Week 8 Flashcards
Thunderstorms
- 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
Lifecycle of a Thunderstorm
Towering Cumulus Stage
Mature Stage
Dissipating Stage
Towering Cumulus Stage
A lifting mechanism forces warm air up to produce a ~6km-high cumulus cloud
Mature Stage
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
Dissipating Stage
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
Three main types of thunderstorms
Multi Cell Storms
Squall Line Storms
Supercell Storms
Multi Cell Storms
The combination of many smaller thunderstorm cells to produce a larger, violent storm that can last for hours
Squall Line Storms
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
Supercell Storms
Gigantic, long-lasting single cells responsible for most of the tornadoes and most damaging weather in North America each year
Hurricanes
- 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’
Hurricane Hazards
- Heavy rain, damaging winds, and strong waves
- Storm Surge is the result of strong waves moving in-land, damaging cars, trees, and infrastructure
Hurricane Formation
- 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
Production of Cyclones
- 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
Two velocities of a hurricane
- Hurricane-Wind Velocity
- Storm-Centre Velocity
Hurricane-Wind Velocity
The speed of the wind inside the storm, travelling counterclockwise around the eye; Range: 119 – 252+ km/h