Researchers calculate that Earth's atmosphere weighs about 5.15 x 10^18 kg, nearly a billion times more than the Great Pyramid of Giza.
The Earth's atmosphere consists of many layers with different temperatures and densities. Photo: Wordpress
Before we get into the weight of the atmosphere, we need to understand the concept of atmospheric pressure. At sea level, the atmosphere exerts a pressure of about 101,325 pascals. This pressure is the result of the weight of gas molecules pressing down due to gravity, according to Sci Tech Daily . Based on the atmospheric pressure over the entire surface of the Earth, scientists estimate that the total weight of the atmosphere is 5.15 x 10^18 kg, which is nearly a billion times heavier than the Great Pyramid of Giza in Egypt. The Earth's atmosphere weighs as much as a giant ocean 10 meters deep that covers the entire surface of the planet.
The Earth's atmosphere is not uniform but is divided into several layers based on temperature variations. These layers include the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer has a different density and composition. The densest layer is the troposphere, which is closest to the Earth's surface. About 78% of the atmosphere is nitrogen, 21% is oxygen, and the remaining 1% is argon, CO2, and trace amounts of other gases.
Although the total mass of the atmosphere is relatively stable (with very small seasonal variations, mainly due to changes in the amount of water vapor), its distribution can vary due to several factors. The first is altitude, as you go up, the atmospheric pressure decreases because there is less air above you. This is also why breathing at high altitudes becomes more difficult.
The second factor is temperature. On warm days, air expands and rises, making it less dense. This redistribution of air causes the atmospheric pressure to decrease near the ground because there is less weight pressing down on it. Conversely, on cold days, air contracts and sinks, causing the pressure to increase near the ground.
The final factor is humidity, humid air is less dense than dry air. This is because water molecules are not as heavy as air molecules. As humidity increases, this can affect the distribution of atmospheric mass, although the effect is less pronounced than with temperature.
By understanding these factors, we can appreciate the dynamic nature of the atmosphere and how its weight is distributed at different altitudes and conditions. The weight of the atmosphere plays an essential role in sustaining life on Earth. It allows people to breathe air, protects humanity from harmful solar radiation, and regulates the planet's temperature. Without the weight and pressure of the atmosphere, water would evaporate into space and life could not exist. Therefore, the weight of the Earth's atmosphere is a testament to the balance that sustains life on the planet.
An Khang (According to Sci Tech Daily )
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