The formation of fog is a physical change, not a chemical one.
Salt and chemical grains can act as cloud condensation nuclei, providing a surface for water vapor to condense on and form cloud droplets. These droplets can eventually coalesce and grow large enough to fall as rain. In fog formation, these particles can also help water vapor condense into tiny droplets, creating the fog.
when we take a bath the mirror has on it some gas, the steam on the sauna, and maybe fire
Some examples of colloid heterogeneous mixtures include milk, mayonnaise, gelatin, fog, whipped cream, and paint. These mixtures have particles that are dispersed throughout a medium but do not settle out.
In the liquid state, water is water. In a solid state, water is ice. In a gas state water is called water vapor.
No, the fog appearing on the windshield from cold weather is a physical change. It occurs when warm, moisture-laden air inside the car comes into contact with the cold windshield, causing water vapor to condense into tiny water droplets, creating the fog.
Examples of condensation include water droplets forming on the outside of a cold glass of water, fog forming on a cool morning, and clouds forming in the atmosphere when warm air rises and cools down.
Fog is a chemical weathering.
The process that changes water vapor into clouds of fog is called condensation. When warm, moist air comes into contact with cooler air or a cooler surface, the water vapor in the air condenses into tiny water droplets, forming fog.
Dry ice doesn't "turn into smoke". Dry ice causes moisture in the air to condense, forming fog. This is a purely physical, not chemical, change.
Fog is a cloud on the ground.
aerosols
Fog
when we take a bath the mirror has on it some gas, the steam on the sauna, and maybe fire
because is liquid to gas
Salt and chemical grains can act as cloud condensation nuclei, providing a surface for water vapor to condense on and form cloud droplets. These droplets can eventually coalesce and grow large enough to fall as rain. In fog formation, these particles can also help water vapor condense into tiny droplets, creating the fog.
The movement of fog inland and back out to sea is primarily driven by changes in temperature and wind patterns. When warm, moist air moves over cooler coastal waters, it cools and condenses, forming fog. Wind direction and speed can then push this fog inland or back out to sea, depending on atmospheric conditions. Additionally, differences in land and sea temperatures, especially during the day and night, can influence this movement.
Condensation forms when water vapor in the air cools and changes into liquid water. This typically occurs when warm, moist air comes into contact with cooler surfaces or when the air reaches its dew point temperature, where it can no longer hold all the moisture. Common examples include dew forming on grass in the morning and fog developing in cooler temperatures.