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Thunderstorms

Thunderstorms

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Thunderstorms. Straight Line Winds. This is the sort of wind that comes out of a thunderstorm. They are produced by the downward momentum within the downdraft region of a thunderstorm. - PowerPoint PPT Presentation

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Page 1: Thunderstorms

Thunderstorms

Page 2: Thunderstorms

Straight Line WindsThis is the sort of wind that comes out of a thunderstorm. They are produced by the downward momentum within the downdraft region of a thunderstorm.

If the air is dry in the middle of the troposphere, the storm has a fast rate of forward movement, and there are strong updrafts and downdrafts, you have the right conditions for strong Straight Line Winds

Page 3: Thunderstorms

Dewpoint Depression

• Difference between temperature and dewpoint at the surface and aloft

Page 4: Thunderstorms

Dewpoint Depression

• This has the following practical results:– When the lower level Tdd (temp – dew point) is small

and air is being lifted, clouds form low bases

– When the lower level Tdd is large and air is being lifted, clouds form bases higher

– IOW, it took more lifting to saturate that air adiabatically

– Can enhance downdrafting and hail formation by enhancing evaporative cooling

Page 5: Thunderstorms

Dewpoint Depression

• Suppose T = 15C and the dew point is 9C. What is TDD?

• 15C-9C = 6.

• It does not equal 6C, it is not a temperature, it’s a difference between temperatures.

Page 6: Thunderstorms

Types of Thunderstorms

1) Air Mass Thunderstorms• Most Common• Least destructive• Contained within a single air mass

Page 7: Thunderstorms

Stages of an air mass thunderstorm1) Cumulus Stage

• Air begins to rise• Rising air cools adiabatically and forms fair weather

cumulus clouds• These initial clouds last for minutes• The initial clouds evaporate and increase the amount of

moisture in the air• New clouds with vertical development form• The new clouds extend to the upper troposphere and

ice crystals grow by the Bergeron process• The thick clouds cause the sky to darken

Page 8: Thunderstorms

Stages of an air mass thunderstorm1) Cumulus Stage

• Air begins to rise• Rising air cools adiabatically and forms fair weather

cumulus clouds• These initial clouds last for minutes• The initial clouds evaporate and increase the amount of

moisture in the air• New clouds with vertical development form• The new clouds extend to the upper troposphere and

ice crystals grow by the Bergeron process• The thick clouds cause the sky to darken

Page 9: Thunderstorms

Stages of an air mass thunderstorm

2) Mature Stage• The storm is at its most intense• Overshooting tops form• Lightening and Thunder may be present• Warm Updraft• Cold downdraft• Strong winds at surface via downdraft

Page 10: Thunderstorms

Stages of an air mass thunderstorm

3) Dissipative Stage• Falling rain or graupel forces air downward

causing down drafts• As precipitation proceeds, downdrafts

increase at the base of the cloud.• This cuts off the water supply• Precipitation diminishes and the sky clears

Page 11: Thunderstorms
Page 12: Thunderstorms

Well Developed Cumulus Cloud

Page 13: Thunderstorms

Severe Thunderstorms• Most form along or ahead of cold fronts in Mid-

latitude cyclones• Wind speeds exceed 93 km/hr (60mile/hr)• Have hailstones larger then 2 cm in diameter• Spawn tornadoes• Last for 12 hours to several days• Account for ~60% of all annual rainfall in the

US and Canada• Typical occur in groups of individual storm cells

Page 14: Thunderstorms

Severe Thunderstorms

• Mesoscale Convective Systems (MCS)– Mesoscale Convective Clusters (MCC)– Squall Line

• Supercell

Page 15: Thunderstorms

Severe Thunderstorm Structure

http://www.theweatherprediction.com/severe/structure/

Page 16: Thunderstorms

MCCs

• Occur as circular or oval clusters of storm• But all storms are part of the same system• Defined by satellite images• Responsible for most severe weather in

the US and Canada

Page 17: Thunderstorms

Satellite Imageof

Mesoscale Convective Complex

Page 18: Thunderstorms

Squall Lines• Consist of a large number of individual storm

cells arranged in a linear band, ~500 km in length

• Tend to form 300 to 500 km ahead of cold fronts• Form mainly in spring and summer• Last 10 hours to days

Page 19: Thunderstorms

Squall-lineThunderstorms

Page 20: Thunderstorms

Classic – Great Plains

High Precipitation – Eastern Great Plains and Eastward

Low Precipitation - leeward side of the Rockies

Three types of Super Cells

Page 21: Thunderstorms

Supercell Thunderstorm

Page 22: Thunderstorms

Cluster of Supercell Thunderstorms

Page 23: Thunderstorms

Supercell Storms• Very violent• Smaller in extent than MCCs or Squall lines (20-

50km in diameter)• Consist of a single, extremely powerful cell

instead of a number of cells• Undergo large scale rotation• Complex updrafts and downdrafts

How do we study storms?

Page 24: Thunderstorms

Studying Storms• Doppler Radar - makes use of the Doppler effect

to image storms, study their patterns, make predictions and issue watches and warnings.

• Doppler Effect – Sound travels in waves– If the object making the sound is traveling toward the listener, the sound waves

become compressed (shift toward shorter wavelengths). This results in a higher pitch.

– If the object making the sound is moving away from the listener, the sound waves are stretched (shift toward longer wavelengths) and the pitch is lower,

Page 25: Thunderstorms

Studying Storms• Doppler Radar takes advantage of the Doppler

Effect.

• A transmitter/receiver is used to emit a pulse of electromagnetic radiation ( = several centimeters)

• Can be used to observe the motion of cloud constituents (raindrops and ice).

• Wind speed, direction and cloud structure can be determined.

Page 26: Thunderstorms
Page 27: Thunderstorms
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Studying Storms

Doppler Radar

• Hook - appearance of the hook usually indicates a tornado will form.

• Vault - inflow of warm surface air enters the cell. Vault results from small newly formed cloud drops that are too small to be visible on radar.

Page 29: Thunderstorms

Hook Echo

http://www.crh.noaa.gov/dtx/images/010521ref_expl.jpg

Page 30: Thunderstorms

The mountain of Gold-Shwedagon Pagoda

Page 31: Thunderstorms

Pagoda

http://www.mir.com.my/leofoo/Burma2005/images/lake_kandagwi.jpg

Page 32: Thunderstorms

Pagoda

http://www.mir.com.my/leofoo/Burma2005/images/lake_kandagwi.jpg

Page 33: Thunderstorms

pagoda

http://www.risc.uni-linz.ac.at/people/sgerhold/images/myanmar/shwedagon.jpg

Page 34: Thunderstorms

Bogalay Village

http://ratchasima.files.wordpress.com

Page 35: Thunderstorms

Bogalay Village

http://ratchasima.files.wordpress.com

Page 36: Thunderstorms

Cyclone Nargis, May 2 2008

Page 37: Thunderstorms

Cyclone Nargis, May 2 2008Hits the Irrawady delta+22K known dead~41K missing10,000 dead in Bogalay24 million people live in the disaster zoneInaccessible with the damage to infrastructureMilitary Junta had always justified its control as being needed to respond to disasters and emergencies.Military response to the cyclone has been much slower and weaker than to the monk protests (the saffron revolution)Reports as of a few years ago of diseases like Japanese Encephalistis in the villages of the deltaSome US ambasadors reporting possiblity of the death toll being 100K