Week 8 Flashcards

1
Q

Thunderstorms

A
  • Smallest cyclonic storm
  • Form when there is moisture and instability in the atmosphere, driven by some lifting mechanism
  • In Ontario, most of the atmospheric moisture comes from the Great Lakes
  • Most atmospheric instability occurs at or near the boundaries of warm and cold air masses
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2
Q

Lifecycle of a Thunderstorm

A

Towering Cumulus Stage
Mature Stage
Dissipating Stage

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3
Q

Towering Cumulus Stage

A

A lifting mechanism forces warm air up to produce a ~6km-high cumulus cloud

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4
Q

Mature Stage

A

The produced cloud can suddenly grow in size, up to 18km-high; air movement is tumultuous, with strong updrafts holding back large amounts of rain and hail

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5
Q

Dissipating Stage

A

As the moisture in the cloud is dropped, the storm enters the Dissipating Stage, where upward moisture supply has been removed and the storm will weaken

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6
Q

Three main types of thunderstorms

A

Multi Cell Storms
Squall Line Storms
Supercell Storms

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7
Q

Multi Cell Storms

A

The combination of many smaller thunderstorm cells to produce a larger, violent storm that can last for hours

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8
Q

Squall Line Storms

A

As a weather front moves forward, it can produce a line of storms 100+ km long; sudden rain produces a ‘gust front’, lifting more moisture to feed the storm

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9
Q

Supercell Storms

A

Gigantic, long-lasting single cells responsible for most of the tornadoes and most damaging weather in North America each year

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10
Q

Hurricanes

A
  • A hurricane is a type of Tropical Cyclone
  • A severe cyclonic tropical storm in the North Atlantic Basin
  • Originates from the tropical trade winds, between 5°N - 20°N
  • Rotates counterclockwise, with a central ‘eye’ attaining minimum wind speeds of 119km/h
  • In the Central Pacific, tropical cyclones are called ‘typhoon’
  • In the South Indian Ocean, tropical cyclones are called ‘cyclone’
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11
Q

Hurricane Hazards

A
  • Heavy rain, damaging winds, and strong waves
  • Storm Surge is the result of strong waves moving in-land, damaging cars, trees, and infrastructure
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12
Q

Hurricane Formation

A
  • These storms begin with a disturbance in westward winds over the warm ocean 26°C
  • As the water vapour rises, it condenses in the troposphere releasing a large amount of latent heat energy
  • With strength, the storm is given the names, ‘tropical wave’ or ‘tropical storm’, with ‘hurricane’ being the strongest
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13
Q

Production of Cyclones

A
  • A mature hurricane has spiraling bands of high wind and torrential rain surrounding the eye
  • These bands of rain are known as Rainbands and rotate counterclockwise, while the overlying Cirrus Overcast rotates clockwise
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14
Q

Two velocities of a hurricane

A
  • Hurricane-Wind Velocity
  • Storm-Centre Velocity
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15
Q

Hurricane-Wind Velocity

A

The speed of the wind inside the storm, travelling counterclockwise around the eye; Range: 119 – 252+ km/h

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16
Q

Storm Center Velocity

A

The travel speed of the entire storm across the Earth, being pushed by outside regional winds; Range: 8 – 100 km/h

17
Q

Hurricane Andrew (1992)

A
  • Hurricane Andrew made landfall south of Miami, producing destructive storm surge and sustained winds
  • 4/5 on Scale
  • 50 deaths, US$25 billion Damages
18
Q

Hurricane Andrew Importance

A
  • Forced scientists to rethink how Cyclonic storms worked
  • Andrew did not produce the strongest winds around the eye like other hurricanes, leading to the postulation of Spin-Up Vortices
  • These are small, intense vortices of wind developed within the winds of a storm, and produce the highest wind speeds of a hurricane
  • The presence of vortices would explain the seemingly selective damage noticed in Homestead following the disaster
19
Q

Hurricane Katrina (2005)

A
  • The 6th strongest hurricane ever recorded
  • 1,604 people, the storm caused the greatest damage ever, estimated at ~US$75 billion
    -Picked up immense strength in the warm Gulf of Mexico, intensifying from a Category 3 to Category 5 (max of scale!) overnight
  • Huge storm surges were resultant along the Mississippi-Louisiana coast, with measured winds reaching 280km/h
  • Upon making landfall in Louisiana, the storm was measured as 190km wide, with 120-205km/h winds
20
Q

Predicting Storms

A
  • There are no easily-measurable metrics to determine whether a storm will develop or not – there is usually great uncertainty over the potential of a cyclone to develop into a cyclonic storm
  • The National Hurricane Center tracks tropical storms forming and/or occurring near the US coast
21
Q

Project Stormfury

A
  • An ambitious US endeavor, Project Stormfury aimed to weaken storms before they make landfall to mitigate the damage incurred
  • The idea was that if a airplane flew over a hurricane, it would be able to “seed” the storm with either silver iodide or dry ice
  • The goal of adding these seeds was to both increase the freezing temperature of water and to produce ice crystals within the storm
  • The idea of growing ice crystals was leaning on the hope that this change in state would release some of the stored latent heat energy driving the storm
  • Even a reduction of ~10% the storm’s intensity would be a huge achievement
  • After trying to seed 4 hurricanes, the project was abandoned due to lack of perceivable evidence