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Slide 1
Visualizing Physical Geography
by Timothy Foresman & Alan Strahler
Chapter 5
Global Atmospheric and Oceanic Circulation
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 2
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Chapter Overview
Atmospheric Pressure
Wind Speed and Direction
Global Wind and Pressure
Patterns
Local Winds
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Oceanic Circulation
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 3
Atmospheric Pressure
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Atmospheric pressure
• Pressure exerted by the atmosphere
because of the force of gravity acting
on the overlying column of air
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Measuring Atmospheric Pressure
• Units = inches of mercury (in. Hg) or
millibars (mb)
• Standard sea level pressure = 1013.2
mb
• Cold, clear night pressure > 1013.2 mb
• Center of a storm with rising warm air
will have a pressure lower than 1013.2
mb
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 4
Atmospheric Pressure
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Measuring Atmospheric Pressure
• Radiosonde (balloon) is launched twice
a day at key locations in United States
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• Radiosondes measure:
• Pressure
• Altitude
• GPS location
• Temperature
• Relative humidity
• Wind speed and direction
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Would one expect low or higher than standard sea level
pressure in a hurricane?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 5
Atmospheric Pressure
Atmospheric Pressure and
Altitude
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• Atmospheric Pressure decreases
with altitude
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 6
Wind Speed and Direction
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Wind
• Horizontal movement of air
• Renewable resource
• Measured with an anemometer
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Wind Direction
• Identified by the direction from
which the wind comes
• West wind blows from west to east
• Measured with a wind vane
Wind speed and direction are determined by 3 factors:
pressure gradient, coriolis effect, and friction
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 7
Wind Speed and Direction
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Pressure Gradients
• Change of atmospheric pressure measured along a line at
right angles to the isobars
• Pressure gradient goes from high to low pressure
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 8
Wind Speed and Direction
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Pressure Gradients
• Isobar = line on a map drawn through all points having the
same atmospheric pressure
• Widely spaced isobars  weak gradient and weaker winds
• Closely spaced isobars  strong PG and stronger winds
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Where would you find the
greatest pressure gradient
on this map?
a. Oklahoma City
b. Southwestern Missouri
c. Memphis
d. Nashville
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 9
Wind Speed and Direction
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Pressure Gradients
• Unequal heating of
the Earth’s surface
leads to a pressure
gradient and causes
wind
• Latitude, terrain
differences and land
cover can cause
uneven heating,
pressure gradients
and wind
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2
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3
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 10
Wind Speed and Direction
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Pressure Gradients
If the island were in the
Arctic and covered by
glacial ice, would the
pressure gradient be the
same or different?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 11
Wind Speed and Direction
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The Coriolis Effect (CE)
• An effect of the Earth’s rotation that acts like a force to
deflect a moving object on the Earth’s surface to the:
• Right in the northern hemisphere
• Left in the southern hemisphere
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 12
Wind Speed and Direction
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The Coriolis Effect (CE)
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• Due to Earth’s rotation, a path from the North Pole to
Chicago along 74° W meridian would curve to the right,
toward Chicago.
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 13
Wind Speed and Direction
The Geostrophic
Wind
• Wind at high
levels (upper
levels) above the
Earth’s surface
moving parallel to
the isobars, at a
right angle to the
pressure gradient
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 14
Wind Speed and Direction
The Frictional Force
(FF)
• Force exerted by the
ground surface that is
proportional to the
wind speed and always
acts in the opposite
direction to the
direction of motion
• Greatest closest to the
surface
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 15
Wind Speed and Direction
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Cyclone (low pressure)
• The PGF, CE, and FF cause the surface wind to spiral,
converging inwards towards the low-pressure center
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• As the inward motion converges, it forces the air to rise
(uplift)  cools adiabatically  clouds and precipitation
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 16
Wind Speed and Direction
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Anticyclone (high pressure)
• Upper troposphere winds spins downward (subsidence) and
diverges outward at the surface
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• Air warms adiabatically as it sinks  inhibiting clouds and
precipitation
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 17
Global Wind and Pressure Patterns
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Global surface winds on an ideal Earth
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•Surface winds are shown on the disk of the Earth, and the
cross section at the right shows winds aloft
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 18
Global Wind and Pressure Patterns
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Tropical Circulation
• Warm air over the equator
rises and form low
pressure resulting in the
equatorial trough (wet
weather)
• Trade winds converge at
the equator
• Air descends near 25 to
30o latitude forming a
subtropical high pressure
(dry weather) zone
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 19
Global Wind and Pressure Patterns
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Tropical Circulation
• Hadley Cell = A lowlatitude atmospheric
circulation cell with rising
air over the equatorial
trough and sinking air
over the subtropical highpressure belts.
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 20
Global Wind and Pressure Patterns
Intertropical Convergence Zone
(ITCZ)
• A zone of convergence of air
masses along the equatorial trough
• Doldrums
• ITCZ shifts with the seasons
following the zone of highest
insolation
• Over the ocean it shifts a few
degrees between January and
July
• Over land, the zone shifts 20o to
as much as 40o in Asia
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 21
Global Wind and Pressure Patterns
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Tropical Circulation
• Monsoon = seasonal reversal of
the wind
• January = north wind (dry)
• July = warm, moist air (wet)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 22
Global Wind and Pressure Patterns
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Considering the direction of the winds compared to the
isobars, which statement is most correct?
a. Because this area is near
the equator, the Coriolis effect
has no influence on these winds.
b. Because the pressure gradients
are great, friction has no influence
on these winds.
c. Because some of the winds are over the ocean, neither the
Coriolis effect nor friction has an influence on these winds.
d. Because the alignment of the wind direction is at 45° to the
isobars, both the Coriolis effect and friction are important.
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 23
Global Wind and Pressure Patterns
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North American Monsoon
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 24
Global Wind and Pressure Patterns
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Subtropical High Pressure Cells
• Area of high atmospheric
pressure centered at
about 30° N and 30° S
• Stable and dry weather
• Trade winds and
westerlies
• Hawaiian and Azores high
• Shift with the seasons
• East and west coast
differences
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 25
Global Wind and Pressure Patterns
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In the days of sailing ships, which pattern of navigation made the
most sense, considering prevailing wind directions?
a. United States to Africa to England back to the United States
b. United States to England to Africa back to the United States
c. United States to England back to the United States
d. United States to Africa back to the United States
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 26
Global Wind and Pressure Patterns
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Midlatitude Circulation
• Westerlies
• Between about 30° and 60°
latitude
• Polar front = boundary between cold
polar air masses and warm
subtropical air masses
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 27
Global Wind and Pressure Patterns
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Midlatitude Circulation
• Jet stream = Highspeed airflow in
a narrow band within the upper-air
westerlies and along certain other
global latitude zones at high
altitudes
• Polar-front jet stream
• Shifts equatorward in the
winter
• Subtropical Jet stream
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 28
Global Wind and Pressure Patterns
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What a Geographer Sees
• Air travel and Jet Streams
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If an airplane flying in the center of this subtropical jet stream travels
east at 1000 km/hr (621 mi/hr), how fast will the same airplane go,
with the same fuel expenditure, when it travels west in the jet stream
on its return flight?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 29
Global Wind and Pressure Patterns
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Jet stream disturbance
• Rossby waves
• Baroclinic instability
• Zonal flow (west to east)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 30
Global Wind and Pressure Patterns
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Jet stream disturbance
• Growth of disturbances in the jet stream
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 31
Global Wind and Pressure Patterns
High-Latitude
Circulation
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• January and July
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 32
Global Wind and Pressure Patterns
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Global Circulation at Higher Altitudes
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 33
Global Wind and Pressure Patterns
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Global surface winds on an ideal Earth (Review)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 34
Global Wind and Pressure Patterns
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Global Air Cells: Ferrel, Hadley, or Polar (Review)?
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 35
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Local Winds
Daily Cycles of Winds
• Daily reversal of the winds as a result of uneven heating
• Sea breeze
• Land Breeze
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 36
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Local Winds
Daily Cycles of Winds
•Mountain breeze
•Valley Breeze
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 37
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Local Winds
Other Topographic Winds
• Chinook
For north–south mountain ranges
in midlatitude regions (30° to
45° latitude), dry regions will be
found on the ____ side in the
northern hemisphere and on the
____ in the southern
hemisphere.
a. east; east
b. west; west
c. east; west
d. west; east
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 38
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Local Winds
Other Topographic Winds
•Santa Ana winds
•Wildfires have already
begun in some
areas, as is apparent from
the smoke
drifting off the Southern
California coast.
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 39
Oceanic Circulation
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Ocean Currents
• A persistent, dominantly
horizontal flow of water
controlled by wind patterns
• Gyres
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What relationship do you notice with the northern hemisphere
ocean current and the pressure type typically located at 30oN ?
Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
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Slide 40
Oceanic Circulation
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Ocean Circulation and Energy Transport
• Warm surface waters in the tropics move poleward
• Thermohaline Circulation
• Cold and dense in the N. Atlantic, these waters sink, flow
equatorward, and eventually upwell to the surface at far
distant locations to cool the surrounding regions and
complete the circuit
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 41
Oceanic Circulation
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Circulation and Energy Transfer
• Energy surplus
• Energy deficit
• In order to maintain the Earth’s energy balance, absorbed
solar energy is moved from regions of excess to regions of
deficit, carried by ocean currents and atmospheric circulation
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 42
Oceanic Circulation
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Cycles in Atmospheric and Oceanic Circulation
• El Niño–Southern Oscillation (ENSO)
• La Niña
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 43
Oceanic Circulation
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Cycles in Atmospheric and Oceanic Circulation
• Climate effects of El Niño events
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.
Slide 44
Oceanic Circulation
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Cycles in Atmospheric and Oceanic Circulation
• North Atlantic Oscillation (NAO)
• Pacific Decadal Oscillation (PDO)
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Visualizing Physical Geography
Copyright © 2012 John Wiley & Sons, Inc.