The Earth's inner core has the greatest temperature, reaching up to around 5700 degrees Celsius. The layer with the greatest pressure is the inner core as well, with pressures exceeding 330 to 360 gigapascals.
The temperature zone layer of Earth's atmosphere shown in the cross-section is the stratosphere. This layer is characterized by an increase in temperature with altitude due to the presence of the ozone layer, which absorbs and scatters UV radiation from the sun.
The layer of the Earth's atmosphere that fits this description is the thermosphere. In the thermosphere, there is little to no water vapor, the atmospheric pressure is less than 1.0 atmosphere, and the air temperature increases with altitude due to the absorption of solar radiation.
The greatest atmospheric pressure occurs in the troposphere, which is the lowest layer of the Earth's atmosphere. The pressure decreases rapidly with height in the troposphere, and it is where weather events and phenomenon like clouds, rain, and storms take place.
At the very center.
Layers in Earth's atmosphere are primarily separated based on temperature variations caused by differences in altitude and composition. The troposphere is the layer closest to the Earth's surface, where temperature generally decreases with altitude. Above that is the stratosphere, where temperature begins to increase due to the presence of the ozone layer.
This happens mostly in the core - near the center of the Sun, where temperature and pressure are greatest.
This happens mostly in the core - near the center of the Sun, where temperature and pressure are greatest.
This happens mostly in the core - near the center of the Sun, where temperature and pressure are greatest.
the mantle
The temperature zone layer of Earth's atmosphere shown in the cross-section is the stratosphere. This layer is characterized by an increase in temperature with altitude due to the presence of the ozone layer, which absorbs and scatters UV radiation from the sun.
The thermosphere is the layer of the atmosphere that has the greatest range in temperature, with temperatures increasing with altitude due to the absorption of solar radiation. Temperature in the thermosphere can vary from below -100°C at the bottom to over 2,500°C at higher altitudes.
The layer of the atmosphere with the greatest temperature range is the stratosphere. In this layer, temperatures increase with altitude due to the absorption of ultraviolet radiation by the ozone layer, leading to significant temperature variations. The temperature can vary from around -60°C (-76°F) at the lower stratosphere to about 0°C (32°F) near the stratopause, resulting in a substantial temperature range.
The layer of the Earth's atmosphere that fits this description is the thermosphere. In the thermosphere, there is little to no water vapor, the atmospheric pressure is less than 1.0 atmosphere, and the air temperature increases with altitude due to the absorption of solar radiation.
The greatest atmospheric pressure occurs in the troposphere, which is the lowest layer of the Earth's atmosphere. The pressure decreases rapidly with height in the troposphere, and it is where weather events and phenomenon like clouds, rain, and storms take place.
At the very center.
Stiffer mantle.
The core because all its heat and pressure is in the misddle where everything started -Emily