Located approximately 85 kilometers above the Earth's surface, the mesopause represents a thermal minimum in our atmosphere. In the mesosphere below, temperatures drop as altitude increases because of the lack of solar-absorbing gases. At the mesopause, this trend reaches its limit. Above this boundRead more
Located approximately 85 kilometers above the Earth’s surface, the mesopause represents a thermal minimum in our atmosphere. In the mesosphere below, temperatures drop as altitude increases because of the lack of solar-absorbing gases. At the mesopause, this trend reaches its limit. Above this boundary, in the thermosphere, temperatures begin to climb dramatically because molecules are directly exposed to intense X-ray and UV radiation from the sun. Despite the high temperatures in the thermosphere, the air is so thin that it would feel freezing to a human, making the mesopause the definitive “cold trap” of the planet.
When light from a distant star enters our atmosphere, it travels through air of changing refractive indices. These changes are driven by temperature fluctuations and air movement. Because stars are essentially point sources of light, even a small amount of bending (refraction) causes the light to hiRead more
When light from a distant star enters our atmosphere, it travels through air of changing refractive indices. These changes are driven by temperature fluctuations and air movement. Because stars are essentially point sources of light, even a small amount of bending (refraction) causes the light to hit the eye from slightly different angles. This causes the star to seem to “dance” or change color and intensity. Planets, being closer and appearing as tiny disks rather than points, twinkle much less because the light from different parts of the disk averages out the refractive interference.
Noctilucent clouds are the highest clouds in Earth's atmosphere. They form under extremely cold conditions—below -120°C—when water vapor freezes onto "smoke" particles left behind by meteors or volcanic dust. Because the mesosphere is incredibly dry, these clouds are very thin and only become visiblRead more
Noctilucent clouds are the highest clouds in Earth’s atmosphere. They form under extremely cold conditions—below -120°C—when water vapor freezes onto “smoke” particles left behind by meteors or volcanic dust. Because the mesosphere is incredibly dry, these clouds are very thin and only become visible when the lower atmosphere is in shadow. Their increasing frequency in recent years is a subject of scientific study, as some researchers believe they are linked to rising methane levels in the upper atmosphere, which breaks down to form the water vapor necessary for these ice crystals to grow.
Solar ultraviolet radiation is categorized into UV-A, UV-B and UV-C based on wavelength. The ozone layer acts as a selective filter. It completely blocks UV-C, which is highly lethal but luckily absorbed by oxygen and ozone high up. UV-B, however, is only partially absorbed. A thinning ozone layer lRead more
Solar ultraviolet radiation is categorized into UV-A, UV-B and UV-C based on wavelength. The ozone layer acts as a selective filter. It completely blocks UV-C, which is highly lethal but luckily absorbed by oxygen and ozone high up. UV-B, however, is only partially absorbed. A thinning ozone layer leads to an increase in UV-B reaching the surface, which disrupts photosynthesis in plants, kills phytoplankton in the oceans and damages the DNA of humans and animals. This is why maintaining the integrity of the stratosphere’s chemical balance is a global priority for biological health.
As an air parcel rises, it expands and cools. If the air is dry, it cools at the Dry Adiabatic Lapse Rate. However, once the air cools to its dew point, water vapor condenses into clouds. This phase change is an exothermic process, releasing latent heat into the air parcel. This added heat offsets sRead more
As an air parcel rises, it expands and cools. If the air is dry, it cools at the Dry Adiabatic Lapse Rate. However, once the air cools to its dew point, water vapor condenses into clouds. This phase change is an exothermic process, releasing latent heat into the air parcel. This added heat offsets some of the cooling caused by expansion. Therefore, moist air stays warmer than dry air at the same altitude, which is a major factor in atmospheric stability and the development of massive, towering thunderstorms that can reach the tropopause.
What is the boundary called where the cooling rate of the atmosphere changes at the top of the Mesosphere?
Located approximately 85 kilometers above the Earth's surface, the mesopause represents a thermal minimum in our atmosphere. In the mesosphere below, temperatures drop as altitude increases because of the lack of solar-absorbing gases. At the mesopause, this trend reaches its limit. Above this boundRead more
Located approximately 85 kilometers above the Earth’s surface, the mesopause represents a thermal minimum in our atmosphere. In the mesosphere below, temperatures drop as altitude increases because of the lack of solar-absorbing gases. At the mesopause, this trend reaches its limit. Above this boundary, in the thermosphere, temperatures begin to climb dramatically because molecules are directly exposed to intense X-ray and UV radiation from the sun. Despite the high temperatures in the thermosphere, the air is so thin that it would feel freezing to a human, making the mesopause the definitive “cold trap” of the planet.
See lessWhich atmospheric phenomenon is responsible for the ‘twinkling’ of stars?
When light from a distant star enters our atmosphere, it travels through air of changing refractive indices. These changes are driven by temperature fluctuations and air movement. Because stars are essentially point sources of light, even a small amount of bending (refraction) causes the light to hiRead more
When light from a distant star enters our atmosphere, it travels through air of changing refractive indices. These changes are driven by temperature fluctuations and air movement. Because stars are essentially point sources of light, even a small amount of bending (refraction) causes the light to hit the eye from slightly different angles. This causes the star to seem to “dance” or change color and intensity. Planets, being closer and appearing as tiny disks rather than points, twinkle much less because the light from different parts of the disk averages out the refractive interference.
See lessWhat are ‘Noctilucent’ clouds primarily composed of? (A) Water droplets (B) Sulfuric acid (C) Ice crystals (D) Methane gas
Noctilucent clouds are the highest clouds in Earth's atmosphere. They form under extremely cold conditions—below -120°C—when water vapor freezes onto "smoke" particles left behind by meteors or volcanic dust. Because the mesosphere is incredibly dry, these clouds are very thin and only become visiblRead more
Noctilucent clouds are the highest clouds in Earth’s atmosphere. They form under extremely cold conditions—below -120°C—when water vapor freezes onto “smoke” particles left behind by meteors or volcanic dust. Because the mesosphere is incredibly dry, these clouds are very thin and only become visible when the lower atmosphere is in shadow. Their increasing frequency in recent years is a subject of scientific study, as some researchers believe they are linked to rising methane levels in the upper atmosphere, which breaks down to form the water vapor necessary for these ice crystals to grow.
See lessWhich specific wavelength of solar radiation is primarily absorbed by the Ozone layer?
Solar ultraviolet radiation is categorized into UV-A, UV-B and UV-C based on wavelength. The ozone layer acts as a selective filter. It completely blocks UV-C, which is highly lethal but luckily absorbed by oxygen and ozone high up. UV-B, however, is only partially absorbed. A thinning ozone layer lRead more
Solar ultraviolet radiation is categorized into UV-A, UV-B and UV-C based on wavelength. The ozone layer acts as a selective filter. It completely blocks UV-C, which is highly lethal but luckily absorbed by oxygen and ozone high up. UV-B, however, is only partially absorbed. A thinning ozone layer leads to an increase in UV-B reaching the surface, which disrupts photosynthesis in plants, kills phytoplankton in the oceans and damages the DNA of humans and animals. This is why maintaining the integrity of the stratosphere’s chemical balance is a global priority for biological health.
See lessWhat is the ‘Lapse Rate’ called when it is influenced by the condensation of water vapor?
As an air parcel rises, it expands and cools. If the air is dry, it cools at the Dry Adiabatic Lapse Rate. However, once the air cools to its dew point, water vapor condenses into clouds. This phase change is an exothermic process, releasing latent heat into the air parcel. This added heat offsets sRead more
As an air parcel rises, it expands and cools. If the air is dry, it cools at the Dry Adiabatic Lapse Rate. However, once the air cools to its dew point, water vapor condenses into clouds. This phase change is an exothermic process, releasing latent heat into the air parcel. This added heat offsets some of the cooling caused by expansion. Therefore, moist air stays warmer than dry air at the same altitude, which is a major factor in atmospheric stability and the development of massive, towering thunderstorms that can reach the tropopause.
See less