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Water cycle and cloud formation
Chapter 14.1 and 14.2 of Earth and Space Science (McGraw Hill)
The condition of the atmosphere at a specific time and place
The study of weather
The continuous process by which water moves from Earth's surface to the atmosphere and back.
The process by which water changes from liquid form to an atmospheric gas.
The process by which a gas changes into a liquid, usually due to a cooling of the gas. When this happens in the atmosphere clouds are formed.
Any form of water that falls from clouds and reaches Earth's surface (rain, snow, sleet, and hail).
The amount of water vapor in the air
The comparison of the actual amount of water vapor to the amount of water vapor that would be in the air if it saturated.
In weather, this refers to the maximum amount of water vapor the air can contain.
The temperature at which condensation begins
A collection of small water droplets or ice crystals suspended in the air, which forms when the air is cooled and condensation occurs.
Clouds that look like a fluff of cotton, these form close to the ground, and are associated with good weather.
Dark gray sheets, these clouds form close to the ground often blocking out the sun. Sometimes they bringing light rain or snow showers (then they are referred to as nimbostratus).
High-altitude clouds that are thin, feathery tufts of ice crystals.
Clouds associated with rain or snow (include several cloud types such as nimbostratus, or cumulonimbus).
Loss of water vapor from the leaves of a plant.