stratosphere
Electrically charged particles are found in the ionosphere, a region of the Earth's upper atmosphere that extends from about 48 kilometers (30 miles) to 965 kilometers (600 miles) above the Earth's surface. The ionosphere contains ions and free electrons that are formed due to the ionization of molecules by solar radiation.
The layer of the atmosphere that contains the ionosphere is the thermosphere. This region is located between the mesosphere and the exosphere and is known for its high temperatures and the presence of ionized particles that allow for the reflection of radio waves.
When air pressure is constant throughout a region of the atmosphere the region is in a state is called equilibrium.
hi koleSPACE
The region of space affected by Earth's magnetic field is called the magnetosphere. It acts as a protective shield around the Earth, interacting with the solar wind and trapping charged particles. This region extends tens of thousands of kilometers into space on the side facing away from the Sun.
The glowing region of the atmosphere caused by charged particles from the sun is called an aurora. Auroras are usually seen in the polar regions and are known as the aurora borealis in the northern hemisphere and aurora australis in the southern hemisphere.
An electric field is a region in which charged particles can be pushed or pulled due to the presence of other charged particles. The strength of the electric field determines the force experienced by charged particles within the region.
Electrically charged particles, also known as ions, are primarily found in the ionosphere layer of Earth's atmosphere. This region is located between 48 km and 965 km above the Earth's surface and is where solar radiation interacts with the gases in the atmosphere to create ions.
The ionosphere is a region of the Earth's upper atmosphere containing ions and free electrons. It is composed of several layers of the atmosphere where solar radiation can ionize atoms and molecules, creating regions of charged particles that affect radio wave propagation and communication.
It is the northern lights. The northern lights are caused by charged particles that sometimes are sucked into the Earth on either ends of the poles. They also have other names but I can't remember. Thanks!!
Electrically charged particles are found in the ionosphere, a region of the Earth's upper atmosphere that extends from about 48 kilometers (30 miles) to 965 kilometers (600 miles) above the Earth's surface. The ionosphere contains ions and free electrons that are formed due to the ionization of molecules by solar radiation.
Auroras occur in the thermosphere, which is the region of the atmosphere located between the mesosphere and the exosphere. This is where charged particles from the sun interact with gases in the Earth's atmosphere, creating the colorful light displays known as auroras.
The region within the lower portion of the thermosphere where particles become electrically charged is called the ionosphere. This layer of the atmosphere contains a high concentration of ions and free electrons, which allows it to reflect radio waves and facilitate long-distance communication.
Aurora borealis or aurora australis, also known as the Northern Lights and Southern Lights respectively, are colorful and shimmering light displays in the sky caused by solar wind particles interacting with Earth's magnetic field. These charged particles collide with gases in the atmosphere, producing the glowing effect seen in the polar regions.
Solar winds come from the outer layer of the Sun's atmosphere called the corona. This region is extremely hot and contains charged particles that are ejected into space, creating the solar wind.
the exosphere is a layer in space and generally is not taken as one of the atmospheric layers whereas the ionosphere is a layer containing highly charged anions and is an upper part of the thermosphere.
A region of air with relatively few particles is known as a low-pressure system or a partial vacuum. These regions can occur naturally, such as at high altitudes in the atmosphere, or they can be created artificially, such as in a vacuum chamber.