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Humidity The amount of water vapor in the air Temperature affects how much moisture is in the air - warmer air can hold more water vapor, tending to make it more humid Relative humidity – the amount of water vapor in the air compared to what it can hold at a specific temperature When air cools, it can’t hold as much water vapor, so the water vapor condenses to liquid or forms ice crystals Dew point – the temperature at which air is saturated and condensation forms

9. Atmosphere 2

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Humidity• The amount of water vapor in the air• Temperature affects how much moisture is in the air

- warmer air can hold more water vapor, tending to make it more humid

• Relative humidity – the amount of water vapor in the air compared to what it can hold at a specific temperature

• When air cools, it can’t hold as much water vapor, so the water vapor condenses to liquid or forms ice crystals

• Dew point – the temperature at which air is saturated and condensation forms

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Clouds• Form when air rises, cools to its dew point, and

becomes saturated• Shape and height of clouds vary with temperature,

pressure, and water vapor in atmosphere

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Clouds• Shape

• Stratus-smooth, even sheets or layers at low altitudes• Cumulus-puffy, white clouds, often with flat bases• Cirrus-high, thin, white feathery clouds made of ice

crystals• Height

• Cirro – high clouds• Alto – middle-elevation clouds• Strato – low clouds• Nimbus clouds are dark and so full of water that sunlight

can’t penetrate them

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Clouds

• LOW CLOUDS – form at 2,000 m or less in altitude• Cumulus – puffy clouds formed when air

currents rise and carry moisture• Stratus – layered dull, gray sheets that can

cover the entire sky• Nimbostratus – low, dark, thick layers that

hide the Sun

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Cumulus

· Clouds formed at medium or

low elevation.

· Cumulus clouds are puffy

with flat bottoms.

· When cumulus clouds are

white they often signal fair

weather, but when they are

darker, they may signal rain

or thunderstorms.

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Stratus•Clouds formed at medium or low elevation; spread out layer upon layer covering a large area•As stratus clouds thicken, precipitation usually occurs over that area.

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Cumulus

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Stratus

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Clouds

• MIDDLE CLOUDS – form between 2,000 m and 8,000 m in altitude• Most are layered• Names have alto- prefix (altocumulus and

altostratus)• Can produce light precipitation

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Clouds

• HIGH AND VERTICAL CLOUDS • Cirrus – wispy, high-level clouds• Cirrostratus – high, layered clouds that can

cover the sky• Cumulonimbus – known as thunderstorm

clouds; produce heavy precipitation

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Cirrus•Clouds formed at high elevations; wispy clouds usually consisting of ice crystals that signal fair weather or may also signal an approaching warm front.

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Cirrus

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Cloud Cover Symbols• You will often see the circles drawn on a weather map

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Air Movement• Wind: Movement of air from one temperature or pressure

area to another• Different areas of Earth receive different amounts of the

Sun’s energy• Equator’s warm air, being less dense, is pushed

upward by denser, colder air• Poles’ cold air, being more dense, sinks and moves

along Earth’s surface• CORIOLIS EFFECT: spinning of the Earth

causes moving air to turn to the right in the northern hemisphere and to the left in the southern hemisphere

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Global Winds• Wind patterns, caused by convection currents combined with

the Coriolis effect, of Earth that affect the world’s weather• Near equator, very little wind and daily rain patterns called

the doldrums• Surface winds:

• Between equator and 30 degrees N and S latitude are steady trade winds

• Between 30 and 60 degrees N and S latitude, the westerlies blow in opposite direction from the trade winds.

• The polar easterlies blow from northeast to southwest near the north pole and from southeast to northwest near the south pole

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Global Winds

Equatorial doldrums

TRADEWINDS

TRADEWINDS

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The Weather Highways• The rotation of the

earth creates the Coriolis effect.

• The Coriolis effect causes the air and water to be deflected to the right (north of the equator).

• This creates global weather highways

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Fronts• Because air and moisture move in the

atmosphere, weather is constantly changing• Fronts are a boundary between two air masses of

different density, moisture, or temperature. • clouds, precipitation, and storms occur at

frontal boundaries• There are four different air masses

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The Air Masses• cP( continental polar) : cold, dry

stable• cT( continental tropical) : hot,

dry, stable air aloft, unstable at the surface

• mP( maritime polar) : cool, moist, unstable

• mT( maritime tropical) : warm, moist, unstable

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This map shows the air mass source regions and there paths

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Air Mass Map

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Cold Front

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Warm Front

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Occluded Front

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Stationary Front

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Anemometer- A tool used to measurewind speed in miles per hour.Wind vane· A tool used to measure wind direction.· Sometimes referred to as awind-weather vane or a wind sock.· Wind direction is described by the direction from which the wind is blowing.Thermometer - A tool used to measure air temperature in degrees Fahrenheit or Celsius.

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Sling Psychrometer- •A two-thermometer instrument also referred to as a wet-dry bulb used to measure relative humidity (the amount of water vapor in the air).• Temperatures readings are converted using a relative humidity table.

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Barometer- A tool used to measure air pressure in inches of mercury or millibars (mb).

Rain gauge- A tool used for measuring the amount of precipitation in inches or centimeters.

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MENU

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Reading a weather map• ISOBAR= connects areas of equal

pressure BAR comes from BARometric pressure

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Reading a weather map...• Isotherm: Connects areas of equal

temperature; therm means temperature

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Satellites· Satellite images are used for seeing cloud patterns and movements.· For example, hurricane clouds and movement can be observed using satellite images.Radar· Radar images can be used to detect cloud cover, rainfall or storm location, intensity, and movement, as well as the potential for severe weather (for example, hurricanes or tornadoes).

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Severe Weather

• Thunderstorms occur inside warm, moist air masses and at fronts• Warm, moist air is forced rapidly

upward, where it cools and condenses

• Strong updrafts of warm air and sinking, rain-cooled air cause strong winds

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Lightning• Movement of air inside a storm

cloud causes parts of the cloud to become oppositely charged

• Current flows between the regions of opposite electrical charge, forming a lightning bolt

• Thunder – lightning superheats the air, causing it to expand rapidly and then contract, forming sound waves

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Tornado• Violent, whirling wind that moves in

a narrow path over land

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Hurricane• Large, swirling, low-pressure system

that forms over tropical oceans• Heat energy from moist air is

converted to wind that can reach speeds of 250 km/h

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Blizzard• A winter storm with strong winds, cold

temperatures, and low visibility, that lasts more

than three hours

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Severe Weather Safety• A National Weather Service WATCH

means conditions are favorable for severe weather to develop

• A warning means that severe weather conditions already exist

• Meteorologists study and predict weather

• National Weather Service makes weather maps and issues watches and warnings

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Let’s break for a short review1.Transfer of heat in liquids or

gases:_____2. _____ air is dense and tends to sink.

4. Cold air holds _____ moisture than warm air

5. The Coriolis effect causes the air and water to be deflected to the _____ (south of the equator)