Clouds and precipitation

20
Clouds and Precipitation Earth Science Ms. Kurtzweil

Transcript of Clouds and precipitation

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Unit Objectives 1. Describe what happens when the

temperature of air drops to or below the dew point.

2. Identify the conditions that must exist for a cloud to form.

3. Name the main types of the clouds and the weather they predict.

4. Describe the various types of liquid and solid precipitation.

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Basics

Evaporation is the changing of water from a liquid to a gas Liquid water on Earth entering the

atmosphere as water vapor (when energy is added at the sunlight)

Condensation is the changing of water from gas to a liquid Water vapor in the atmosphere

condensing into liquid water droplets in a cloud (when energy is released = cooled)

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Water Cycle

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* When water reaches the dew point, or saturation point, it will begin to condense

into water droplets that form a cloud.

Four ways that air may cool enough below the dew point to begin condensation:

1. Contacting a colder surface (blade of grass, cold glass)

2. Radiating heat

3. Mixing with colder air

4. Expanding when it rises

“Expanding when it rises” is KEY to cloud formation!

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Before a true cloud can form, water vapor still needs something to condense upon!

Condensation nuclei: tiny particles on which water vapor condenses.

-The foundations of water droplets in a cloud

Examples of possible condensation nuclei in our atmosphere:

1. Salt

2. Dust

3. Ice

4. Smoke

5. Sulfate/nitrate particlesCloud Seeding during droughts

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How Do Clouds Form?

1. Water leaves the Earth’s surface.

2. Warm, moist air is less dense; it rises high up into the atmosphere.

3. At high altitudes, lower air pressure allows the air mass to expand and cool… eventually to the dew point.

4. Water condenses on condensation nuclei in the atmosphere, and…

Voila!!!

A cloud is born!

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“Fog is just a cloud near to the ground.” Is this true?

There are different types of fogs, radiation or advection, but overall, fog is formed nearer to the ground than a cloud. This occurs when moist air close to the ground cools to its dew point.

Fog can be considered a cloud at ground level. Like clouds, fog is made up of  condensed water droplets which are the result of the air being cooled to the  dewpoint, where it can no longer hold all of the water vapor it contains. For instance, rain can cool and moisten the air near the surface until fog forms.

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Radiation Fog Forms under similar conditions as dew On calm, clear nights, the ground will quickly

lose heat via radiation Cold air sinks and cools A whole layer of air is cooled below the dew

point and fog forms Common in humid valleys, near rivers or

lakes

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Cloud Types The shapes of clouds show how air is moving

through them. Rising? Horizontally? Stable?

main cloud types, based on their location in the sky

Cirrus “curly”• Highest family of clouds in the sky

Stratus “sheetlike” or “layered”• Mid-level clouds

Cumulus “piled” or “heaped”• Lowest clouds, closest to Earth’s surface

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Cloud Type DescriptionWhat kind of weather?

Picture

Cirrus High-level clouds.Thin, feathery, ice crystals

Just before snowfall or rainfall

Stratus Low sheets or layers

Little precipitation to heavy rains or snowfall

Cumulus Thick, puffy masses, “cotton balls”

Fair weather, maybe leading to abrupt storms

Nimbus Thick, grey masses

Rain, snow and thunderstorms

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Nimbus and Stratus are the clouds that bring rain, heavy rain or snow.

Thunderstorms are usually associated to the cumulonimbus .

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Precipitation

The falling of any form of water from the air to Earth’s surface

When will water leave a cloud and fall to the ground as precipitation? Basically, when gravity tells it to. Like

thick beads of condensation on a glass, when cloud droplets grow into drops heavy enough to fall to Earth, precipitation occurs.

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4 major types of precipitation

Hail Solid ppt in the form of

lumps of ice Begins as raindrops falling

from a cumulonimbus cloud

Convection currents toss the droplet high up into the cloud where it freezes. It then falls to a lower level and water condenses on it as a liquid. The tossing and freezing process repeats itself and the hailstone keeps adding layers and growing larger.

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Cloud Type DescriptionWhat kind of weather?

Picture

Cirrus High-level clouds.Thin, feathery, ice crystals

Stratus Little precipitation to heavy rains or snowfall

Thick, puffy masses, “cotton balls”

Fair weather, maybe leading to abrupt storms

Nimbus Thick, grey masses