Actually, as you go from the surface of the earth to space, temperature decreases until it reaches approximately 15 km( the tropopause). Then it increases until it reaches approximately 50 km ( stratosphere) . then it decreases again until the dheight is about 80 km ( mesosphere), then it increases again in the thermosphere up until 120 km above sea level.
Temperature decreases with height due to the decrease in atmospheric pressure as altitude increases. The air molecules at higher altitudes are more spread out and have lower energy, causing the temperature to drop. This relationship is known as the lapse rate, which is approximately 6.5°C per kilometer in the troposphere.
it depends on weather and climate.
As the height of a dropped ball decreases, its potential energy also decreases. This is because potential energy is directly proportional to an object's height - the higher the object, the greater its potential energy.
As the temperature of an object decreases, its thermal energy also decreases because the particles within the object have less kinetic energy. Conversely, as the temperature increases, the thermal energy of the object increases as the particles move more rapidly, resulting in higher kinetic energy.
Yes, temperature is a measure of the average kinetic energy of particles in a substance. When thermal energy decreases, the average kinetic energy of the particles also decreases, leading to a decrease in temperature.
Generally, as height increases, atmospheric pressure decreases which results in lower air density. This is because the concentration of air molecules is lower at higher altitudes. However, local conditions such as temperature and humidity can also impact air density at a given height.
atmospheric
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Troposphere: Temperature decreases with hight Stratosphere : Temperature increases with height
Other things being equal, temperature decreases with height.
It decreases with height.
In the troposphere, temperature generally decreases with increasing altitude at a rate of around 6.5°C per kilometer due to the adiabatic cooling effect as air pressure decreases with height. This relationship is known as the environmental lapse rate and defines the temperature profile of the troposphere.
Temperature decreases with altitude. On an average, the temperature decreases by 3.5 degrees F for every 1000 ft of altitude (6.5 degrees C for every 1000 meters). The rate depends on if the air is dry or moist - in dry air, the temperature decreases more quickly, in moist air more slowly.
There are four layers of the atmosphere. At the ground is the troposphere, followed by the stratosphere, mesosphere and thermosphere. Temperature decreases with height through the troposphere, increases in the stratosphere, decreases in the mesosphere, then increases again in the thermosphere.
Pressure always decreases with height. This is because atmospheric pressure is just a measure of how much air is weighing down. So the higher you go in the atmosphere, the less air is above you (more of it is below you) and the lower the pressure will be.
it depends on weather and climate.
As the temperature decreases, kinetic energy decreases, and particles slow down.
The volume decreases!