Chapter 5 Atmospheric Pressure and Wind - PowerPoint PPT Presentation

Loading...

PPT – Chapter 5 Atmospheric Pressure and Wind PowerPoint presentation | free to download - id: 735e57-NzQ0Z



Loading


The Adobe Flash plugin is needed to view this content

Get the plugin now

View by Category
About This Presentation
Title:

Chapter 5 Atmospheric Pressure and Wind

Description:

Chapter 5 Atmospheric Pressure and Wind Physical Geography A Landscape Appreciation, 9/e Animation Edition Victoria Alapo, Instructor Geog 1150 – PowerPoint PPT presentation

Number of Views:110
Avg rating:3.0/5.0
Slides: 40
Provided by: Ging161
Category:

less

Write a Comment
User Comments (0)
Transcript and Presenter's Notes

Title: Chapter 5 Atmospheric Pressure and Wind


1
Chapter 5 Atmospheric Pressure and Wind
  • Physical Geography
  • A Landscape Appreciation, 9/e
  • Animation Edition

Victoria Alapo, Instructor Geog 1150
2
Atmospheric Pressure and Wind
  • Atmospheric Processes
  • The Nature of Wind
  • General Circulation of the Atmosphere
  • Modifications of General Circulation
  • Localized Wind Systems

3
Atmospheric Processes
  • Atmospheric pressure is the force exerted by gas
    molecules on some area of the Earths surface,
    including physical bodies. At sea level, it is
    14.7 pounds/sq. inch. See Fig 5-2, page 108.
  • We dont feel it because we are at equilibrium
    with nature the pressure inside of us, is the
    same as that outside. We only notice it when we
    leave sea level.

4
Atmospheric Processes
  • Pressure, Density, and Temperature
  • While pressure is directly related to density
    (proportional), it is inversely related to
    temperature.
  • So, the higher the density, the higher the
    pressure, and vice-versa. So solids are more
    dense than gases (gases spread).
  • The lower the temperature of air or water
    (colder), the higher the pressure and the higher
    the temperature (hotter), the lower the pressure.
    This is because things expand as they get warmer
    and vice-versa. Sea floors have the highest
    pressures (why?).

5
Pressure and Density
6
Mapping Pressure with Isobars
Isolines all have the same concept. However,
unlike contours that stay the same, pressure
lines can change with atmospheric
conditions. Here, a ridge is an elongated
area of high pressure and a trough is an
elongated area of low pressure. Atmos. pressure
is measured with a Barometer. Millbars (mb)
are now the preferred unit of measurement
(metric). At sea level, it is 1013.25 mb.
7
The Nature of Wind
  • Direction of Movement caused by
  • Pressure Gradient
  • Coriolis Effect (see chapter 3)
  • Friction
  • Wind Speed
  • Cyclones and Anticyclones

8
Pressure Gradient
Wind is air in motion. And air always moves
from an area of high pressure to an area of low
pressure. This is what causes wind. Thats
why Chapter 5 is titled Air Pressure Wind
the 2 go together. It is the change in
pressure that causes wind. Also, thats why
people can get sucked out of a pressurized plane
(high to low pressure).
9
Wind Speed
Same concept as an isoline lines close together
means steep pressure or fast, far apart lines
means gentle pressure or slow. Pressure
gradient is the spacing of the isobars. Note
the direction of flow. See pg 115 wind speeds
in the U.S. and pg 114 for definition of a knot.
10
Coriolis Effect
11
Friction
Friction is caused by trees, buildings,
mountains, hills, etc anything in the way. It
slows air down changes its direction, causing
more turbulence (see figure on right).
12
Cyclones and Anticyclones
Cyclones are low pressure centers (air flows into
them) e.g. hurricanes, tornadoes. Also assoc.
with clouds (air condenses as it rises). See
figure on right. Anticyclones are the opposite
air flows out and are assoc. with clear weather.
13
Circulation Patterns
14
Circulation Patterns
15
General Circulationof the Atmosphere
  • Hadley Cells giant convection systems close to
    the equator. As the warm air rises to about
    50,000 ft, it cools and part of the air moves
    towards the poles, where it descends at about 30
    degrees N and S to become the sub-tropical high
    pressure winds (STHs). The other part moves back
    to the equator to repeat the process. See next
    slide.

16
Hadley Cells
17
Components of General Surface Circulation
  • Subtropical Highs
  • Trade Winds
  • Intertropical Convergence Zone
  • The Westerlies
  • Polar Highs
  • Polar Easterlies
  • Subpolar Lows/Polar Front

18
General SurfaceCirculation
19
Subtropical Highs (STHs)
Formed by the high pressure created from
descending air of Hadley Cells. They are giant
anticyclones (characteristic?) They are
persistent, and are found about 30 degrees N
S. Also called the horse latitudes (16th 17th
cent.) STHs are the source of Trade Winds
Westerlies.
20
Subtropical Highs
Responsible for the worlds greatest deserts. Dry
conditions caused by no uplift of air due to high
pressure.
21
Trade Winds
Major wind systems of the tropics, btw latitudes
25 degrees N S. Dominates the earth more than
any other wind system. They are Easterly (blow
from East). Thats how winds are named
(continued on next page).
22
General SurfaceCirculation
Trade winds are the most reliable of ALL winds
their direction speed is extremely consistent
(whether it be summer, winter, day or night).
There is one exception (discussed later). Hence
trade winds, mean winds of commerce. 16th
century sailors found that it was the fastest
most reliable route from Europe to America.
23
Intertropical Convergence Zone (ITCZ)
This is where the Trade Winds converge. Known
for low pressure a lot of storms. Also called
the doldrums (calm air) even though its a
zone of convergence, horizontal air flow is weak.
24
The Westerlies
Why are they called Westerlies? Found btw 30
to 60 degrees N S, and originate from the STHs.
25
Jet Streams
Jet streams form the BOUNDARIES of the
Westerlies. There are 2 types polar and
subtropical. They are high speed winds, and 60
knots is the minimum to qualify. See Fig 5-24,
pg 122. Whenever the paths of jet streams change
or meander, theyre called Rossby Waves. Fig
5-25, pg 123.
26
General SurfaceCirculation
  • Polar Highs
  • Polar Easterlies
  • Subpolar Lows/Polar Front

27
General Surface Circulation
  • Polar Highs located over both the N S poles.
    Air movement is mainly anticyclonic (divergent,
    high pressure cold air), hence, polar highs.
    The weather is usually nice or rather, clear,
    and this leads to them becoming polar deserts.
    The Antarctic high is more persistent than the
    Arctic high (thats why its colder in the
    Antarctic).
  • Polar Easterlies located btw the polar highs
    latitude 60 degrees N S. The move from the
    east, and are very dry. See next slide.
  • Sub-Polar Lows/ Polar Front btw 50 and 60
    degrees N S, and its a zone a low pressure.
    Usually contains a polar front (where the cold
    polar easterlies and the warmer westerlies meet).
    This results in storms gale-force winds. See
    Fig. 5-28, pg 125.

28
General Surface Circulation
29
Modifications of General Circulation
  • Seasonal Variations in Latitude
  • Monsoons

30
Seasonal Variationsin Latitude
31
MonsoonsMonsoon Areas of the World
32
South Asian Monsoon
33
Localized Wind Systems
  • Sea and Land Breezes
  • Valley and Mountain Breezes
  • Katabatic Winds
  • Foehn/Chinook Winds

34
Sea and Land Breezes
35
Valley Breezes
36
Mountain Breezes
37
Chinook Winds
38
El Niño and La Niña
  • El Niño Conditions in Pacific Ocean
  • Related Weather Events (next slide)
  • La Niña

39
El Niño and Weather Events
About PowerShow.com