It is directly proportional to its temperature.
The edible part, because the "lower layer of the atmosphere" would be the troposphere that takes 75% of the mass of air in the atmosphere itself. The core is the earth, and the skin is the rest of the atmosphere.
The Earth's atmosphere consists of several layers: troposphere, stratosphere, mesosphere, thermosphere, and exosphere. The thickness of each layer varies, but on average, the total thickness of the Earth's atmosphere is about 480 kilometers.
It's about 20 km near the equator and less than half that at the poles. Cold air is denser and therefore compresses much more than the warm, humid air of the tropics, so the atmosphere takes up much less space at the poles before you reach the point where there is almost no pressure left (top of the troposphere is defined as the point where temperature begins to increase with height).
Temperature, among other factors, effects the viscosity(thickness) of magma. However, for the most part, the temperature of magma is relatively consistent because magma is the type of molten rock that has not yet exited the volcano, so there are fewer factors to effect the temperature.
To calculate vertical thickness, you can use the formula: Vertical thickness = True thickness / cos(strike angle) To calculate true thickness, use the formula: True thickness = Vertical thickness * cos(strike angle)
The average tropospheric temperature refers to the typical temperature of the layer of Earth's atmosphere closest to the surface, which decreases with altitude. The thickness of the troposphere, on the other hand, refers to the vertical extent of this layer, which varies with location and weather conditions but is generally around 7-17 kilometers thick.
85km
The troposphere can vary in thickness from about 8 km at the poles to 16 km at the equator. The mesosphere is typically around 50 km thick.
The thickness of the troposphere typically increases during the summer season due to higher temperatures at the Earth's surface, which cause the air to expand and the troposphere to expand with it. This expansion leads to a thicker layer of the troposphere during this time.
The Earth's atmosphere is divided into five main layers: the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. They differ in characteristics such as temperature profiles, composition, and thickness. The troposphere is the lowest layer where weather occurs, while the thermosphere is the outermost layer where temperatures can reach thousands of degrees Celsius.
- The troposphere is the lowest part of Earth's atmosphere. - It contains about 75% of the atmosphere's mass. - It also contains about 99% of the atmosphere's water vapour and aerosols. - Most weather phenomena occur in the troposphere. - It ranges in thickness from 8km at the poles to 16km over the equator.
The thickness of Earth's atmosphere within 20 miles is approximately 11 miles. This region is known as the troposphere, where most weather phenomena occur and where the majority of Earth's atmospheric mass is concentrated. Beyond the troposphere lies the stratosphere.
taste
The edible part, because the "lower layer of the atmosphere" would be the troposphere that takes 75% of the mass of air in the atmosphere itself. The core is the earth, and the skin is the rest of the atmosphere.
You cannot. In general there is no relationship between the area of a slab and its thickness.
The Earth's atmosphere consists of several layers: troposphere, stratosphere, mesosphere, thermosphere, and exosphere. The thickness of each layer varies, but on average, the total thickness of the Earth's atmosphere is about 480 kilometers.
The troposphere is characterized by the greatest air density of any atmospheric layer. Also, it has a variable thickness of around 5 to 10 mi from the poles to the equator. The troposphere contains 99% of the water vapor contained in the atmosphere.