Condensation, Evaporation, Weather, and the Water Cycle

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Last name: First name: Date: Period: COM INC COM* Condensation, Evaporation, Weather, and the Water Cycle Evaporation and boiling are both types of vaporization, in which a liquid changes into a gas. The molecules are moving fast enough to overcome their attractions and spread out. 1. What is the difference between evaporation and boiling? Describe what happens in the ocean vs a pot of water on the stove as part of your explanation. 2. When water evaporates, do the water molecules themselves break apart or do whole water molecules separate from one another? Describe how water changes as it goes from its liquid form to its gas form. Condensation happens when water molecules in the air slow down so much that their attractions become greater than their speed. This makes them move closer together, forming liquid water. 1. List THREE common examples of condensation. a. b. c. 2. When you breathe out in the winter, you see smoke, which is really tiny droplets of liquid water. Using what you know about condensation, explain why you think this happens. (Hint: There is water vapor in your breath.) Weather: For each weather phenomenon below, write 1 sentence to explain how it works. Think about what phase changes are involved and at what temperatures it occurs. Weather phenomenon Clouds How it works Rain

Snow Hail Dew Frost Fog Mist on a pond Mastery question preview: Describe how water changes states during the water cycle. Discuss the processes involved. What happens in each? (in terms of energy and motion/spacing of the molecules BE SPECIFIC, don t just name the process)

Clouds Clouds form when liquid water evaporates to become water vapor and moves up into the sky in upward-moving air. Air at higher altitudes is usually cooler than air near the ground. So as the water vapor rises, it cools and condenses, forming tiny drops of water. These droplets are suspended in the air as clouds. Clouds at higher altitudes where the air is even colder also contain ice crystals. Clouds at very high levels are composed mostly of ice crystals.

Rain Rain begins as tiny droplets of water suspended in the air as clouds. These droplets are so small that they don t fall yet to the ground as rain. They are similar to the tiny droplets in fog or mist. But when these droplets collect and join together, they become bigger and heavier drops. Eventually these drops become so heavy that they fall to the ground as rain.

Snow Like rain, snow begins with condensing water vapor that forms clouds. However, when it s cold enough, water vapor not only condenses but also freezes, forming tiny ice crystals. More and more water vapor condenses and freezes on these seed crystals, forming the beautiful ice crystals with six-sided symmetry that we know as snowflakes.

Hail Hail forms when a small drop of water freezes, falls, and then gets pushed back up into a cloud. More water droplets collect and freeze on this ice crystal, which makes it heavier, and it begins to fall again. The violent air in a thundercloud (cumulonimbus cloud) repeatedly bounces the ice crystal upward. Each time it gets another coating of freezing water. Finally, the ice crystal is so heavy that it falls all the way down to the ground as hail.

Dew Dew is produced when moist air close to the ground cools enough to condense and forms liquid water. Dew is different than rain because dew doesn t fall onto the ground in drops. It slowly accumulates to form drops on objects near the ground. Dew often forms on blades of grass and leaves and can make beautiful designs on spider webs.

Frost If the temperature of surfaces on the ground is low enough, water vapor in the air can change directly to the solid frost without first condensing to a liquid.

Fog Usually the air near the ground is warmer than the air above it, but the conditions that cause fog are just the reverse. Fog forms when warm, moist air passes over cold ground or snow. As the water vapor in the air cools, it condenses, forming very tiny drops of water suspended in the air. Fog is very much like a cloud, but closer to the ground.

Mist on a Pond Water evaporates even when the air is cold. To form mist, the water in a pond, pool, or hot tub must be warmer than the air above it and the air must be cold enough to cause the water vapor to condense as it rises. The mist seems to disappear as the water droplets evaporate to become water vapor again.