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Which layer of the atmosphere helps in radio transmission?

Ionosphere of the atmosphere helps in radio transmission. various layers in the atmosphere: our atmosphere is composed of many components. but the structure of the atmosphere is a combination of various layers. the composition of the atmosphere is divided into five layers based on temperature. these layers are as follows: troposphere stratosphere mesosphere thermosphere exosphere ionosphere the ionosphere is the lowest part of the thermosphere. ions are electrically charged particles that make up the ionosphere. this layer is defined as the layer of the atmosphere of earth that is ionized by cosmic and solar radiation. it lies between 80 and 400 kilometers above the mesopause..

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18. In ________ layer of atmosphere TV waves do not get reflected. Hence, artificial satellites are used for television transmission.

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10 Things to Know About the Ionosphere

The limb of Earth with glowing auroras and a thin band of atmosphere under part of the International Space Station.

1. It’s home to all the charged particles in Earth's atmosphere

Earth’s ionosphere overlaps the top of the atmosphere and the very beginning of space. The Sun cooks gases there until they lose an electron or two, which creates a sea of electrically charged particles.

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.

Illustration showing Earth's ionosphere "breathing."

3. It changes – sometimes unpredictably

The ionosphere is constantly changing. Because it's formed when particles are ionized by the Sun’s energy, the ionosphere changes from Earth’s day side to night side. When night falls, the ionosphere thins out as previously ionized particles relax and recombine back into neutral particles. But there are also more unpredictable changes, caused by factors both from Earth below and space above, that make it hard to know exactly what the ionosphere will be like at a given time.

Illustration showing satellites passing through Earth's ionosphere.

4. It's home to many of our satellites

This boundary to space is right where many of our Earth-orbiting satellites hang out, including the International Space Station. That means these satellites can be affected by the constantly changing conditions in the ionosphere – including sudden swells of charged particles that increase drag on satellites and shorten their orbital lifetimes, or how long they can continue orbiting Earth.

5. Disturbances there can disrupt signals

The ionosphere also plays a role in our everyday communications and navigation systems. Radio and GPS signals travel through this layer of the atmosphere, or rely on bouncing off the ionosphere to reach their destinations. In both cases, changes in the ionosphere's density and composition can disrupt these signals.

radio waves travel in which layer of atmosphere

6. It's influenced by weather

Weather from Earth, like hurricanes or large thunderstorm systems, can create pressure waves that ripple up into the ionosphere. This is one of the factors that can cause changes in the ionosphere.

These effects were only discovered when data from NASA satellites revealed connections between weather conditions and changes in Earth's ionosphere.

A massive coronal mass ejection erupting from the Sun.

7. …And it’s influenced by space weather too

Because the ionosphere is made up of charged particles, it's uniquely reactive to the changing magnetic and electric conditions in space. These conditions – along with other events like bursts of charged particles – are called space weather and usually connected to solar activity. Along with regular weather from here on Earth, space weather is the other major factor that impacts the ionosphere.

8. The ionosphere constantly glows

Airglow is what we call the bright swaths of light that shine from Earth's upper atmosphere. It happens when atoms and molecules in the upper atmosphere, excited by sunlight, emit light to shed their excess energy. Or, it can happen when atoms and molecules that have been ionized by sunlight collide with and capture a free electron. In both cases, they eject a particle of light – called a photon – in order to relax again.

Airglow isn't just a beautiful sight: It's a useful marker for what happens in the ionosphere. Each atmospheric gas has its own favored airglow color depending on the gas, altitude region, and excitation process, so we can use airglow to study where these gases are and how they behave.

9. We study the ionosphere with invisible types of light

In January 2018, NASA sent GOLD – short for Global-scale Observations of the Limb and Disk – to space aboard a commercial communications satellite. From its steady vantage point 22,000 miles over the Western Hemisphere, GOLD creates full-disk images of Earth in far-ultraviolet light, a type of light that's invisible to our eyes, but reveals day-to-day changes in the upper atmosphere.

10. More images from the ionosphere

On Oct. 10, 2019, NASA launched ICON – the Ionospheric Connection Explorer – to join GOLD in studying the ionosphere. The spacecraft is now in low-Earth orbit, 360 miles above Earth. ICON studies the ionosphere using a combination of airglow, invisible wavelengths of light, and direct measurements of its surrounding particles. And the mission just sent back its first science images ! Together, GOLD and ICON are helping us learn a lot more about the ionosphere, this part of space that is closest to home.

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