Natural Disasters Week 8
For thunderstorms, the lifted air has to become less dense than the air around it to keep is rising
It has to stay warmer than the surrounding air or it will stop rising and stary sinking again
IF a Rising Air Parcel is Unsaturated
It Cools More Quickly than the Surrounding Air
Reaches the same Temperature/Density as Surrounding air
Then it stops rising.
IF an Air Parcels is Saturated
Water Vapor Condenses as it Rises
The Parcel Cools Slower than an Unsaturated Air Parcel
Then IF
The rising saturated air parcel Cools Faster than surrounding Ai
Water Condenses Into Clouds but no Thunderstorms
(System Stabilizes)
OR
Rising saturated air parcel Stays Warmer than surrounding Air
It keeps rising and Thunderstorms Can Occur!
LIMBS
LIFT - do I have less dense air that can rise over dense air?
INSTABILITY - Do I have colder/denser air aloft, so that my rising less dense air keeps rising?
MOISTURE - Relatively high humidity
BOUNDARIES - Do I have clear boundaries between two distinct air masses that don’t mix well (cold fronts)
SHEAR - Do I have strong winds flowing in different directions, especially lower and upper winds?
Types of thunderstorms
Single cell - convection cells or orographic lifting, fairly shortly lived
Multicell - strung along a distinct line formed by cold fronts (most rain in Midwest
Supercell - contains partially strong rotating updraft, 30 miles wide
vertical wind shear - condition where adjacent air mass winds differ in speed
Lightning
Electrons from atoms flow into our body making the skin negatively charged relative to the object you touch
Particles move around in the clouds making them larger
Electrostatic potential frows until it drives electrons across the air
PROFESSOR GOING TO SACREMENTO
Derechos
Widespread long windstorms
Product of concentrated strong winds by downdraft
Happens when conditions pf down burst keeps happening in the same spot
Hurricanes
Deadliest storms on earth
Most costly natural hazard in the U.S.
Large tropical storm spiraling around
The eye is a cloud free circular area
The eye wall is a dense upward flowing rapidly spiraling
Spiral rainbands arc shaped cloud banks of tall, aligned thunderstorms
Intensity can increase and decrease
Storm lines bulge or shrink
Eye walls contract and regenerate