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Water and Weather

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Water and Weather Chapter Six: Weather and Climate 6.1 Introduction to Weather 6.2 Weather Patterns 6.3 Climates and Biomes Investigation 6B How does Doppler radar work? – PowerPoint PPT presentation

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Title: Water and Weather


1
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2
Water and Weather
3
Chapter Six Weather and Climate
  • 6.1 Introduction to Weather
  • 6.2 Weather Patterns
  • 6.3 Climates and Biomes

4
Investigation 6B
Storms
  • How does Doppler radar work?

5
6.2 Meteorology
  • A meteorologist is a person who uses scientific
    principles to explain, understand, observe, or
    forecast Earths weather.

6
6.2 Meteorology
  • Many meteorologists have college degrees in
    physics, chemistry, or mathematics.

7
6.2 Meteorology
  • Meteorologists use satellite and computer
    technology to inform people about the weather.

8
6.2 Water in the atmosphere
  • Higher temperatures cause liquid water molecules
    to move faster.
  • These water molecules become water vapor in the
    atmosphere.

9
6.2 Cloud formation
  • Different conditions cause different clouds.
  • Cumuliform clouds include
  • cirrocumulus
  • altocumulus
  • cumulus
  • cumulonimbus

10
6.2 Cloud formation
  • Stratiform clouds form when a large mass of
    stable air gradually rises, expands, and cools.
  • Stratiform clouds include
  • cirrostratus
  • altostratus
  • stratus
  • nimbostratus

11
6.2 Cloud formation
  • Sometimes a cloud formation combines aspects of
    both cumuliform and stratiform clouds.
  • We call these clouds stratocumulus clouds.

12
6.2 Cloud formation
  • Cirrus clouds are thin lines of ice crystals high
    in the sky, above 6,000 meters.
  • They are just a thin streak of white across a
    blue sky.

13
6.2 Rain
  • Rain is the result of a cooling air mass.
  • Cooling an air mass is like wringing out a wet
    sponge.
  • Tiny droplets form a cloud or fog.
  • Larger droplets fall as rain.

14
6.2 Snow
  • Snow usually forms when both ice crystals and
    water droplets are present in the sky.
  • The water droplets attach to ice crystals and
    freeze.
  • When the ice crystals are large enough, they will
    fall to the ground as snow.

15
6.2 Air masses and fronts
  • An air mass is a large body of air with
    consistent temperature and moisture
    characteristics throughout.
  • Two air masses that affect the United States are
    the continental polar air mass and the maritime
    tropical air mass.

Changing conditions and global winds cause these
air masses to move.
16
6.2 Fronts
  • A cold front occurs when cold air moves in and
    replaces warm air.

17
6.2 Fronts
  • A warm front occurs when warm air moves in and
    replaces cold air.

18
6.2 Fronts
  • On a weather map, a cold front is shown using a
    line marked with triangles.
  • The triangles point in the direction the front is
    moving.
  • A warm front is shown using a line marked with
    semicircles.

19
6.2 Low- and high-pressure areas
  • When a cold front moves into a region and warm
    air is forced upward, an area of low pressure is
    created near Earths surface at the boundary
    between the two air masses.
  • A center of high pressure tends to be found where
    a stable cold air mass has settled in a region.

20
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21
6.2 Thunderstorms
  • Thunderstorms occur because of convection in the
    atmosphere.
  • The downdraft and updraft form a type of
    convection cell called a storm cell within the
    cloud.

22
6.2 Lightning
  • Lightning is a bright spark of light that occurs
    within a storm cloud, between a cloud and Earths
    surface, or between two storm clouds.

23
6.2 Hurricanes
  • A hurricane is a tropical cyclone with wind
    speeds of at least 74 miles (119 km) per hour.
  • The Saffir-Simpson Hurricane Scale is one scale
    used for rating hurricanes.

24
6.2 Tornadoes
  • A tornado, like a hurricane, is a system of
    rotating winds around a low-pressure center.
  • As the rotating wind pattern narrows and
    lengthens, it forms a funnel cloud.

25
6.2 El Nino Southern Oscillations
  • Storm patterns across the globe can happen in
    cycles.
  • Usually the trade winds blow warm water from east
    to west across the Pacific Ocean.
  • Every so often the trade winds weaken and the
    warm water reverses direction.

26
6.2 El Nino Southern Oscillations
  • Along with warm water comes greater thunderstorm
    activity across the Pacific.
  • This change in wind flow, air pressure, and
    thunderstorm activity is known as the El Niño
    Southern Oscillation.
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