Storms 4: Hail, Mamatus clouds, Atmospheric Rivers

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28 Terms

1
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mammatus clouds

form below anvil (underside)

2
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What effects do winds have?

1) cause damage directly

2) blows in more warm humid air (ex. storm fuel!)

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moisture advection

blow in warm humid air to feed storm

  • positive feedback

  • longer-lasting storms

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Force equation

F= m x a

  • force mass x acceleration

  • newtons second law

  • if you push on an object harder (bigger force), it will accelerate faster in the direction you push it

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Acceleration

  • the change in velocity during time

  • (V new - V old)/ time

  • SPEED & DIRECTION

  • ex. car increases speed 50 to 90 km in 15 seconds, it accelerates.

  • if car maintain 50km/h, acceleration = 0

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Air parcel

hypothetical blob of air about size of a city block

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Forecast Equation for the Wind

wind (horizontal or vertical)

V new = V old + [(f/m) x delta t]

  • tells us how wind will increase or decrease or change direction depending on forces that act on the air parcel

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What does buoyancy force cause in storms?

  • vertical movement

  • causes up & downdrafts

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What does Pressure-gradient force (PGF) in storms?

  • horizontal or vertical movement

  • hortizontal winds

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Warm air rises, cold air sinks cause what phenomena in storms?

updrafts and downdrafts

why?? temperature affects density affects buoyancy

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Buoyancy of air parcel depends on

Parcel temp vs Temp of surrounding air

<p>Parcel temp vs Temp of surrounding air</p>
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Buoyancy drives Thunderstorms

  • condensation in thunderstorms release latent heat

  • latent heat warms thunderstorm (latent—>sensible heat) , making it buoyant, causes air to rise

  • Drives violent updraft of thunderstorm

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Pressure equation

P = F / A

  • Pressure = force/area

Temperature alters Pressure to drive horizontal winds!!

14
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Pressure differences important because,,

pressure difference across a distance is called PRESSURE GRADIENT

  • these pressure gradients form in hurricanes

<p>pressure difference across a distance is called PRESSURE GRADIENT</p><ul><li><p>these pressure gradients form in hurricanes</p></li></ul>
15
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Where in a hurricane are there lots of thunderstorms?

in the core! condensation in the core makes the core even warmer

<p>in the core! condensation in the core makes the core even warmer</p>
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What happens as warm air expands in core?

warm air less dense than cool air—> takes up more space

pressure at top of core is > surrounding pressure

17
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Pressure gradient drives..

  • drives horizontal winds

  • creatures outward spiralling winds

  • winds remove molecules from the core

<ul><li><p>drives horizontal winds</p></li><li><p>creatures outward spiralling winds</p></li><li><p>winds remove molecules from the core</p></li></ul>
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How does the storm—> spiral inflow into bottom of hurricane?

  • low pressure at bottom of core creates pressure gradient that sucks in air

  • the inflow advects in more fuel

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Summary of pressure gradients driving horizontal winds

  • horizontal changes in temp—>

  • horizontal changes in pressure increase with height—>

  • pressure gradient increase at higher altitudes

  • drives faster winds @ higher altitude

-drives violent winds in hurricanes

-drives atmospheric rivers

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Hurricane anatomy

  • occluded front

  • cold front

  • warm front

  • know location of high and low pressure

<ul><li><p>occluded front</p></li><li><p>cold front</p></li><li><p>warm front</p></li><li><p>know location of high and low pressure</p></li></ul>
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atmospheric rivers

  • giant flowing streams of water vapor

  • weaker ones bring rainfall, extreme ones can cause flooding and mudslides

  • caused by pressure gradients

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Air molecules (continuity concept)

  • air molecules spread evenly

  • don’t leave gaps

  • don’t get bunched together

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Continuity causes circulations

1) buoyant parcel rises (hole where it used to be—> partial vaccum (lower pressure than surrounding air)

2) surrounding air molecules get sucked in to fill hole (maintain continuity)

3) above the rising parcel, molecules compressed ( higher pressure) expands laterally

initial VERTICAL MOTION due to buoyancy (generates)

HORIZONTAL MOTION in surrounding air

—> CIRCULATION

<p>1) buoyant parcel rises (hole where it used to be—&gt; <em>partial vaccum (lower pressure than surrounding air)</em></p><p>2) surrounding air molecules get sucked in to fill hole (maintain continuity)</p><p>3) above the rising parcel, molecules compressed ( higher pressure) expands laterally</p><p></p><p>initial VERTICAL MOTION due to buoyancy (generates)</p><p>HORIZONTAL MOTION in surrounding air </p><p>—&gt; CIRCULATION</p>
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vertical horizontal motions linked by effect of ..

continuity

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Hail Safety

1) wear safety glasses

2)if possible, turn away from storm and drive away

3) stay under a roof, inside a car, under farm tractor. to protect from falling hail

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Rain Hazards

Hazards:

  • downpours cause flash floods, reduced visibility while driving

Safety:

  • move to high ground, dont drive though water of unknown depth

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Hail Hazards

Occurence

can come from any large thunderstorm- most common with supercell Low precipitation

Hazards

  • injury, death, dent metal cars, break windows, flatten crops, kill livestock

Safety

  • get indoors

  • park under a roof

  • close eyes to keep shards out

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What is true about the eye of a hurricane?

1) It occupies more space because its warmer (particles more spread out)

2) High Pressure @ the top

3) Low Pressure @ the bottom