Storms 4 Flashcards
Where are mammatus clouds
underside of thunderstorm anvil
What are winds
air motions
or air-parcel movement
Moisture Advection
wind blowing in warm, humid air (storm fuel)
Storms can become organized due to
moisture advection
-> positive feedback
-> longer-lasting storms
Radiative heat from the sun causes (what does sensible and latent heat do)
sensible: air gets warmer
latent: humidity rises
What creates winds
forces
acceleration formula
(Vnew - Vold) ÷ ∆t
Prognostic equation / “forecast method” for wind
Vnew = Vold + [ (F/m) x ∆ t ]
Air parcel is
hypothetical blob of air
- size of city block
Buoyancy force
vertical
causes up and downdrafts
Pressure-gradient force (PGF)
horizontal OR vertical
drives horizontal winds
How does temperature alter buoyancy to drive vertical winds?
Temp -> density -> buoyancy
warm air rises (updraft)
cold air sinks (downdraft)
Buoyancy of an air parcel depends on the DIFFERENCE btwn ___ & ___
parcel temp and surrounding air temp
What is the driving force of storms?
Buoyancy
What processes drives the violent updrafts in Tstorms?
- Condensation in storms release latent heat
- latent heat warms the air, making it buoyant / rise
Pressure equation and units
Force / Area
N / m^2
True or false: pressure drives winds
true
Pressure gradient is
pressure DIFFERENCE across a distance
(air moves to lower pressure region)
force uses ∆ p, the diff btwn opposing pressures
What is in the core of a hurricane? How does this make the core warmer?
lots of thunderstorms
-> condensation in these storms makes the core warmer
Summary of how pressure gradients drive horizontal winds
Review slides for explanation
Horizontal changes in temp
-> Horizontal changes in pressure (High pressure at top, Low at bottom)
-> pressure gradient increases at higher altitudes
-> drives faster winds at higher heights
What type of force drives the violent winds in hurricanes? (and also atmospheric rivers)
Pressure-gradient force
What are atmospheric rivers and how do they pose a danger?
flowing streams of water vapour
-> when air hits mountains, it is forced to rise
-> air cools at adiabatic lapse rate (10C/km)
-> causes water vapour to condense = rain + flooding
Continuity concept
(Assuming at the same temperature)
Air molecules tend to spread smoothly and evenly
- no gaps, don’t get bunched together
What does continuity cause?
circulations