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Chapter 7: Atmospheric Circulations

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Chapter 7: Atmospheric Circulations Scales of atmospheric motions Eddies - big and small Local wind systems Global winds Global wind patterns and the oceans – PowerPoint PPT presentation

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Title: Chapter 7: Atmospheric Circulations


1
Chapter 7 Atmospheric Circulations
  • Scales of atmospheric motions
  • Eddies - big and small
  • Local wind systems
  • Global winds
  • Global wind patterns
  • and the oceans

2
Scales of Atmospheric Motions
  • Microscale meters - kilometers
  • Mesoscale km a few hundred km
  • synoptic scale a few hundred km a few thousand
    km
  • planetary scale a few thousand km and larger
  • Q what is the scale of atmospheric boundary
    layer turbulence?
  • a) microscale, b) mesoscale, c) synoptic
    scale
  • Q what is the scale of weather fronts?
  • a) microscale, b) mesoscale, c) synoptic
    scale
  • Q what is the scale of lake breeze over the
    Great Lakes
  • a) microscale, b) mesoscale, c) synoptic
    scale

3

4
Eddies - Big and Small
  • eddy or turbulent eddy caused by convection
    (heating or cooling), wind shear (or near surface
    wind), or waves
  • Rotor caused by mountain waves
  • wind shear change of
  • wind speed or direction
  • with height

5
  • Clear-air turbulence caused by wind shear
    important for aviation

Billow clouds caused by mountain waves in a wind
shear zone
Q what could cause bumpy aircraft flight in the
upper troposphere? a) clear-air turbulence,
b) rotor, c) billow clouds
6
Local Wind Systems
  • Thermal Circulations warm air rises and cool air
    sinks
  • Warm air leads to H in the air (i,e, pushing
    isobar up)
  • Air moves from H to L
  • increases surface pressure (i.e., pushing
    near-surface isobar up) over cool place
  • Leads to circulation from cool place to warm
    place near surface
  • Pay attention to the change of isobars with
    height

7
Sea and Land Breezes
  • sea breeze from sea to land
  • land breeze land to sea
  • sea breeze front clouds
  • Florida sea breezes
  • Sea and land breezes also occur near the shores
    of large lakes, such as the Great Lakes
  • Pay attention to the change of isobars with
    height
  • Q which is stronger in general?
  • a) sea breeze, b) land breeze,
  • c) the same

8

Q When do you expect to see the thunderstorm in
summer in Florida? a)
10am, b) noon, c) 3pm, d) 6pm
Q For the prevailing northeasterly wind over
southern Florida, where does the strongest sea
breeze occur in general ? a) Eastern coast of
southern Florida, b) western coast, c) central
part
9
height
Q7 given the isobars as left, what is the
near-surface wind direction? a) from A to B b)
from B to A Q8 During the day, if you stand on
beach, what would be the wind direction due to
sea breeze? a) from sea to beach b) from land to
sea
A B
10
Seasonally Changing Winds - the Monsoon
  • Monsoon wind system change with season
  • India and eastern Asian monsoon
  • Global monsoons
  • Q What are the differences and similarities
    between monsoon and sea/land breeze?
  • A Monsoon system is much greater in
    geographic area changes with season sea/land
    breeze changes with diurnal cycle both due to
    horizontal temperature difference

11
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12
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13

North American monsoon Q Coriolis force is
important for monsoon circulation. Is it
as important for sea breeze as for monsoon? a)
yes b) no Q Still, is Coriolis force important
for sea breeze? a) yes b) no
14
Mountain and Valley Breezes
  • valley breeze daytime from valley to top
  • mountain breeze nighttime from top to valley
  • The nighttime mountain breeze is sometimes
    calledgravity winds or drainage winds, because
    gravitycauses the cold air to drain downhill.
  • Q Which is stronger in general?
  • a) valley breeze, b) mountain breeze, c) the
    same

15
Katabatic Winds
  • Strong drainage wind from cold elevated plateau
    down steep slope and/or narrow channel
  • Katabatic winds are quite fierce in parts of
    Antarctica, with hurricane-force wind speeds.
  • Bora a cold, gusty northeasterly wind along the
    Adriatic
  • coast in the former Yugoslavia

Q why is the air parcel temperature much warmer
at bottom of the mountain in the figure?
16
Chinook (Foehn) Winds
  • Chinook winds one type of drainage wind warm
    and dry wind down the eastern slope of the Rocky
    Mountains
  • It is called a Foehn along the leeward slopes of
    Alps.
  • Q Which wind is weakest in general?
  • a) drainage wind, b) katabatic wind, c)
    Chinook wind

17

Chinook wall cloud indicates that chinook is
coming
18
Santa Ana Winds
  • Santa Ana wind warm, dry wind from the elevated
    desert plateau down to southern California
  • compressional heating
  • Could have very strong wind
  • wildfires
  • Q which wind comes from elevated desert plateau?
  • a) Chinook wind b) Santa Ana wind
  • c) Katabatic wind d) mountain breeze
  • Q The drainage wind over the lee side of the
    Rocky Mountain is
  • a) Chinook wind b) Santa Ana wind
  • c) Katabatic wind d) mountain breeze

19
Desert Winds
  • dust and sand storms occurs over arid and
    semiarid regions
  • dust devils from surface
  • usually with a diameter of a few
  • meters and a height of lt100 m
  • Q What is the difference between tornado and
    dust devil? A Tornado is larger horizontally and
    deeper vertically from cloud base down

20
Haboob A spectacular example of duststorm caused
by thunderstorm downdraft tens of kilometers
horizontally and hundreds of meters vertically
21
Q give a phenomenon and its typical
temporal/spatial scales for each scale (micro,
meso, synoptic, global) Q What is the
direction of sea breeze? What is the formation
mechanism? Q what wind would produce clouds? a)
valley breeze, b) mountain breeze Q Indian
summer monsoon brings rainfall to India. The
winter monsoon is a) wet, b) dry Q
Suppose you are fishing in a mountain stream in
the early morning. The Wind is more likely
blowing a) upstream, b) downstream
22
General Circulation of the Atmosphere
  • cause unequal net heating of the earths surface
    and atmosphere
  • effect atmospheric circulation and ocean
    currents to transport heat from the equator to
    the poles

Fig. 2.19 on p. 46
23
Single-cell Model
  • basic assumptions no rotation
  • Originally proposed by George Hadley in England
    in the 18th Century
  • Hadley cell
  • Q Why is the single-cell model wrong? A
    Because single cell does not exist due to earths
    rotation
  • UKs Hadley Centre for Climate
  • Research is named after George Hadley.

24
Three-cell Model
  • model for a rotating earth overall realistic for
    surface fields

25
Three-cell Model
  • realistic over the tropics in winter hemisphere
  • Hadley cell doldrums subtropical
    highs
  • trade winds intertropical convergence
    zone (ITCZ)
  • Over mid- and high latitudes Ferrel cell and
    polar cell do not play major roles
  • westerlies in the upper troposphere
  • polar front
  • polar near-surface easterlies
  • Q if near-surface wind is southwesterly over NH
    midlatitudes, what is the direction of upper
    troposphere wind?
  • a) westerly, b) easterly, c) southerly,
    d) northerly

26
Average Surface Winds and Pressure The Real World
  • semipermanent highs Bermuda high Pacific high
  • Pacific high moves north in summer
  • Bermuda high moves west in summer
  • Semipermanent low Icelandic low
  • it moves north in summer
  • Siberian high in winter due to very cold air
  • Aleutian low in winter due to storm track
  • ITCZ stays in the warm hemisphere (e.g., NH in
    July)
  • There are three semipermanent highs in SH

27

28

29
The General Circulation and Precipitation Patterns
  • Most of the worlds thunderstorms are found along
    the ITCZ.
  • Low rainfall over the subtropical regions
  • Fronts and precipitation over the subpolar lows
  • Q which is correct?
  • a) desert causes subtropical high
  • b) subtropical high causes desert

30
Q Why is Los Angeles dry in summer, while
Atlanta is wet?
31
Westerly Winds and the Jet Stream
  • jet streams
  • subtropical jet stream
  • polar front jet stream

Low-level jet stream over the Central plains of
the U.S. (within 2 km above surface), bringing
moist and warm air to form nighttime
thunderstorms
32
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33

(warm) Gulf Stream (warm) Kuroshio
Current (cold) California Current (cold)
Canary Current Equatorial Current and Counter
Current in the Pacific
Global wind drives ocean current Q These ocean
circulations are consistent with wind of a)
high pressure system b) low pressure
system
Fig. 7-29, p. 193
34
Winds and Upwelling
  • Upwelling is strongest when wind is parallel to
    the coastline
  • Q Why is ocean coldest in northern California in
    the left figure?
  • A wind is parallel to the coastline upwelling
    is strongest cold deep water is brought to
    surface

35
El Niño and the Southern Oscillation
  • Q what is the El Niño? A warming, pressure
    decrease, and weakened upwelling over the central
    and eastern Pacific trade wind weakened as well
  • (cooling, pressure increase over western
    Pacific)
  • La Niña opposite
  • Q What is the Southern Oscillation (SO)? A
    oscillation of surface pressure over tropical
    western and eastern Pacific
  • ENSO El Nino and SO are closely related
  • Q What is teleconnections? A local changes
    (e.g., in sea surface temperature) affect weather
    in remote regions.
  • SST animation
  • www.esrl.noaa.gov/psd/map/clim/sst.anom.anim.year.
    html

36

Thermocline is incorrect in bottom panel
37
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38
  • ENSO is an example of a global-scale weather
    phenomenon.
  • Q What is the El Nino effect on winter weather
    in the U.S.? A Northwestern U.S. usually
    has a warmer winter, Southeast usualy has a
    wetter winter, and often Arizona has a wetter
    winter

El Nino effect
39
Other Atmosphere-Ocean Interactions
  • North Atlantic Oscillation (NAO) based on
    pressure difference between Bermuda and Iceland
  • Arctic Oscillation (AO) pressure difference
    between about 45oN and Arctic describes the same
    phenomenon in a similar way as NAO.
  • Positive (negative) phase stronger (weaker)
    zonal wind

40

Pacific Decadal Oscillation Pacific surface
temperature pattern changes every 20-30
years Over the tropical Pacific, PDO pattern is
not very different from ENSO Over midlatitude
Pacific, PDO pattern is different from
ENSO Positive (negative) phase warmer (cooler)
surface water along the west coast of North
America Amplitude is smaller than ENSO
41
Q Most U.S. is located in a) westerly wind
belt, b) easterly wind belt, c) southerly wind
belt, d) northerly wind belt Q Why do
summers along the west coast of U.S. tend to be
dry? Q What coastal wind along the west coast
of North America would produce strong upwelling?
a) northerly, b) southerly, c) easterly, d)
westerly Q What is a major El Nino? Q for the
positive phase of NAO, a) Greenland is colder and
northern Europe is milder, b) Greenland is milder
and northern Europe is colder, c) Greenland and
northern Europe are both colder, d) Greenland
and northern Europe are both milder
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