Weather exam 2

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Last updated 2:22 PM on 9/17/26
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178 Terms

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Earth's axial tilt / obliquity

Approximately 23.5

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Sun directly over the Tropic of Capricorn

Winter solstice

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Northern Hemisphere winter

Occurs when the Northern Hemisphere tilts away from the Sun

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When Earth is closest to the Sun

Perihelion

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When Earth is farthest from the Sun

Aphelion

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Order of sunrise stages

Astronomical sunrise occurs first, followed by nautical sunrise, then civil sunrise

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Fundamental cause of global wind circulation

Differences in solar energy receipt

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Equatorial region

Typically referred to as the ITCZ (Intertropical Convergence Zone)

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Typical wind direction from 60–90 degrees North and South

Easterly

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Boundary between warmer tropical air and colder polar air

Polar Front

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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

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Typical number of air masses over the United States at one time

5

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Air mass

A large body of air with similar horizontal characteristics of moisture and temperature

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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)

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Warm air moving into cold air

The boundary is called a warm front

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Cold fronts

Cause uplift when they meet warm air

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Occluded front

A front in which a mass of warm air is cut off from the surface

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First step in classical cyclogenesis

A polar front separates masses of warm and cold air

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Last step in classical cyclogenesis

Occlusion occurs

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Anticyclone

A high-pressure system

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Station model: light rain

Two black dots side by side

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Station model: 75% black central circle

Cloud cover ranges over 70 to 80 percent of the sky

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Three stages of an air-mass thunderstorm

Towering cumulus, mature, dissipating

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Air-mass thunderstorms

Extinguish themselves through the formation of extensive downdrafts

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Thunderstorms in the United States are most common in

Florida

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Lightning

A discharge of static electricity

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Most lightning discharges

Occur within clouds

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Typical cloud-to-ground lightning event

Several distinct steps that look to the human eye like a single lightning strike

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Principal hazard of microbursts to aircraft during takeoff or landing

Sudden changes in lift and tailwinds

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NOT a reason for flooding from thunderstorms

Downdrafts

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Month when tornadoes are most likely in the United States

May

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Mesocyclone formation

The horizontal tube of air must be tilted upward

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Thunderstorm ingredients

Moisture, a lifting mechanism, and instability

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Thunderstorm ingredient: moisture

Moisture is one of the required ingredients for thunderstorm development

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Thunderstorm lifting mechanism: convection

Convection is a lifting mechanism for thunderstorms

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Thunderstorm lifting mechanism: orographic lifting

Orographic lifting is a lifting mechanism in which terrain forces air upward

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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

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Developing thunderstorm stage

Also called the towering cumulus stage, updrafts dominate

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Mature thunderstorm stage

Strong updrafts and induced downdrafts occur, heavy rain and an anvil top are present

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Dissipating thunderstorm stage

Downdraft dominates

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Severe thunderstorms

Can occur as a series of storms called a mesoscale convective system (MCS) or mesoscale convective complex (MCC)

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Pennsylvania thunderstorm note

The severe-weather slides state that mostly air-mass thunderstorms occur in Pennsylvania, not MCSs

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Downdrafts and storm systems

Downdrafts can propagate to other storms, and the whole system can rotate

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Hail formation

Updrafts cause riming

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U

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S

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record hail stone listed in the slides

Vivian, South Dakota, July 23, 2010, 8-inch diameter, 1

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94 pounds

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Microburst

A concentrated downdraft that moves straight down and then spreads outward, winds can reach 100 mph

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Lightning: basic definition

Static electricity, a huge electrical discharge

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Lightning voltage listed in the slides

More than 100 million volts

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Lightning duration listed in the slides

A fraction of a second

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Lightning temperature effect

Lightning heats air to more than 54,000°F

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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

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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

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Thunder

Always occurs with lightning, although you may not hear it

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It results from rapid expansion and contraction of air

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Heat lightning

Lightning whose thunder may not be heard

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Lightning deaths

The slides list about 100–200 deaths annually, with most in Florida

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Lightning safety

Stay indoors or in your car, do not touch anything, stay away from isolated or tall trees

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If your hair stands on end, crouch alone on the balls of your feet to reduce the path available for current

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Tornadoes

Associated with severe thunderstorms, especially supercells, the slides identify intense low pressure and wind shear as associated conditions

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Mesocyclone

Forms when the horizontal tube of air is tilted upward

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Hurricane: names and locations

Hurricane: Atlantic and eastern Pacific

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Typhoon: western Pacific

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Tropical cyclone: Indian Ocean

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Relative size: tornado

Less than 7 miles wide

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Relative size: thunderstorm

About 10–100 miles wide

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Relative size: hurricane

About 200–400 miles wide

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Relative size: midlatitude cyclone

About 500–800 miles wide

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Hurricane structure

Low-pressure center, strong pressure gradient, high winds, spiraling thunderstorms, warm core, ocean water, condensation, low temperatures aloft, and cirrostratus clouds

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Hurricane eye

The center of the hurricane, about 15 miles in diameter in the slide example, has clear sky, light wind, and descending air

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Hurricane eyewall

The most intense part of the storm

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Hurricane rain bands

Spiraling bands of thunderstorms around the hurricane

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Hurricane formation: easterly wave

A disruption in the easterly trade winds, associated with the west coast of Africa

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Convergence on the eastern side of the wave creates a tighter gradient, rising air, and a tropical disturbance

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Easterly wave movement

Typically moves 10–20 mph and takes about 7–10 days to cross the Atlantic

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Hurricane formation: warm water

Warm ocean water enhances development, the slides specify a deep warm layer around 81°F (28°C)

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Previous hurricanes can mix the water layer

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Instability and condensation are also involved

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Hurricane season

June 1 to November 30

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Saffir-Simpson: tropical depression

Less than 37 mph

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Saffir-Simpson: tropical storm

38–73 mph

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Saffir-Simpson: Category 1

74–95 mph

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Saffir-Simpson: Category 2

96–110 mph

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Saffir-Simpson: Category 3

111–130 mph

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Saffir-Simpson: Category 4

131–155 mph

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Saffir-Simpson: Category 5

More than 156 mph

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General hurricane movement: easterly trades

Move storms from east to west

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General hurricane movement: Bermuda High

Helps guide hurricanes from south to north

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General hurricane movement: westerlies

Can move storms from west to east

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Hurricane movement

Overall movement depends on easterly trades, the Bermuda High, westerlies, and specific weather conditions

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Storm surge

A rise in coastal water level caused by winds piling water toward the coast and low pressure raising the water level

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Most dangerous part of a hurricane

Storm surge

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Storm surge especially dangerous when

It coincides with high tide, especially around a new or full moon, and in low-lying areas

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Hurricane right-front quadrant

The most severe weather occurs here, including strong wind, heavy rain, tornadoes, and storm surge

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Right-front quadrant conditions

The slides associate the most severe quadrant with warm water and note that there is no land

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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

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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

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Hurricane Katrina

August 23–31, 2005, lowest pressure 902 mb, highest wind 175 mph, damage $160 billion, listed as costliest in U