WRAP UP Direction: State the different layers of the atmosphere and give a short description for each. 1. 2. 3. 4. 5. please pasagot po brainly or Hindi Basta kailangan Lang po
- This is the lowest part of the atmosphere - the part we live in. It contains most of our weather like our clouds, rain, snow.
2. Stratosphere
- It contains much of the ozone in the atmosphere. The increase in temperature with height occurs because of absorption of ultraviolet (UV) radiation from the sun by this ozone.
3. Mesosphere
- It contains much of the ozone in the atmosphere. The increase in temperature with height occurs because of absorption of ultraviolet (UV) radiation from the sun by this ozone.
4. Thermosphere
- The main components of air in the thermosphere include helium, atomic nitrogen, and atomic oxygen. The thermosphere absorbs a lot of the UV radiation and X-ray given off by the sun
5. Exosphere
- The exosphere is the uppermost region of Earth's atmosphere as it gradually fades into the vacuum of space. The air in the exosphere is extremely thin - in many ways it is almost the same as the airless void of outer space.
Answers & Comments
Answer:
1. Troposphere
- This is the lowest part of the atmosphere - the part we live in. It contains most of our weather like our clouds, rain, snow.
2. Stratosphere
- It contains much of the ozone in the atmosphere. The increase in temperature with height occurs because of absorption of ultraviolet (UV) radiation from the sun by this ozone.
3. Mesosphere
- It contains much of the ozone in the atmosphere. The increase in temperature with height occurs because of absorption of ultraviolet (UV) radiation from the sun by this ozone.
4. Thermosphere
- The main components of air in the thermosphere include helium, atomic nitrogen, and atomic oxygen. The thermosphere absorbs a lot of the UV radiation and X-ray given off by the sun
5. Exosphere
- The exosphere is the uppermost region of Earth's atmosphere as it gradually fades into the vacuum of space. The air in the exosphere is extremely thin - in many ways it is almost the same as the airless void of outer space.