1.-The atmosphere can be divided into four layers based on temperature variations. The layer closest to the Earth is called the troposphere. Above this layer is the stratosphere, followed by the mesosphere, then the thermosphere.
2. Troposphere= No
Explanation; As the density of the gases in this layer decrease with height, the air becomes thinner. Therefore, the temperature in the troposphere also decreases with height in response. As one climbs higher, the temperature drops from an average around 62°F (17°C) to -60°F (-51°C) at the tropopause.
Mesosphere= Yes
Explanation; the region of the atmosphere between about 50 kilometers (31 miles) and 80-85 kilometers (50-53 miles), extending from the top of the stratosphere to the upper temperature minimum; it is characterized by a broad temperature maximum (near 0 degrees Celsius) at its base, from which the temperature
Stratosphere= Yes
Explanation; Heat is produced in the process of the formation of Ozone and this heat is responsible for temperature increases from an average -60°F (-51°C) at tropopause to a maximum of about 5°F (-15°C) at the top of the stratosphere. This increase in temperature with height means warmer air is located above cooler air decreases to a minimum.
Thermosphere= No
Explanation; The thermosphere is typically about 200° C (360° F) hotter in the daytime than at night, and roughly 500° C (900° F) hotter when the Sun is very active than at other times. Temperatures in the upper thermosphere can range from about 500° C (932° F) to 2,000° C (3,632° F) or higher.
3. Troposphere
Temparature= 62°F (17°C)
Altitude= 14.5 kilometers
Stratosphere
Temperature = 60 degrees Fahrenheit (negative 51 degrees Celsius)
Altitude=15 miles (25 km)
Mesosphere
Temperature =-90° C (-130° F)
Altitude= 50 to 85 km (31 to 53 miles)
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Answers & Comments
1.-The atmosphere can be divided into four layers based on temperature variations. The layer closest to the Earth is called the troposphere. Above this layer is the stratosphere, followed by the mesosphere, then the thermosphere.
2. Troposphere= No
Explanation; As the density of the gases in this layer decrease with height, the air becomes thinner. Therefore, the temperature in the troposphere also decreases with height in response. As one climbs higher, the temperature drops from an average around 62°F (17°C) to -60°F (-51°C) at the tropopause.
Mesosphere= Yes
Explanation; the region of the atmosphere between about 50 kilometers (31 miles) and 80-85 kilometers (50-53 miles), extending from the top of the stratosphere to the upper temperature minimum; it is characterized by a broad temperature maximum (near 0 degrees Celsius) at its base, from which the temperature
Stratosphere= Yes
Explanation; Heat is produced in the process of the formation of Ozone and this heat is responsible for temperature increases from an average -60°F (-51°C) at tropopause to a maximum of about 5°F (-15°C) at the top of the stratosphere. This increase in temperature with height means warmer air is located above cooler air decreases to a minimum.
Thermosphere= No
Explanation; The thermosphere is typically about 200° C (360° F) hotter in the daytime than at night, and roughly 500° C (900° F) hotter when the Sun is very active than at other times. Temperatures in the upper thermosphere can range from about 500° C (932° F) to 2,000° C (3,632° F) or higher.
3. Troposphere
Temparature= 62°F (17°C)
Altitude= 14.5 kilometers
Stratosphere
Temperature = 60 degrees Fahrenheit (negative 51 degrees Celsius)
Altitude=15 miles (25 km)
Mesosphere
Temperature =-90° C (-130° F)
Altitude= 50 to 85 km (31 to 53 miles)
Ayesha: Ikaw nalang sumagot sa iba sumabog na utak ko kakaisip TwT
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