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Earth's axial tilt / obliquity
Approximately 23.5
Sun directly over the Tropic of Capricorn
Winter solstice
Northern Hemisphere winter
Occurs when the Northern Hemisphere tilts away from the Sun
When Earth is closest to the Sun
Perihelion
When Earth is farthest from the Sun
Aphelion
Order of sunrise stages
Astronomical sunrise occurs first, followed by nautical sunrise, then civil sunrise
Fundamental cause of global wind circulation
Differences in solar energy receipt
Equatorial region
Typically referred to as the ITCZ (Intertropical Convergence Zone)
Typical wind direction from 60–90 degrees North and South
Easterly
Boundary between warmer tropical air and colder polar air
Polar Front
Three-cell model and Coriolis
If global circulation were driven only by temperature gradients, there would be one circulation cell in each hemisphere. Earth's three-cell structure is associated with the Coriolis effect
Typical number of air masses over the United States at one time
5
Air mass
A large body of air with similar horizontal characteristics of moisture and temperature
Air mass descriptors
The class material identifies moisture and temperature as the key horizontal characteristics used to describe an air mass. Air mass dominant over the southeastern USA, especially in summer: mT (maritime tropical)
Warm air moving into cold air
The boundary is called a warm front
Cold fronts
Cause uplift when they meet warm air
Occluded front
A front in which a mass of warm air is cut off from the surface
First step in classical cyclogenesis
A polar front separates masses of warm and cold air
Last step in classical cyclogenesis
Occlusion occurs
Anticyclone
A high-pressure system
Station model: light rain
Two black dots side by side
Station model: 75% black central circle
Cloud cover ranges over 70 to 80 percent of the sky
Three stages of an air-mass thunderstorm
Towering cumulus, mature, dissipating
Air-mass thunderstorms
Extinguish themselves through the formation of extensive downdrafts
Thunderstorms in the United States are most common in
Florida
Lightning
A discharge of static electricity
Most lightning discharges
Occur within clouds
Typical cloud-to-ground lightning event
Several distinct steps that look to the human eye like a single lightning strike
Principal hazard of microbursts to aircraft during takeoff or landing
Sudden changes in lift and tailwinds
NOT a reason for flooding from thunderstorms
Downdrafts
Month when tornadoes are most likely in the United States
May
Mesocyclone formation
The horizontal tube of air must be tilted upward
Thunderstorm ingredients
Moisture, a lifting mechanism, and instability
Thunderstorm ingredient: moisture
Moisture is one of the required ingredients for thunderstorm development
Thunderstorm lifting mechanism: convection
Convection is a lifting mechanism for thunderstorms
Thunderstorm lifting mechanism: orographic lifting
Orographic lifting is a lifting mechanism in which terrain forces air upward
Atmospheric instability
Unstable air means rising air, the atmosphere becomes more unstable when it is colder with height and when dry air is above humid air
Developing thunderstorm stage
Also called the towering cumulus stage, updrafts dominate
Mature thunderstorm stage
Strong updrafts and induced downdrafts occur, heavy rain and an anvil top are present
Dissipating thunderstorm stage
Downdraft dominates
Severe thunderstorms
Can occur as a series of storms called a mesoscale convective system (MCS) or mesoscale convective complex (MCC)
Pennsylvania thunderstorm note
The severe-weather slides state that mostly air-mass thunderstorms occur in Pennsylvania, not MCSs
Downdrafts and storm systems
Downdrafts can propagate to other storms, and the whole system can rotate
Hail formation
Updrafts cause riming
U
S
record hail stone listed in the slides
Vivian, South Dakota, July 23, 2010, 8-inch diameter, 1
94 pounds
Microburst
A concentrated downdraft that moves straight down and then spreads outward, winds can reach 100 mph
Lightning: basic definition
Static electricity, a huge electrical discharge
Lightning voltage listed in the slides
More than 100 million volts
Lightning duration listed in the slides
A fraction of a second
Lightning temperature effect
Lightning heats air to more than 54,000°F
Lightning charge separation
Friction from rising and sinking hail and water helps separate charge, lighter hail or drops are carried toward the top and carry positive charge, while negative charge develops at the bottom of the cloud
Cloud-to-ground lightning sequence
A positive charge on the ground is attracted, a stepped leader comes from the cloud and a return stroke comes from the ground
Thunder
Always occurs with lightning, although you may not hear it
It results from rapid expansion and contraction of air
Heat lightning
Lightning whose thunder may not be heard
Lightning deaths
The slides list about 100–200 deaths annually, with most in Florida
Lightning safety
Stay indoors or in your car, do not touch anything, stay away from isolated or tall trees
If your hair stands on end, crouch alone on the balls of your feet to reduce the path available for current
Tornadoes
Associated with severe thunderstorms, especially supercells, the slides identify intense low pressure and wind shear as associated conditions
Mesocyclone
Forms when the horizontal tube of air is tilted upward
Hurricane: names and locations
Hurricane: Atlantic and eastern Pacific
Typhoon: western Pacific
Tropical cyclone: Indian Ocean
Relative size: tornado
Less than 7 miles wide
Relative size: thunderstorm
About 10–100 miles wide
Relative size: hurricane
About 200–400 miles wide
Relative size: midlatitude cyclone
About 500–800 miles wide
Hurricane structure
Low-pressure center, strong pressure gradient, high winds, spiraling thunderstorms, warm core, ocean water, condensation, low temperatures aloft, and cirrostratus clouds
Hurricane eye
The center of the hurricane, about 15 miles in diameter in the slide example, has clear sky, light wind, and descending air
Hurricane eyewall
The most intense part of the storm
Hurricane rain bands
Spiraling bands of thunderstorms around the hurricane
Hurricane formation: easterly wave
A disruption in the easterly trade winds, associated with the west coast of Africa
Convergence on the eastern side of the wave creates a tighter gradient, rising air, and a tropical disturbance
Easterly wave movement
Typically moves 10–20 mph and takes about 7–10 days to cross the Atlantic
Hurricane formation: warm water
Warm ocean water enhances development, the slides specify a deep warm layer around 81°F (28°C)
Previous hurricanes can mix the water layer
Instability and condensation are also involved
Hurricane season
June 1 to November 30
Saffir-Simpson: tropical depression
Less than 37 mph
Saffir-Simpson: tropical storm
38–73 mph
Saffir-Simpson: Category 1
74–95 mph
Saffir-Simpson: Category 2
96–110 mph
Saffir-Simpson: Category 3
111–130 mph
Saffir-Simpson: Category 4
131–155 mph
Saffir-Simpson: Category 5
More than 156 mph
General hurricane movement: easterly trades
Move storms from east to west
General hurricane movement: Bermuda High
Helps guide hurricanes from south to north
General hurricane movement: westerlies
Can move storms from west to east
Hurricane movement
Overall movement depends on easterly trades, the Bermuda High, westerlies, and specific weather conditions
Storm surge
A rise in coastal water level caused by winds piling water toward the coast and low pressure raising the water level
Most dangerous part of a hurricane
Storm surge
Storm surge especially dangerous when
It coincides with high tide, especially around a new or full moon, and in low-lying areas
Hurricane right-front quadrant
The most severe weather occurs here, including strong wind, heavy rain, tornadoes, and storm surge
Right-front quadrant conditions
The slides associate the most severe quadrant with warm water and note that there is no land
Hurricane naming
All depressions are given names, names are alphabetical using 21 letters, there are 6 rotating lists, a supplemental list is used if names run out, male and female names alternate, famous names can be retired
2005 Atlantic hurricane season
28 named storms (record at the time), 7 Category 3 or stronger, strongest was Wilma at 882 mb and 185 mph, damage exceeded $100 billion (record at the time), and fatalities were 2,048
Hurricane Katrina
August 23–31, 2005, lowest pressure 902 mb, highest wind 175 mph, damage $160 billion, listed as costliest in U