meteorology weather – short term variations in atmospheric conditions

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METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

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Page 1: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

METEOROLOGY

WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

Page 2: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

WHAT CAUSES WEATHER?

•The main cause of all weather is the imbalanced heating of the Earth’s surface.

•As the various areas of Earth are heated differently, the air interacts in various ways which we will study in this section.

Page 3: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

AIR MASS- LARGE VOLUME OF AIR THAT HAS

CHARACTERISTICS OF THE AREA OVER WHICH IT

FORMS.

• Types of Air Masses

A (Arctic)- Extremely cold and dry, forms over northern Canada.

cP (Continental Polar) dry and cold, forms over central Canada.

mP (Maritime Polar) Cold and wet, forms over northern Pacific and Atlantic oceans.

mT (Maritime Tropical) warm and wet, forms over southern Pacific and Atlantic Oceans.

cT (Continental Tropical) Warm and dry, forms over Mexico in the SUMMER ONLY.

Page 4: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

cP

mP

mTmT

cT

EXAMPLES OF AREAS THAT HAVE

SPECIFIC AIR MASSES

cP- Central Canada, North Dakota, SiberiamP- Maine, Northern Canadian Coast, Washington and AlaskamT- Florida, Rainforests, Northern Australian CoastcT- Texas, Mexico, Los Vegas, ArizonaA- Northern Siberia, Arctic Circle, Northern Canada and Alaska and Greenland

A

Page 5: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

The global winds discussed in our last are one of the forces that carry air masses across the globe

The Coriolis Effect causes global winds and ocean currents to curve. This is due to the Earth’s rotation.

**In the northern hemisphere, winds and currents rotate clockwise.**In the southern hemisphere, winds and currents rotate counter-clockwise.

How come an airplane you are travelling on never travels in a straight line?

Page 6: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

The other force that moves these air masses is the jet stream. It is a narrow band of wind that occurs in the stratosphere above large temperature contrasts.

Jet stream

Page 7: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

Fronts- The boundary at the front of an air massThe front created depends on the characteristics of the

air mass..

http://www.physicalgeography.net/fundamentals/7r.html

Cold Front – Cold air moves in, forcing warm air up. Intense precipitation and storms are common with cold fronts.Warm Front – Warm air moves in, displacing the cold air. The warm air rises gradually causing widespread light precip. Stationary Front – When 2 air masses meet but neither advances. They are usually similar in temperature. Causes cloudy weather with light winds and occasional precipitation.Occluded Front – When a cold front catches up to and takes over a warm front. Warm air is forced up violently. Typically causes strong winds and heavy precipitation.

Page 8: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

LOW/HIGH PRESSURE SYSTEMSRising air (makes clouds/precipitati

on)

Sinking air (no rising air means

no clouds)

Page 9: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

ISOTHERMS AND ISOBARSIsotherms – Lines on a weather map of equal temperature.

Isobars – Lines on a weather map of equal pressure.

Both can be useful in predicting and analyzing weather

Page 10: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

SUPERCELLS AND DOWNBURSTS

A supercell in Montana. Supercells are intense rotating storms in which updrafts can take 10-20 minutes to reach the top of the clouds.

Downbursts are violent downward drafts of wind with speeds over 100 mph. These winds can cause as much damage as tornadoes.

Page 11: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

Cumulonimbus Clouds- these are the dangerous thunderstorm clouds, they are also called thunderheads. These clouds usually form on a hot and humid day when the warm air rises quickly

Lightning- is a sudden spark or discharge released from energy within a cumulonimbus cloud. Lightning can be up to 30,000°C.

Thunder- is the sound of the explosion. Since light travels so much faster than sound, you always see the lightning first, than HEAR there explosion within seconds of the lightning.

Page 12: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

Tornadoes- is a rapidly whirling, funnel-shaped cloud that reaches from the cloud to the Earth’s surface.Tornadoes usually last less than 15 minutes but within that time, tornadoes can have winds speeds up to 320 miles per hour and be up to half a mile wide!

TV Warning vs Watch- Thunderstorm or tornado Warning means that there IS A STORM or funnel cloud and it is heading your way! Watch means that there is a very good chance that the thunderstorm and tornado COULD FORM.

Tornado Safety- safest places are a strong cement basement or bath tub with a mattress over your body. If in a car, get out! Get to a bridge overpass or lie in a ditch with your hands over your head away from any objects that could become projectile.

TORNADO FORMATION

Page 13: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

CAUSE FOR TORNADO ALLEY:1. CP AIR MASS FROM THE NORTH MIXES WITH THE MT FROM THE SOUTH. THE LARGE TEMPERATURE CONTRASTS CAUSE THE FORMATION OF SUPERCELLS (EXTREMELY POWERFUL THUNDERSTORMS). THE ROTATION BEGINS WITHIN THE THUNDERSTORM CLOUDS AND THE UPDRAFTS CREATE A COLUMN WHICH INCREASES ROTATION. THE AIR PRESSURE LOWERS IN THE CENTER CAUSES A VIOLENT INCREASE IN WIND SPEED.

The Fujita Scale Rates Tornadoes :

F0-F1 (last 1-10 minutes and winds up to 45-120 mph)

F2-F3 (last 20 minutes, winds up to120-220mph)

F4- F5 (Last up to 1 hour, winds are up to 220-340mph)

What is the most violent season for tornadoes?

Page 14: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

Location of Tornado Alley

Page 15: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

Hurricane Irene

Hurricane Katrina

HURRICANES:Hurricane Formation:

1. Warm air absorbs moisture from the ocean.

2. Water Vapor is lifted into the atmosphere.

3. As the water vapor rises, the cooler upper air condenses it into liquid droplets.

4. Condensation releases latent heat into the atmosphere, making the air less dense.

5. As the lighter air rises, moist air from the ocean takes its places creating a wind current.

6. Moving air begin the rotate due the Coriolis Effect (the process curving large wind and water systems due to the very fast rotation of the Earth)

7. Tropical Depression- Some thunderstorms and winds are 25-40 mph

8. Tropical Storm- thunderstorm wall becomes more solid, winds 42-78mph

9. Hurricane or Cyclone- distinguished eye with a surrounding eyewall (layers of thunderstorms that surrounds the eye) and winds are more than 78 mph.

HURRICANE FORMATION

Sandy Prezi

Page 16: METEOROLOGY WEATHER – SHORT TERM VARIATIONS IN ATMOSPHERIC CONDITIONS

STORM SURGEA wall of water

created as hurricane-force

winds force ocean water toward land.