7.E.1.3 Severe Storms & 7.E.1.5 Air Mass & Wind – Study Guide

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Vocab Words to know

What is an air mass

Names of Air Masses

Air masses that affect US weather

Air masses are classified by

Different types of wind

What is pressure gradient

How does the Coriolis effect affect wind

Warm vs. cold current

Major types of storms

El Nino

7.E.1.3 Severe Storms & 7.E.1.5 Air Mass & Wind – Study Guide

Know all your vocabulary words large section of the lower troposphere that has the same weather throughout continental maritime tropical polar arctic continental tropical (cT) continental polar (cP) maritime tropical (mT) maritime polar (mP) moisture and temperature of an area where it formed

Local

Sea Breeze - Land heats faster during day then water; occurs only during day

Land breeze - Water stays warmer at night than land; occurs only during night

Global

Polar easterlies  cold, fairly weak winds blowing from east to west

Doldrums  very calm air in a band over the equator

Trade winds  warm, steady winds that blow back toward the equator in usually

 clear skies

Prevailing westerlies

Unseasonably warm weather patterns

Fish die and storms reign all over the globe

 cool air, usually moving quickly toward the poles from west to east in both hemispheres

Earth’s rotation causes winds to curve

Curves right in northern hemisphere

Curves left in the southern hemisphere

Molecules move faster in warmer air

Steeper pressure gradient  stronger wind

Warm – starts near equator moves towards poles; shallow water

Cold – starts near poles, moving towards equator; deep water

Gulf Stream o o

Responsible for weather in Europe

One of the strongest known warm currents

3 causes of storms

Different types of precipitation

7.E.1.3 Severe Storms & 7.E.1.5 Air Mass & Wind – Study Guide

Heat of sun

Water in air

Spin of earth

Types of

Precipitation Description

Rain

Snow

Sleet

Freezing rain precpitation falling through only warm air precpitation falling through only cold air occurs when ice crystals begin to fall through warm air, encounter cold air at the surface and refreeze falls through mostly warm air, until it nears the ground where it encounters cold air and freezes again

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