In life, why does the higher the altitude, the lower the temperature?

The higher the altitude, the thinner the air, the fewer molecules in the air under the same circumstances, the less material that can absorb the sun's energy, and the less energy absorbed, the temperature will naturally be lower than at lower altitudes.

Because of the higher altitude, the air is relatively thin, resulting in its poor energy storage capacity, and ground radiation is also a major factor affecting temperature, and the air absorbs heat energy poorly.

The Earth is too far from the Sun, so going to a higher altitude makes no difference to the heat provided by the Sun. However, the higher the altitude, the thinner the air, which leads to poor heat storage capacity, and ultimately the higher the altitude, the lower the temperature.

The higher the altitude, the more space there is for the molecules in the air to move, and the chance of molecule collisions decreases, thus allowing the kinetic energy of the molecules to be distributed over a large area, thus reducing the average temperature.

Mainly because of the high air pressure and low air thinness, the atmosphere here is relatively poorly heated, resulting in a lot of heat loss.

Because the higher the altitude, the thinner the air, and the thinner the air, the lower the temperature of the surrounding air, the higher the altitude, the cooler the temperature.

The higher the altitude, the thinner the air and the lower the air pressure. And the temperature will decrease as the air pressure drops.

It's because it's getting closer to the sun, so the temperature is getting higher and higher, but the altitude is getting higher and higher, but the temperature is getting lower and lower.

Because the higher the altitude, the lower the air pressure, and the lower the air pressure, the temperature will be very low, so this phenomenon occurs.

The ground, on the other hand, can absorb visible energy and be heated, which in turn releases infrared radiation with longer wavelengths. Electromagnetic radiation in this band can be absorbed by the atmosphere, raising temperatures. So, while the main energy** of the Earth's atmosphere temperature is the sun overhead, it directly heats the atmosphere on the Earth's surface.

This is what we see in the summer when the heat wave rises on the ground, heating the atmosphere by convection.

The range of warmth of fire on Earth is very limited, and small changes in distance can make a big difference, and this change is noticeable to us. And since the Earth is 100 million kilometers from the Sun, this is only the average distance, and the difference between the Earth's aphelion and perihelion is about 5 million kilometers. The more direct the sun, the warmer the ground, for example, the equator is warm all year round.

The higher an air mass rises, the more its temperature drops. So, although the warm air rises, it cools down quickly as it moves to higher altitudes.

While some of the sun's heat is absorbed by the Earth's surface and atmosphere, more heat is absorbed by the ground, resulting in relatively high temperatures close to the ground. Also, the further up you go, the thinner the air becomes, as does its ability to absorb and retain heat That's why Venus is not the closest planet to the Sun, but it is the planet with the highest average temperature. In the case of the Earth, the difference between aphelion and perihelion is about 5 million kilometers.

On the summer solstice, when the Northern Hemisphere is in summer, the Earth is furthest from the Sun. Visible distance is not the only factor that determines the temperature of the Earth's surface.

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Because the higher the altitude, the air is very thin, the ability to store heat will be very poor, and the altitude is too high to receive very little heat, so the temperature will be very low.

Because the higher the altitude, the less organisms are present, and the air and oxygen are particularly thin, so the temperature is getting lower and lower.

This is because the higher the altitude, the lower the amount of gases in the air and the inability to transmit heat, so the lower the temperature.

Because the higher the altitude, the less organisms exist, and the atmosphere and oxygen are particularly thin, so the temperature is getting lower and lower.

The higher the altitude, the lower the temperature mainly for the following reasons: first, at high altitude, the thinner the air and poor heat storage capacity, second, at high altitude, the less reflected heat energy from the ground, and the weaker the reverse radiation, third, the higher the altitude, the thinner the cloud layer, and the faster the heat loss.

Topography has a certain influence on the climate, with every 100 meters above sea level decreasing, and at the same latitude, the land temperature is high in summer and the sea temperature is low, and the opposite is true in winter.

Altitude is the abbreviation of altitude, which generally refers to the vertical distance between a certain place on the ground above sea level, and is the height difference between a certain place and the sea level.

The atmosphere is mainly divided into five layers, from bottom to top, in the order of troposphere, stratosphere, mesosphere, warm layer and fugitive layer, in the troposphere, the higher the altitude, the lower the temperature, in the stratosphere, the higher the altitude, the higher the temperature.

Because the altitude is higher and the atmospheric pressure is lower, less heat is retained, so the temperature is lower. In addition, the air at high altitudes is thin, and most of the solar radiation heat absorbed by the ground will be lost to the middle of the universe, that is, the heat preservation of the atmosphere is weak, resulting in low temperatures.

In contrast, at lower altitudes, where the atmospheric pressure is higher, the air molecules do not move freely enough, they carry a lot of energy and collide with each other more frequently, resulting in higher temperatures. Therefore, it is hotter under the mountain than on the mountain. This law of physics applies anywhere, whether at the equator or at the poles.

Factors influencing air temperature:

1. Location. The temperature decreases from low latitudes to high latitudes. Due to the difference in the thermal properties of land and sea, land and sea at the same latitude have a larger warming range in summer and a larger cooling range in winter.

2. Atmosphere. Cloudy during the day with cooler temperatures; The nights will be cloudy with high temperatures; It will be cloudy throughout the day, with a small temperature difference between day and night; It was sunny all day, and there was a large temperature difference between day and night.

3. Terrain. The higher the altitude, the lower the temperature. The temperature in the mountain basins and river valleys is high. The sunny slopes of the mountains are warmer than the shady slopes.

4. Ocean currents. The warm current warms and humidifies, and the cold current cools and dehumidifies.

5. Vegetation. The vegetation coverage is high and the temperature difference is small.