Thunderstorms Flashcards
What are the requirements for the development of a thunderstorm?
- Lifting/Trigger action
- Conditionally unstable atmosphere through a deep layer
- CB cloud
- High moisture content
How do thermal thunderstorms form?
What is it related to?
When are they likely to occur?
- Where warm convective patterns warm the air forcing it rise.
- Usually diurnal and land-related, must be close to a water source for CB developments.
- In temperature latitudes, favours coastal regions during summer and usually early to mid-afternoon.
- In tropical latitudes, it can be a daily occurrence throughout the year, starting early afternoon until well after sunset.
How do convergence thunderstorms form?
Where they most likely to occur?
- Occurs when there are convergence patterns near the surface.
- Thermal/heat thunderstorm can fall in same category as convergence thunderstorm e.g. during a summer day when there is strong sea breeze activity, unstable conditions force moisture aloft.
- When the region is at the ITCZ, convergence thunderstorms are most common.
How do orographic thunderstorms form?
Does the time of day or season have an influence on when they form?
How long can they last?
- Where terrain gives moist unstable air sufficient lift for cloud formation to occur.
- Time of day or season has no influence.
- Can last for days.
- With high moisture content in an orthographic cloud, precipitation can be severe.
- Not unusual for mountains and adjacent plains to experience heavy hail.
How do nocturnal tropical thunderstorms form?
When do they form?
- Where oceanic areas are within 10º latitude of either side of the equator see pre-existing cumulus clouds becoming increasingly unstable at night due to temperature difference between air over the warm oceans and upper atmosphere.
- Sea temperatures are warm throughout the year.
- This type is most active towards DAWN when ELR has reached its steepest value.
- After daybreak, thunderstorms persist for some time but will cease to exist around mid-morning.
How do cold advection thunderstorms form?
Where are they likely to be found?
How intense are these thunderstorms?
- When a volume of cold air passes rapidly over a warm ocean area, it absorbs large amounts of water from the sea surface, while at the same time, its lower levels warm quickly.
- As ELR steepens and vertical mixing intensifies, it is perfect for the development of CB cloud.
- Can be experienced in Australia and NZ (during spring and early summer for NZ).
- Not severe.
How are frontal thunderstorms formed?
and what does it indicate?
How long is this severe feature?
Occurs when warm unstable air is lifted aloft the boundary between two air masses. Cloud base is lower than most air mass thunderstorms, and the number of CB clouds is greater.
What is the cross-sectional width of a frontal thunderstorm?
This thunderstorm is short-lived and its cross-sectional width is not more than 80 to 120 km.
What is the most severe feature of a frontal thunderstorm?
This thunderstorm is more severe, numerous and faster moving than other storms. Most severe of these are SQUALL LINES which often advance in front of the front.
How is a squall line formed?
Squall lines are created when the frontal uplift creates large numbers of linked storms along a sustained linear boundary.
What does squall lines indicate?
Squall lines indicate the severity of the front and is marked by a sudden wind change and very gusty conditions.
How long is a squall line and how long can it last for?
Squall lines can be several hundreds of kilometres long and can last for days.
Where is turbulence likely to be encountered with regards to flight in and around a thunderstorm?
The middle level of the storm.
Is turbulence the most serious aspect of flight in a thunderstorm?
Yes.
With regards to updraughts and downdraughts in turbulence, where are these most found common?
- Updraught = development stage
- Downdraught = decaying stage
