The warm air mass
Wiki User
∙ 8y agoWiki User
∙ 16y agowarm air
Yes it dose. Its just not very dense. If you boil water and can some how capture the steam the weight it the total weight of the steam and water that is left will have the same weight as the water you started with. (Mass can not be created or Destroyed)
Yes they do as all mattars has mass and occupies space.It has definite mass,occupies space,does not have a definite shape and no definte volume.Why?Becase it has already evaporated and changed from water state toa gaseous state.Hope this is useful!!
Evaporation.
Add water (vapor) ... evaporation. Lower the temperature of the air mass.
The amount of water vapor present in the air determines if the air mass is dry or humid. Humid air masses have high water vapor content, while dry air masses have low water vapor content. This water vapor content is influenced by factors such as temperature, proximity to bodies of water, and weather conditions.
A warm air mass can hold more water vapor than a cold air mass. This is because warm air has a higher capacity to hold moisture due to its higher temperature. When warm air cools down, it reaches its dew point and can no longer hold all the water vapor, leading to condensation and possibly precipitation.
Yes, water vapor does have mass. Water vapor is a gas composed of water molecules, and like all matter, it has mass. However, the mass of water vapor is much lighter compared to liquid water.
It is saturated.
Cooler. The cloud forms because the water vapor condenses by cooling down. Thunderstorms occur because a warm, moist air mass is cooled by an incoming cold air mass. When the moist air gets chilled, the water vapor condenses to form clouds, resulting in rain.
The actual amount of water vapor in a mixture of air and water is called absolute humidity. It represents the mass of water vapor divided by the total mass of the mixture, including both the water vapor and dry air.
The mass of water vapor in air is typically expressed in terms of relative humidity, which is the ratio of the actual water vapor pressure in the air to the saturation vapor pressure at a given temperature. It varies depending on temperature and pressure. A psychrometric chart can be used to determine the mass of water vapor in a given volume of air based on these factors.
The air mass with the highest actual water vapor content is the maritime tropical air mass, which originates over warm ocean waters. This air mass contains a significant amount of water vapor due to the high level of evaporation from the ocean surface.
becomes the mass of clouds.....
Water vapors makes up only a few percent of the mass of the atmosphere. However, this small amount of water vapor has in oceans and water bodies changes to a gas, water vapor. The mount of water vapor in the air is called humidity
When water evaporates, the water molecules gain enough energy to break free from the liquid and become water vapor. While the volume of the water vapor increases due to the increased space between the molecules, the total mass remains the same as when it was in liquid form.
The process that changes water vapor into liquid is called condensation. This creates rain when a moist air mass is elevated and/or cooled. It also happens on objects that are a colder temperature then the surrounding air (e.g. cold beverage containers, dew on grass).
When water evaporates, the water molecules gain energy from the surroundings to overcome intermolecular forces and escape into the air as vapor. While the water loses mass during evaporation, this mass is not lost but rather converted into the potential energy of the water vapor. Therefore, the total mass and energy of the system (water and surroundings) remains constant, demonstrating conservation of mass and energy.