The Atmosphere and the Weather

What is a Gas?

The material that makes up the atmosphere is mostly in the form of a gas. A gas is one of three basic forms or "states" of matter.

1. Gas - substance in which individual molecules are not chemically bonded together. Even though many gases are not visible, it does not mean there is nothing there. Gases are composed of the same molecules that make up liquids and solids, the difference being that individual gas molecules are not chemically bonded together. Water vapor is an example of a type of gas.
2. Liquid - substance in which individual molecules are chemically bonded together, but the bonds are continuously breaking and reforming, so the substance flows. Liquid water is an example of a liquid.
3. Solid - substance in which individual molecules are tightly bonded togther in an orderly fashion. Bonds are difficult to break and the substance does not flow. Ice is an example of a solid.

Kinetic Model of Matter

The kinetic model concept is used to help us to understand and visualize how matter behaves at the level of individual molecules. A model is necessary because molecules are too small to observe individually; however, in order to understand some of the properties of matter, we need to consider how individual molecules behave. The kinetic model can be used to differentiate the behavior of solids, liquids, and gases. Look at slides 1-8 in this Kinetic Model Slide Show for a more visual explanation of the Kinetic Theroy of Matter.

We will use the kinetic model concept to help us to understand and visualize how gases behave. In the kinetic model for gases, the individual molecules that make up a gas are treated like tiny spheres, all moving in random directions. As in the atmosphere of Earth, the gas molecules (spheres) are quite small compared to the average distance between molecules (spheres). The spheres collide with each other and any solid or liquid that happens to be in the way, but they remain separate, i.e., they do not stick together. Please refer to this NASA link describing the Kinetic Model for Gases.

As described in the previous link, the energy state of a gas is determined by its

1. Temperature
2. Pressure
3. Density

Temperature of a Gas

Temperature is determined by the average speed of the molecules making up a substance. The higher the temperature, the faster they move. For gases, this is the random motion of the individual molecules that make up the gas. Random motion is disordered, i.e., individual molecules are equally likely to be moving in any direction. At temperatures common in Earth's atmosphere, the average speed of each molecule is approximately 1000 mi/hr. This is different from what we call "wind" which is ordered movement of air at the macro scale (basically the ordered movement of a fluid in a given direction). For example, when the windspeed is 10 mi/hr, it means that "blobs" of air are moving at 10 mi/hr, but individual molecules are still moving at an average speed of about 1000 mi/hr.

Using the concept of energy, the higher the temperature, the more energy that is possessed by the gas. It should make sense, then, that the higher the temperature, the higher the energy, and the faster the speed at which the molecules are moving.

We sense temperature by touch. Thermoreceptor nerve cells in our body are sensitive to the average speed at which air molecules are moving. Similarly, when air molecules strike a thermometer, energy is transferred between the thermometer and the air. The reading on the thermometer is calibrated to read the average thermal motion of all of the air molecules that collide with it.

Number Density of a Gas

The number density of a gas is defined as the number of gas molecules per unit volume. In Earth's atmosphere, near sea level there are about 2.7x10¹⁹ molecules per cm³(cubic centimeter) or 4.4x10²⁰ molecules per inch³(cubic inch). While this may seem like a lot of molecules in a small volume, molecules are very small. At this number density, there is acually much more "empty" space than the space occupied by gas molecules. By comparison, the number density for solids and liquids is much higher.

An important property of gases is that they are easily compressed, i.e., squeeze a gas together and its number density increases. In other words, we say gases are compressible because they can easily be squeezed into a smaller volume. Solids and liquids on the other hand are not easily compressed.

Pressure

From a microscopic point of view, gas pressure is caused by the collisions of gas molecules on a surface. Each individual collision provides a tiny push (or force) on the surface that it contacts. The sum total of all of these tiny forces determines the gas pressure. The physical units for pressure is force per area. More generally, all fluids (liquids and gases) exert pressure on the surfaces of solids that are immersed in them, which is simply the force of the molecules of the fluid bouncing off the solid surface. When gas is placed in a sealed container, the collisions of the randomly moving gas molecules with the sides of the container is the gas pressure.

Ideal Gas Law

The temperature, number density, and pressure of a gas are related to each other through the gas law equation:

pressure

=

temperature

x

number density

x

constant

We will use the ideal gas law and the kinetic model representation of a gas to explain the behavior of air. It much simplier to understand this material if one of the three state variable (temperature, pressure, or number density) is held constant, while the other two are allowed to change.

A. Hold number density constant

Suppose we put some air (gas) in a sealed, rigid container. No gas can enter or leave the container, so the number of gas molecules in the container cannot change. The container is rigid so that the size and shape of the container cannot change, in other words the volume of the container cannot change. Therefore, the number density (number of molecules divided by the volume of the container) cannot change.

Now suppose we heat the air in the container. This raises the temperature of the air in the container. At a higher temperature, the average speed of the individual gas molecules increases. Therefore, gas molecules hit the walls of the container harder and more often, increasing the pressure in the container. The reverse happens if you cool the air in the container. In summary, if the number density of a gas is held fixed, increasing the temperature of the gas, increases its pressure and decreasing the temperature of the gas, decreases its pressure.

B. Hold pressure constant

This situation is most applicable to understanding some of what happens in Earth's atmosphere. In this case, suppose we put some air (gas) in a sealed, flexible container like a balloon. Gas cannot enter or leave the container, but the size (volume) of the container adjusts so that the air pressure inside the container equals the air pressure outside of the container. In such a flexible container, the gas pressure inside the container (pushing outward) must always be equal to the gas pressure surrounding the container (pushing inward). If the inside pressure is greater than the outside pressure, the flexible container will pushed outward by the pressure difference, expanding the container. On the other hand, if the outside pressure is greater than the inside pressure, the flexible container will be pushed inward by the pressure difference, compressing the container. The change in volume will continue until the inside and outside pressures are equal. Later, we will apply this concept to study how individual "bubbles" of air, which we will call air parcels, will move about.

Now suppose we heat the air in the container (or an air parcel). The average speed of individual molecules increases, so they hit the walls of the container harder and more often, initially causing the pressure inside to increase. This forces the container to get larger until the air pressure inside the container (parcel) again equals the air pressure outside the container (parcel). In this case, the number density of the air in the container (parcel) has decreased because we have the same number of molecules in a larger volume. Thus, a parcel of air that is warmer than the air surrounding it will be less dense than the surrounding air and will be forced upward. This fits the old saying "warm air rises." The reverse happens if you cool the air in the container. A cold container (parcel) of air surrounded by warmer air will be denser than the surrouding air and will sink downward. In summary, if the pressure of a gas does not change, increasing the temperature of the gas causes the gas to expand (decrease number density) and decreasing the temperature of the gas causes the gas to contract (increase number density).