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  1. Humidity measurement is crucial because it affects everything from human comfort to the likelihood of rain. There are various types of hygrometers; the "psychrometer" uses two thermometers (one wet, one dry) to calculate humidity through evaporation. Modern electronic hygrometers use changes in elecRead more

    Humidity measurement is crucial because it affects everything from human comfort to the likelihood of rain. There are various types of hygrometers; the “psychrometer” uses two thermometers (one wet, one dry) to calculate humidity through evaporation. Modern electronic hygrometers use changes in electrical capacitance or resistance to provide digital readings. High humidity readings suggest that the air is nearly saturated, which can lead to dew, fog or cloud formation. Conversely, low humidity indicates dry air, which promotes evaporation. Monitoring these levels helps meteorologists predict precipitation and helps industries maintain the specific environmental conditions required for manufacturing.

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  2. 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.

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  3. 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.

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  4. 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.

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  5. 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.

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