphere – Thermosphere (MIT) system. This system is driven by the solar wind and Interplanetary Magnetic Field (IMF) interaction with the Earth’s magnetosphere.

What is the best layer for ionosphere?

The F layer or region, also known as the Appleton–Barnett layer, extends from about 150 km (90 mi) to more than 500 km (300 mi) above the surface of Earth. It is the layer with the highest electron density, which implies signals penetrating this layer will escape into space.

What is ionosphere physics?

The ionosphere is the part of the atmosphere that is ionized by solar radiation. It plays an important part in atmospheric electricity and forms the inner edge of the magnetosphere. It has practical importance because, among other functions, it influences radio propagation to distant places on the Earth.

Who discovered the ionosphere?

Discovery of the Ionosphere

1820 Hans Christian Oersted discovers that electricity and magnetism are related
1909 Marconi awarded Nobel Prize
1924 Edward Appleton and others develop the ionosonde and begin ground-based soundings; prove existence of ionosphere
1925 Appleton discovers second layer (the F region)

What is Pedersen conductivity?

Pedersen conductivity is for the direction vertical to the magnetic field and parallel to the electric field. It is denoted as “σ1”. Hall conductivity. Hall conductivity is for the direction vertical to both the magnetic and electric fields. It is denoted as “σ2”.

Can you breathe in the ionosphere?

2. The ionosphere is where Earth’s atmosphere meets space. The ionosphere stretches roughly 50 to 400 miles above Earth’s surface, right at the edge of space. Along with the neutral upper atmosphere, the ionosphere forms the boundary between Earth’s lower atmosphere — where we live and breathe — and the vacuum of space …

What is ionosphere also called?

It plays an important part in atmospheric electricity and forms the inner edge of the magnetosphere. It has practical importance because, among other functions, it influences radio propagation to distant places on the Earth. It is also called as thermosphere.

Why is the ionosphere so important to humans?

the ionosphere is important because it reflects and modifies radio waves used for communication and navigation. Other phenomena such as energetic charged particles and cosmic rays also have an ionizing effect and can contribute to the ionosphere. The density of the ionosphere changes accordingly.

Is the ionosphere hot or cold?

In the ionosphere, radiation from the sun is so powerful that it ionizes, or breaks electrons free from different atoms present in the atmosphere. Due to fluxes in solar radiation, temperatures in the ionosphere vary from 200 Kelvin (or -99 degrees Fahrenheit) to 500K (or 440 degrees Fahrenheit).

Is ionosphere a layer in the atmosphere?

The active, changing layer An interesting layer called the ionosphere overlaps the mesosphere, thermosphere, and exosphere. It’s a very active part of the atmosphere, and it grows and shrinks depending on the energy it absorbs from the sun.

Is the ionosphere conductive?

As a consequence, ionospheric conductivity is highly anisotropic, resulting in values that are so high parallel to the field that the magnetic field lines are nearly equipotential lines.

What kind of currents are in the ionosphere?

Ionospheric currents The ionosphere consists of several layers, generally referred to as D (60 km – 90 km), E (90 km – 150 km) and F ( >150 km) regions. Horizontal ionospheric currents, such as the polar electrojets, the equatorial electrojetand the Sq (solar quiet) current systems are largely confined to the E region.

How much current is in the ionospheric dynamo region?

This current configuration is fixed to the sun, while the earth rotates beneath it. A total current of about 140 kA flows within one daytime vortex. The rotating Sq current and the electrically conducting earth interior behave like a huge transformer with the dynamo region as the primary winding and the earth as the secondary winding.

How are the critical frequencies of the ionosphere measured?

Ionograms show the virtual heights and critical frequencies of the ionospheric layers and which are measured by an ionosonde. An ionosonde sweeps a range of frequencies, usually from 0.1 to 30 MHz, transmitting at vertical incidence to the ionosphere.

How does the geomagnetic dip equator affect the ionosphere?

Near the geomagnetic dip equator, a west-east directed electric field generates vertical Hall currents which cannot close. Therefore, a vertical polarization field builds up generating a horizontal Hall current which adds to the Pedersen current.

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