Weather Weather
SCOTT HANDEL
National Oceanic and Atmospheric Administration
Photo: Courtesy AP
Outline Outline
• Clouds
• Thunderstorms
• Hail/Lightning
• Tornadoes
• Hurricanes
CLOUDS
CLOUDS
Cirrus Clouds
Cirrus Clouds
Stratus
Stratus Nimbostratus Nimbostratus
Cumulus
Cumulus
Cumulonimbus Cloud
Cumulonimbus Cloud
Cloud Formation
Thunderstorm Formation
Thunderstorm Formation
Lightning
Lightning
How Lightning Forms How Lightning Forms
The connection is made and the protons rush up to meet the electrons. It is at that point that we see lightning and hear thunder. A bolt of lightning heats the air along its path causing it to expand rapidly.
Thunder is the sound caused
by rapidly expanding air.
Hail Hail
How does Hail Form?
How does Hail Form?
Strong updrafts of warm air and down- drafts of cold air are in a thunderstorm.
If a water droplet is picked up by the
updrafts...it can be carried well above the freezing level. With temperatures below 32°F...our water droplet freezes.
As the frozen droplet begins to
fall...carried by cold downdrafts...it may thaw as it moves into warmer air toward the bottom of the thunderstorm
But...it may also get picked up again by another updraft...carrying it back into very cold air and re-freezing it. With each trip above and below the freezing level our frozen droplet adds another layer of ice.
Finally...our frozen water droplet...with
What can hail do?
What can hail do?
Tornadoes Tornadoes
What is a tornado?
"a violently rotating column of air, pendant from a cumuliform
cloud or underneath a cumuliform cloud, and often (but not
always) visible as a funnel cloud."
HOW DO TORNADOES FORM?
HOW DO TORNADOES FORM?
WHERE DO TORNADOES FORM?
WHERE DO TORNADOES FORM?
WHY DO TORNADOES LIKE WHY DO TORNADOES LIKE THE CENTRAL U.S.?
THE CENTRAL U.S.?
Fujita Tornado Damage Scale Fujita Tornado Damage Scale
Scale
Scale Wind Estimate Wind Estimate (MPH)
(MPH) Typical Damage Typical Damage
F0 F0 < 73 < 73
Light – Some damage to chimneys, branches Light – Some damage to chimneys, branches broken, signs damaged.broken, signs damaged.
F1 F1 73-112 73-112
Moderate – Peels surface off roofs; mobile Moderate – Peels surface off roofs; mobile homes pushed off foundations or overturned.homes pushed off foundations or overturned.
F2 F2 113-157 113-157
Considerable – Roofs torn off frame houses, Considerable – Roofs torn off frame houses, mobile homes demolished, large trees snapped mobile homes demolished, large trees snappedF3 F3 158-206 158-206
Severe – Roofs and some walls torn off well Severe – Roofs and some walls torn off well constructed homes, trains overturnedconstructed homes, trains overturned
F4 F4 207-260 207-260
Devastating – Well-constructed homes leveled; Devastating – Well-constructed homes leveled;cars thrown and large missiles generated cars thrown and large missiles generated
F5 F5 261-318 261-318
Incredible – Strong frame houses leveled off Incredible – Strong frame houses leveled off foundation and swept away, trees debarked foundation and swept away, trees debarkedF0 Damage
F0 Damage
F1 Damage
F1 Damage
F2 Damage
F2 Damage
F3 Damage
F3 Damage
F4 Damage
F4 Damage
F5 Damage
F5 Damage
Tornado Embeds
Tornado Embeds
Tornado Embeds
Tornado Embeds
Tornado Embeds
Tornado Embeds
Rate the Tornado
Rate the Tornado
Rate the Tornado Rate the Tornado
F2
Rate the Tornado
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Rate the Tornado Rate the Tornado
F4
Rate the Tornado
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Rate the Tornado Rate the Tornado
F1
Rate the Tornado
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F2
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F4
Rate the Tornado
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F3
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F5
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F2
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F2
HURRICANES!
HURRICANES!
…An overview of tropical cyclones
…An overview of tropical cyclones
Tim Marchok Tim Marchok
NOAA/Geophysical Fluid Dynamics NOAA/Geophysical Fluid Dynamics Laboratory
Laboratory
timothy.marchok@noaa.gov timothy.marchok@noaa.gov
Princeton University
Quest Science Workshop
What is a hurricane?
What is a hurricane?
A hurricane is an intense cyclonic storm (i.e., a
cyclone) that begins as an area of low pressure over the tropical oceans.
“ “ Hurricane” is a specific regional Hurricane” is a specific regional name. In general, these storms are name. In general, these storms are
known as “tropical cyclones”:
known as “tropical cyclones”:
– Tropical depression: Tropical depression: winds < 39 mph winds < 39 mph – Tropical storm: Tropical storm: winds < 74 mph winds < 74 mph
– Hurricane: Hurricane: winds winds > > 74 mph 74 mph ( gets named! )
- - Atlantic and Eastern Pacific Oceans Atlantic and Eastern Pacific Oceans (hurricanes)
(hurricanes)
- Western North Pacific Ocean - Western North Pacific Ocean
(typhoons) (typhoons)
- South Pacific and Indian Oceans - South Pacific and Indian Oceans
(cyclones) (cyclones)
Where do tropical cyclones form?
(26) (10)
(14) (15)
(5) (9)
(nn) Number of storms per year
Why are the winds so strong in a Why are the winds so strong in a
hurricane?
hurricane?
Winds always move from areas of higher pressure to areas of lower pressure. The bigger the difference between the high and low pressure, the stronger the winds.
H L
The winds from Hurricane Fabian
battering Bermuda on
September 5, 2003
.What causes the winds to rotate around What causes the winds to rotate around
a hurricane?
a hurricane?
H
H H
H L
The Coriolis Effect: A change in the direction of moving objects due to
If the Coriolis effect causes objects to move to the right If the Coriolis effect causes objects to move to the right of the direction of motion in the Northern Hemisphere, of the direction of motion in the Northern Hemisphere, then why is the circulation counter-clockwise around a then why is the circulation counter-clockwise around a
low-pressure center?
low-pressure center?
H
H H
H L
Keep in mind that there is a mixture of forces that determines the path a particle of air takes, with the Coriolis effect being just one force. Previously, we’ve
seen how air moves from high to low pressure. The force that causes this is called the “pressure gradient
force” (PGF). At large distances from a low (e.g., at point A in the diagram on the right), there is almost a balance between the Coriolis effect and the PGF. As a
parcel of air gets closer to the low pressure center, often the pressure gradient intensifies (analogous to a terrain gradient increasing when on a mountainside and getting ready to drop rapidly into a canyon), accelerating
the parcel (this is felt in the increase of winds as you near a hurricane’s center). Close to a strong low, the influence of the Coriolis effect becomes unimportant compared to the PGF, and the parcel moves more in a direction towards the low. Very close to an intense hurricane’s center (e.g., at point B in the diagram on the
right), as the air rotates rapidly around the center, there is nearly a balance between the PGF and an
outward force due to centripetal acceleration.
A B
How is a lawn mower like a How is a lawn mower like a
hurricane?
hurricane?
Gas provides the fuel for the mower’s engine
The engine uses the fuel to perform work
and move the grass-cutting
blade
The starter rope and spark plug are
the “triggers” for making the mower
start
Exhaust fumes are expelled out
away from the
engine
The hurricane heat engine: how it The hurricane heat engine: how it
works works
3. Having lost most of its heat and energy, the air is now expelled outward away from the center of the storm in the cooler hurricane outflow at high levels.
In mature hurricanes, an eye forms in the center. Here, the air is
descending and the region is generally cloud-free.
2. The warm, moist air rises in thunderstorms surrounding the eye, supplying the fuel that helps strengthen the storm and intensify the winds.
1. As air rushes into the hurricane’s low pressure center, the air picks up heat and moisture (fuel) from the warm ocean surface.
H L H
Wind Damage examples Wind Damage examples
A 1x4 board of wood was
pierced
through a palm tree by
Hurricane
Andrew’s winds in August,
1992.
A mobile home park near Miami, FL was completely destroyed by Hurricane Andrew in August, 1992.
How are hurricanes different from tornadoes?
How are hurricanes different from tornadoes?
Hurricanes
Hurricanes Tornadoes Tornadoes
Where they form
Where they form Hurricanes form over warm Hurricanes form over warm water in the tropical oceans water in the tropical oceans and develop best when far and develop best when far
from the jet stream.
from the jet stream.
Tornadoes form over land Tornadoes form over land and form within storms and form within storms that are often very close that are often very close
to the jet stream to the jet stream
How big they are
How big they are Up to several hundred miles wideUp to several hundred miles wide No more than ¼ mile wideNo more than ¼ mile wide
How long they last
How long they last Average of 9 days (up to 3 Average of 9 days (up to 3 weeks)
weeks) No more than an hourNo more than an hour
How strong the winds How strong the winds
areare
Less than 200 mph
Less than 200 mph Up to 300 mphUp to 300 mph
Occurrences per year
Occurrences per year An average of 10 tropical storms An average of 10 tropical storms in the Atlantic Ocean
in the Atlantic Ocean In the United States, 800-In the United States, 800- 10001000
Advance warning from Advance warning from forecasters
forecasters
Several days
Several days No more than 15-30 minutesNo more than 15-30 minutes
Saffir Simpson Scale
Saffir Simpson Scale
Storm Surge
Storm Surge
Storm Surge examples Storm Surge examples
Storm surge from
Hurricane Carol
completely inundates a yacht club in August, 1954.
Hurricane Katrina’s 30-foot storm surge obliterated every home within several blocks of the shoreline in Pass Christian and Waveland, Mississippi.