When it receives the aids virus.
Scientists have shot aids into the clouds, angering them with this mutation.
It is their immune systems and temperment that is unstable.
An air parcel is a theoretical volume of air used in meteorology to study and analyze atmospheric processes. It is typically considered as a small, imaginary cube of air that retains its properties as it moves within the atmosphere. By tracking the behavior of air parcels, meteorologists can better understand the dynamics of weather systems.
An air parcel cools down when it rises to higher altitudes in the atmosphere, where the air pressure decreases. As the air pressure decreases, the air parcel expands and does work on its surroundings, which leads to a decrease in temperature due to the loss of heat energy.
An air parcel cools as it rises in the atmosphere due to a decrease in air pressure. As the parcel moves to higher altitudes, the lower pressure causes it to expand, which leads to a decrease in temperature. This process is known as adiabatic cooling.
Yes, unstable air is necessary for a thunderstorm to develop. Unstable air is characterized by a rapid decrease in temperature with height, creating buoyant conditions that promote the rapid upward movement of air and the formation of thunderstorms.
As a parcel of air rises, it expands and cools adiabatically. This cooling causes relative humidity to increase, as the air temperature drops and its capacity to hold moisture decreases. If the air parcel reaches its dew point temperature, the relative humidity will reach 100% and condensation or cloud formation may occur.
An air parcel is a theoretical volume of air used in meteorology to study and analyze atmospheric processes. It is typically considered as a small, imaginary cube of air that retains its properties as it moves within the atmosphere. By tracking the behavior of air parcels, meteorologists can better understand the dynamics of weather systems.
An air parcel is an imaginary body of air with the basic properties of atmospheric air.
When a parcel of air is saturated with water vapor the relative humidity of that parcel of air is 100%.
Why is Greece's environment considered unstable?
how heat would change the density of a parcel of air?
A buoyant parcel of air exhibits vertical motion in the atmosphere due to its lower density compared to the surrounding air. This parcel of air rises when it is warmer than the air around it and sinks when it is cooler, following the principles of buoyancy.
An air parcel cools down when it rises to higher altitudes in the atmosphere, where the air pressure decreases. As the air pressure decreases, the air parcel expands and does work on its surroundings, which leads to a decrease in temperature due to the loss of heat energy.
what is the only way air can become unstable
Why is Greece's environment considered unstable?
Warm air rises....and when it rises it becomes cooler. ...If the pressure of surrounding air is reduced then the rising air parcel will expand. The molecules are doing work as they expand . This will affect the parcel's temperature.
When a parcel of air is less dense than the surrounding air, it will rise due to buoyancy forces. As the parcel rises, it will expand and cool adiabatically, which can lead to cloud formation and possibly precipitation. This process is known as atmospheric convection.
An air parcel cools as it rises in the atmosphere due to a decrease in air pressure. As the parcel moves to higher altitudes, the lower pressure causes it to expand, which leads to a decrease in temperature. This process is known as adiabatic cooling.