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Slide 1
Visualizing Physical Geography
by Alan Strahler and Zeeya Merali
Chapter 6
Weather Systems
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 2
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Chapter Overview
Air Masses
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Fronts
Midlatitude Cyclones
Tropical Cyclones
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Thunderstorms and
Tornadoes
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 3
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Air Masses
Weather
• Weather refers to the state of the atmosphere at one
location and at one time
• Weather variables include:
• Temperature
• Moisture (Dew Point and RH)
• Precipitation
• Winds
• Weather conditions
change from day to day
or even from hour to hour
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 4
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Air Masses
Weather
• Weather systems are patterns of atmospheric circulation
that lead to distinctive weather events, such as cyclones
or thunderstorms.
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 5
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Air Masses
Weather
• Air mass = An extensive body of air in which
temperature and moisture characteristics are fairly
uniform over a large area
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1) What is the current high temperature, wind, moisture (dew
point), and precipitation forecast for today?
2) Based on today’s weather, where do you think the air mass
came from?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 6
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 7
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Air Masses
Source Regions of Air Masses
•Source region: region where an air mass
acquires its characteristics
•Moisture characterized by whether it
came from the:
• Ocean = moist = m
• Continent (land) = drier = c
•Also classified by latitude:
• Maritime equatorial (mE)
• Maritime tropical (mT)
• Continental tropical (cT)
• Maritime polar (mT)
• Continental Arctic (cA)
• Continental Antarctic (cAA)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 8
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Air Masses
Source Regions of Air
Masses
•Maritime equatorial (mE)
•Maritime tropical (mT)
•Continental tropical (cT)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 9
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Air Masses
Source Regions of Air
Masses
•Maritime polar (mT)
•Continental Arctic (cA)
•Continental Antarctic (cAA)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 10
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Air Masses
Movement of Air
Masses (Air mass
modification)
• When an air mass
moves to a new
area, its properties
change due to the
influence of the new
surface environment
What air mass is impacting your region today?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 11
Fronts
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Front = The surface or boundary of contact between
two different air masses associated with a
midlatitude cyclone (MLC)
• Four types of fronts:
• Cold
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• Warm
• Stationary
• Occluded
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 12
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Fronts
Cold Front
• A moving weather front along which a cold air mass
moves underneath a warm air mass, causing the warm
air mass to lift rapidly
• Air rises steeply
• Cumulonimbus clouds and thunderstorms may form
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 13
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Fronts
Warm Front
• A moving weather front along which a warm air mass
slides over a cold air mass, producing stratiform clouds
and precipitation
•Air rises gradually
•Nimbostratus clouds may form
Which type of clouds first
indicates an approaching
warm front?
a. nimbostratus
b. stratus
c. altostratus
d. cirrus
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 14
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Fronts
Occluded front
• A weather front along which a fast-moving cold front
overtakes a warm front, forcing the warm air mass aloft
• Triangles and semicircles pointing in the same direction
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Stationary Front
• Little to no relative motion
• Blue triangles and red semicircles pointing in opposite
directions
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 15
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Fronts
1. Why was the warm air forced upward?
2. The clouds mark an advancing front. What type of front
might this be?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 16
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Midlatitude Cyclones
Cyclones
• Air spirals inward, converges and moves upward
• As the air rises, it cools adiabatically
• If the air becomes saturated at the LCL, condensation or
deposition occurs, forming clouds and possibly
precipitation
• Low pressure
• Three types: midlatitude cyclone (MLC), tropical cyclone,
and mesocyclone
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Anticyclone
•
•
•
•
Air spirals outward and diverges as it sinks
The air warms as it sinks
Fair skies
High pressure
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 17
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Midlatitude Cyclones
Cyclones and Anticyclones
C
B
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A
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1) Is a cyclone or anticyclone impacting the region shown in
Figure A?
2) Is a cyclone or anticyclone impacting letter C?
3) Is a cyclone or anticyclone impacting letter A?
___________________________________
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 18
Midlatitude Cyclones (MLC)
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Evolution of a midlatitude cyclone
• Midlatitude cyclone also known as a wave cyclone
• Dominant in middle and higher latitudes
• Large inspiral of air that repeatedly forms, intensifies,
and dissolves along the polar front
• In the northern hemisphere, a cyclone normally forms
at a polar front and moves eastward as it develops,
propelled by prevailing westerly winds aloft
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 19
Midlatitude Cyclones (MLC)
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Evolution of a midlatitude cyclone
• Initial conditions
• Cyclogenesis
• Open stage
• Occluded stage
• Dissolving stage
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 20
Midlatitude Cyclones
(MLC)
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In the open stage of the cyclone depicted in step 3, a ____ air mass could
be behind the warm front, and a ___ air mass could be behind the cold front.
a. maritime tropical; continental polar
b. continental polar; maritime tropical
c. maritime polar; continental tropical
d. continental polar; continental tropical
___________________________________
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 21
Midlatitude Cyclones (MLC)
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Weather changes within a midlatitude cyclone
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 22
Midlatitude Cyclones (MLC)
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Weather changes within a midlatitude cyclone
• Cyclonic storm = An intense weather disturbance within a
moving cyclone that generates strong winds, cloudiness,
and precipitation
• Nor’easter
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 23
Tropical Cyclones
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Tropical Cyclone
• An intense traveling cyclone of
tropical and subtropical latitudes,
accompanied by high winds and
heavy rainfall
• Naming:
• Hurricanes in western
hemisphere
• Typhoons in the western
Pacific
• Cyclones in the Indian Ocean
• Develop over oceans approximately
between 8 to 20oN/S
• Winds greater than 74 mph
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 24
Tropical Cyclones
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Tropical Cyclone
• Characteristics
• Eye = relatively calm, sinking air at its center
• Eyewall = strongest section, with intense rising air and
wind
• Spiral rain bands
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 25
Tropical Cyclones
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Formation of Tropical Cyclones
• Four conditions need to be in place:
• Low pressure
• Weak Coriolis force
• High humidity
• Warm sea surface temperatures
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 26
Tropical Cyclones
Formation and Movement of
Tropical Cyclones
• Tropical cyclone originates as a
slow-moving band of low
pressure, which then intensifies
and grows into a deep, circular
low
• Easterly wave = a slowly moving
trough of low pressure within the
belt of tropical easterlies
(trades) that grows over the
warm ocean
• Does not form over the equator
since there is no coriolis force
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 27
Tropical Cyclones
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Formation and Movement of Tropical Cyclones
• High humidity = Always form over the warm ocean with
high water vapor content.
• Warm sea surface temperatures (SST) greater than 81oF
• Season = peaks in late summer/early autumn due to
warmest SST
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___________________________________
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 28
Tropical Cyclones
Movement of Tropical
Cyclones
• Typically, clockwise
movement in the N.
hemisphere
• West with trade winds
• Then moves northwest,
north, and eventually
northeast following the
winds from the
subtropical high and
the upper level
westerlies
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 29
Tropical Cyclones
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Tropical cyclones do not form in the southern Atlantic Ocean because _____.
a. the water is too warm
b. the water is not warm enough
c. cyclones rotate clockwise in the southern hemisphere
d. cyclone tracks would hit land
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 30
Tropical Cyclones
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Movement of Tropical Cyclones
• Hurricane tracks for 1985–1994 (blue) and 1995–2004 (red)
• The intensity of storms increases when sea surface
temperatures increase
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 31
Tropical Cyclones
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Significant Tropical Cyclones
• Naming of Tropical Cyclones
• Hurricane Andrew (1992)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 32
Tropical Cyclones
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 33
Tropical Cyclones
Tropical Cyclone Intensity and Damage
• Saffir-Simpson Scale
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 34
Tropical Cyclones
Tropical Cyclone Intensity and Damage
• Precipitation
• Earthflow
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 35
Tropical Cyclones
Tropical Cyclone Intensity and Damage
• Storm Surge
• A rapid rise of coastal water level accompanying the
onshore arrival of a tropical cyclone
• Deadliest aspect of tropical cyclone
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 36
Tropical Cyclones
Tropical Cyclone Intensity and Damage
• Hurricane Katrina Flooding (2005) in New Orleans
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 37
Thunderstorms and Tornadoes
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Thunderstorms and Unstable Air
• Thunderstorms may form as a result of intense heating of
the ground, resulting in the heated parcel of air warmer
(and less dense) than the surrounding air
• Air cools to the dew point, clouds form (cumulus) and may
grow into cumulonimbus (thunderstorm) clouds
• Clouds and storm may dissipate with the loss of heating
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___________________________________
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 38
Thunderstorms and Tornadoes
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Thunderstorm
• An intense local storm associated with a tall, dense
cumulonimbus cloud in which there are very strong
updrafts of air
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 39
Thunderstorms and Tornadoes
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Severe Thunderstorm
• Intense winds,
precipitation, and hail
• Strong updrafts and
downdrafts
• Anvil shape
• Wind shear
• Change in wind
velocity with height
• Required in a severe
thunderstorm
• May result in rotation
(mesocyclone)
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In which direction is this
thunderstorm moving, and how
do you know?
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
___________________________________
Slide 40
Thunderstorms and Tornadoes
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Lightning
• Upward and
downward motions
in a thunderstorm
create areas of
positive and
negative static
charge within the
cloud that are
discharged by
lightning
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 41
Thunderstorms and Tornadoes
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Forecasting Thunderstorms
• Hot, summer weather in central and SE US
• National Oceanic and Atmospheric Administration
(NOAA) and National Weather Service (NWS)
• For a thunderstorm outlook, go to:
www.spc.noaa.gov/products/exper/enhtstm/
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 42
Thunderstorms and Tornadoes
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Tornadoes
• A small, very intense wind vortex with extremely low air
pressure in the center, formed below a dense
cumulonimbus cloud as apart of a cyclone, typically an MLC
• Mesocyclone (rotating thunderstorm)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 43
Thunderstorms and Tornadoes
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Tornadoes
• Enhanced Fujita
Scale
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 44
Thunderstorms and Tornadoes
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Tornadoes
• Most Common in
central (tornado
alley) and SE
United States
where cold and
warm air clash
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 45
Thunderstorms and Tornadoes
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Which stage of a thunderstorm leads to tornado formation?
a. cumulus
b. mature
c. dissipating
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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