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Title: http:www'srh'noaa'govsrhjetstreamsynopticwind'htm


1
Wind, Air masses, and Fronts
Clare 102 Weather and Climate Change Spring 2009
2
Key question can we predict weather?
Never, no matter what may be the progress of
science, will honest scientists who care for
their reputation venture to predict weather.
Francois Arago, 1786 -1853
We shall know more and more by degrees.
Robert FitzRoy, 1850s
3
Heres what it takes
  • Vilhelm Bjerknes - first modern scientific
    forecaster. In a 1904 publication he argued that
    weather prediction requires
  • sufficiently accurate knowledge of the current
    state of the atmosphere
  • sufficiently accurate knowledge of the laws
    according to which one state of the atmosphere
    develops from another.
  • Cox. Stormwatchers. 154

Critics complained that his method of forecasting
storms took longer than just waiting to see how
the storms actually developed. What he needed
was ?
4
Computing power
About 1 calculation per second
About 5,000 calculations per second
1.7 quadrillion calculations per second
http//campus.udayton.edu/hume/Computers/The20Ea
1.jpg
http//strongtowersoftware.com/eniac1.gif
http//en.wikipedia.org/wiki/FileRoadrunner_super
computer_HiRes.jpg
5
A brief history of weather prediction
  • Aristotle (384-322 B. C.) Meteorologica. He
    discussed winds, earthquakes (which he thought
    were caused by underground winds), thunder,
    lightning, rainbows, and meteors, comets, and the
    Milky Way which he thought were atmospheric
    phenomena). http//www.ucmp.berkeley.edu/history
    /aristotle.html
  • Jacques Charles and others (starting 1783)
    Charles invented the gas balloon made the first
    atmospheric ascent with thermometer and
    barometer. Hydrometer added later. Cox.
    Stormwathers. 21
  • Elias Loomis (1837) attempted to reconstruct
    the wind speeds in a tornado. Collected data on
    individual storms from dozens of stations. First
    synoptic weather maps. Cox. Stormwathers.
    41-49

6
A brief history (2)
  • Joseph Henry (1849) as Secretary of the
    Smithsonian he established a telegraph network of
    weather stations. Permitted first
    near-simultaneous tracking of storms.Cox.
    Stormwathers. 47
  • Robert FitzRoy (1850s) first national weather
    forecasts (he coined the phrase). Beginning
    in Aug. 1861 his forecasts featured in several
    London newspapers. Optimistic about meteorology
    (We shall know more and more by degrees) Cox.
    Stormwatchers. 80
  • William Ferrel (1858) first complete
    mathematical description of global circulation
    patterns.

7
Ferrels paper
8
A brief history (3)
  • Francis Capen (1863) - tried to convince Pres.
    Lincoln of the value of meteorology for wartime
    strategies. Lincoln commented, It seems to me
    that Mr. Capen knows nothing about weather He
    told me three days ago that it would not rain
    again till the 30th of April or the 1st of May.
    It is raining now and has been for 10 hours. I
    can not spare any more time for Mr. Capen. Cox.
    Stormwatchers. 63
  • Cleveland Abbe (1870) established first U. S.
    network of weather stations, under Army Signal
    Corps. Transferred to U. S. D. A. renamed the
    Weather Bureau (1891) Cox. Stormwatchers.
    Chapt. 12

9
A brief history (4)
  • Vilhelm Bjerknes (1904) - first fully scientific
    approach to weather forecasting. Applied
    Newtonian physics to atmospheric science.
    Founded the Bergen (Norway) school of
    meteorology. Critics complained that his method
    of forecasting storms took longer than the
    weather itself. Cox. Stormwatchers. 154
  • Jacob Bjerknes (1918-1960s) Vilhelm s son.
    Theories of fronts and life cycle of cyclones
    (in his 20s). Foundation of all modern weather
    forecasting. First clear explanation of El Nino
    (1969, age 71) Cox. Stormwatchers. Chapt. 12

10
Who to study
  • Know
  • Be aware of
  • Appreciate

11
Air pressure and isobars
  • iso means equal
  • bar means pressure
  • So isobar lines join places with air

12
Isobars show high and low pressure systems
Left Ahrens. Meteorology Today. Fig.
8.16 Right Lutgens Tarbuck,. The Atmosphere.
Fig. 11-4a
13
Pressure gradient force
Like this
http//www.eoearth.org/article/Wind
http//www.deskpicture.com/DPs/Sports/Skier.jpg
14
The Coriolis Effect
http//www.srh.noaa.gov/srh/jetstream/synoptic/win
d.htm
In the Northern Hemisphere, objects in motion are
deflected
Originally suggested by Hadley (1735)
Mathematics worked out by Ferrel (1858)
15
Try it on a globe
Try it N -gt S or S -gt N The deflection is always
(in the Northern hemisphere)
http//luna.tau.ac.il/tomer/staff/morris/NewSite/
Chapter3/Coriolis_Effect.htm
16
East-west motions are also deflected
Ahrens. Meteorology Today. 8th ed. Fig. 8.22
The deflection is greatest at the poles and zero
at the equator
17
Why do winds spiral into low pressure zones?
  • Atmospheric circulation involved a of forces
  • The net force causes a
  • circulation pattern around a low pressure
    system, called cyclonic flow

Ahrens. Meteorology Today. Fig. 8.26a
18
Cyclones and Anticyclones
Ahrens. Meteorology Today. Fig. 8.26
19
Hurricanes other tropical storms are cyclones
which way do they spin?
http//www1.ncdc.noaa.gov/pub/data/nexradviewer/ka
trina/klix-landfall-anim_med.gif
20
Converging air masses
  • Air moves into a Low pressure zone (much as
    water moves toward a sink drain)
  • Air cant just pile up there, so it is
  • As the air rises, it . Often it
  • This is why Low pressure often leads to

http//www.srh.noaa.gov/srh/jetstream/synoptic/win
d.htm
21
Diverging air masses
  • Air moves way from a High pressure zone (much as
    water flows off of a hill)
  • Air from above must sink to replace it. As the
    air sinks, it
  • Warmer air can support more evaporation, so its
    relative humidity
  • This is why High pressure often leads to

http//www.srh.noaa.gov/srh/jetstream/synoptic/win
d.htm
22
Fronts
  • a line of contact between
  • Vilhelm Bjerknes (1920) used military language to
    describe frontsThe warm is victorious to the
    east of centre. The cold, which is pressed hard,
    escapes to the west, in order suddenly to make a
    sharp turn towards the south, and attacks the
    warm air in the flank it penetrates under it as
    cold West wind. Cox. Stormwatchers. 166-7

23
Fronts seen from above
http//www.physicalgeography.net/fundamentals/7s.h
tml
24
Anatomy of a warm front
http//www.physicalgeography.net/fundamentals/7r.h
tml
25
Weather associated with warm fronts
http//www.physicalgeography.net/fundamentals/7r.h
tml
26
Anatomy of a cold front
http//www.physicalgeography.net/fundamentals/7r.h
tml
27
Weather associated with cold fronts
http//www.physicalgeography.net/fundamentals/7r.h
tml
28
Sometimes fronts collide
http//www.physicalgeography.net/fundamentals/7r.h
tml
29
What caused this weather?
Source SBU Weather Station
30
What caused this weather?
Source SBU Weather Station
31
What caused this weather?
Source SBU Weather Station
32
Friday, 26 December 2008
33
Saturday, 27 December 2008
34
Sunday, 28 December 2008
35
Monday, 29 December 2008
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