Sem#2 Chap 2 Flashcards
(85 cards)
Thunderstorms
Towering clouds that produce lightning and thunder. May rise to the troppause
Typically <30 km diameter, with speed ~90 km/hr
Most occur over land within the tropics.
Severe thunderstorms (defined by the NWS) may produce:
- Winds >93 km/hr
- Hail >2.5 cm in diameter
- A tornado
Thunderstorm Development, Temperate climates:
- Thunderstorms are frequent during warm seasons.
Thunderstorms are rare in :
- Within high latitudes
- Over subtropical deserts
- Over oceans
Thunderstorm days:
- Days on which at least 1 thunderstorm occurs.
3 conditions must be present for thunderstorm:
- Moist air (mostly from oceans, lakes, and wetlands)
- A lifting mechanism
- Atmospheric instability
5 Lifting Mechanisms Force Air to Rise
Movement along a front:
Gust fronts:
Less distinct boundaries:
High relief (orographic lift):
Convergence:
Movement along a front:
- Advancing cold air forceswarm, moist air up.
Gust fronts:
- Thunderstorms create cold downdrafts.
- Downdrafts act like small cold fronts
Less distinct boundaries:
- Warm areas may contain less dense, buoyant air.
- Cool air may move beneath warm air
High relief (orographic lift):
- Mountains force air upslope.
Convergence:
- Colliding air flows may create lift.
Air May Rise Without Being _________.
Physically Lifted
Air above ground becomes buoyant enough to rise. Which is common during…..
Common during the summer on plains and mountain slopes
Unstable air:
- When an air parcel is less dense than its environment
Adiabatic expansion:
- Air parcel expands as it rises.
- Air in a rising, expanding parcel will cool.
Environmental lapse rate:
The rate temperature drops with increasing altitude.
* Typical rate is 4°–9°C/km
Unsaturated air parcels:
- Do not form clouds as they rise and cool
Saturated air parcels:
- Form clouds as they rise and cool
Dry adiabatic lapse rate (DAR):
- Applies to unsaturated air parcels
- Cool at ~10°C/km
- Relative humidity increases as air parcel rises and cools.
If DAR > than environmental lapse rate:
- Air parcel will cool, become stable, and stop rising.
Moist adiabatic lapse rate (MAR):
- Applies to saturated air parcels
- Cool at ~6°C/km
- Slower rate is due to latent heat released during condensation.
Conditional instability:
- An air parcel’s MAR < than the environmental lapse rate
- Air parcel remains warmer than environment.
- Air parcel remains buoyant and continues rising
Thunderstorm development depends on 2 variables:
- The environmental lapse rate
- An air parcel’s moisture content