The layer above the photosphere is called the chromosphere. It is a region of the Sun's atmosphere where temperatures increase with altitude. Above the chromosphere lies the corona, which is the outermost layer of the Sun's atmosphere.
The stratosphere is the layer of the atmosphere that is relatively calm and has stable temperatures. This layer is above the troposphere and contains the ozone layer, which helps trap heat in the atmosphere. Temperatures in the stratosphere increase with altitude due to the absorption of ultraviolet radiation by the ozone layer.
The hottest layer in the atmosphere is the thermosphere, which can reach temperatures of up to 2,500 degrees Celsius (4,500 degrees Fahrenheit). Temperatures in the thermosphere increase with altitude due to the absorption of high-energy solar radiation.
No, the temperature in the troposphere decreases as the altitude increases.
Vertical temperature gradients in the atmosphere refer to the change in temperature with altitude. Typically, in the troposphere, temperatures decrease with increasing height at an average rate of about 6.5 °C per kilometer, known as the environmental lapse rate. However, in the stratosphere, temperatures can actually increase with altitude due to the absorption of ultraviolet radiation by ozone. These gradients are crucial for understanding weather patterns, stability, and atmospheric dynamics.
No, as altitude increases in the Troposphere, the temperature generally decreases. This is because the Troposphere is the layer of the Earth's atmosphere where weather occurs, and the temperature decreases with altitude due to the decrease in air pressure and thinning of the air molecules that can store heat.
Stratosphere. This is because the stratosphere is above the troposphere and contains the ozone layer, which absorbs UV radiation from the sun, causing temperatures to increase with altitude.
As altitude increases, barometric pressure decreases. This is because the air pressure decreases with increasing altitude, as there are fewer air molecules in the atmosphere exerting pressure on a given area.
Yes.
The temperature decreases
No. Atmospheric pressure decreases as altitude increases.
The layer above the photosphere is called the chromosphere. It is a region of the Sun's atmosphere where temperatures increase with altitude. Above the chromosphere lies the corona, which is the outermost layer of the Sun's atmosphere.
B. Stratosphere. In the stratosphere, temperatures generally increase with altitude due to the presence of the ozone layer, which absorbs ultraviolet radiation from the sun and heats the surrounding air.
The stratosphere is the layer of the atmosphere that is relatively calm and has stable temperatures. This layer is above the troposphere and contains the ozone layer, which helps trap heat in the atmosphere. Temperatures in the stratosphere increase with altitude due to the absorption of ultraviolet radiation by the ozone layer.
Temperature decreases as altitude increases because there are less molecules in the atmosphere to hold in the heat.
The density of air decreases with increasing altitude.
Yes, on average, temperature decreases by 6.5°C per kilometer as altitude increases in the troposphere. This is known as the normal lapse rate. However, in some regions, temperature inversions can cause temperatures to increase with altitude.