meteorology of ozones
In the troposphere, the temperature generally decreases with altitude. The reason is that the troposphere's gases absorb very little of the. The troposphere is the layer of the atmosphere closest to the earth's surface where the weather takes place. The warmest temperatures in the troposphere are . The troposphere is the lowest layer of Earth's atmosphere, and is also where nearly all weather conditions take place. It contains approximately 75% of the atmosphere's mass and 99% of the total mass of water vapor and aerosols. The average height of the troposphere are 18 km (11 mi; 59, ft) in the The temperature of the troposphere decreases with altitude.
Atmospheric scientists use a concept called a "standard atmosphere" to represent an average atmosphere with variations caused by weather, latitude, season, and so forth, removed.
Higher up in the troposphere, where less heat from the surface warms the air, the temperature drops. Typically, the temperature drops about 6.
The rate at which the temperature changes with altitude is called the "lapse rate". Of course, the atmosphere is always changing and is never "standard". Temperatures in the troposphere, both at the surface and at various altitudes, do vary based on latitude, season, time of day or night, regional weather conditions, and so on.
When a weather phenomenon called at " temperature inversion " occurs, temperature in some part of the troposphere gets warmer with increasing altitude, contrary to the normal situation. The summit of Mt.
Everest is a little over 29, ft. Cruising altitude in a passenger jet is usually between 30, and 40, near or just above the top of the troposphere, and at the bottom of the stratosphere. Temperature remains constant between 10 and 20 km and then increases with increasing altitude between 20 and 50 km. These two sections form the stratosphere.
Changes in air temperature with altitude
The stratosphere is a very stable air layer. Increasing temperature with increasing altitude is called an inversion. This is what makes the stratosphere so stable. A kilometer is one thousand meters. Since 1 meter is about 3 feet, 10 km is about 30, feet. There are feet in a mile so this is about 6 miles. We can see the visible light.
High School Earth Science/Atmospheric Layers - Wikibooks, open books for an open world
This warms the ground. The thickness and the boundary of each layer are not identical throughout the globe but vary in different time and places Fig. Vertical temperature profile of the atmosphere. The troposphere is about 12 kilometers thick on average; it is thicker in summer than in winter. The troposphere over low latitude regions is usually thicker than over high latitude regions.
The troposphere over the equator is about 18 kilometers thick, while its thickness in the regions nearest the two poles is only about eight to nine kilometers. The temperature in the troposphere usually decreases with height at the average lapse rate of 6.
The air in the troposphere is more unstable and with strong convection.