Table of Contents
- 1 What causes water vapor to condense out of air?
- 2 What are 2 important things about the water vapor in our atmosphere?
- 3 Which two events must occur for condensation to happen?
- 4 What 2 things can increase the rate of condensation?
- 5 Which of the following processes in the water cycle causes the formation of clouds?
- 6 How is condensation related to the natural water cycle?
- 7 How does sunlight affect the temperature of a condenser?
What causes water vapor to condense out of air?
Condensation generally occurs in the atmosphere when warm air rises, cools and looses its capacity to hold water vapor. As a result, excess water vapor condenses to form cloud droplets.
What are the factors that lead to condensation?
The factors governing condensation
- The water vapour content of the air.
- Inside room temperature.
- Outside temperature.
- Internal and external temperature variation.
What are 2 important things about the water vapor in our atmosphere?
Water vapor is also the most important greenhouse gas in the atmosphere. Heat radiated from Earth’s surface is absorbed by water vapor molecules in the lower atmosphere. The water vapor molecules, in turn, radiate heat in all directions. Some of the heat returns to the Earth’s surface.
What must happen to water in the air to become condensation?
Condensation happens one of two ways: Either the air is cooled to its dew point or it becomes so saturated with water vapor that it cannot hold any more water. Dew point is the temperature at which condensation happens. When warm air hits the cold surface, it reaches its dew point and condenses.
Which two events must occur for condensation to happen?
Condensation is the term for water changing state from a vapor to a liquid. The process requires the presence of water vapor in the atmosphere, falling temperature and the presence of another object for water vapor to condense around.
What are the two necessary conditions for condensation to occur?
Two things must be present for condensation to occur: warm moist air, and cool surface temperatures below the dew point. The proper control of these two factors can minimize condensation.
What 2 things can increase the rate of condensation?
Making water vapor colder increases the rate of condensation. Increasing the concentration of water vapor in the air increases the rate of condensation.
How is water vapor created?
Water vapour is water in gaseous instead of liquid form. It can be formed either through a process of evaporation or sublimation. Water vapour in the atmosphere is often below its boiling point. When water is boiled the water evaporates much faster and makes steam.
Which of the following processes in the water cycle causes the formation of clouds?
Condensation is the process by which water vapor in the air is changed into liquid water. Condensation is crucial to the water cycle because it is responsible for the formation of clouds.
What do you need to know about condensation in air?
Two things must be present for condensation to occur: warm moist air, and cool surface temperatures below the dew point. The proper control of these two factors can minimize condensation.
Condensation and the Water Cycle. Condensation is the process by which water vapor in the air is changed into liquid water. Earth’s water is always in movement, and the natural water cycle, also known as the hydrologic cycle, describes the continuous movement of water on, above, and below the surface of the Earth.
Why does water have to enter from the bottom of a condenser?
By allowing water to enter from the lower hole, the entire volume of the chamber would have to be filled before the water left, provide far more efficient cooling, It also prevents thermal shock which could cause the glass to crack.
How does sunlight affect the temperature of a condenser?
(Right) As ambient air diffuses through the porous MOF, water molecules preferentially attach to the interior surfaces. Sunlight entering through a window heats up the MOF and drives the bound water toward the condenser, which is at the temperature of the outside air.