Chapter 6 Atmospheric and Oceanic Circulations

Slides:



Advertisements
Similar presentations
Part 3. Distribution and Movement of Air
Advertisements

Global Average Barometric Pressure: January
The General Circulation of the Atmosphere
Unit 9: Circulation Patterns of the Atmosphere
Chapter 13 The Atmosphere in Motion
Warm Up 3/21/08 The deflection of wind due to the Coriolis effect is strongest at ____. a. the poles c. midnight b. the equator d. the midlatitudes.
Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 5 Winds and Global Circulation.
Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 5 Winds and Global Circulation Visualizing Physical Geography.
WIND Wind is movement of air caused by differences in air pressure.
The General Circulation of the Atmosphere
Atmospheric Circulation.
Chapter 19. © Air pressure weight of air above © Exerted in all directions (up, down, and sideways)
Outline Further Reading: Chapter 07 of the text book - Surface Winds on an Ideal Earth - Subtropical High-Pressure Belts - Wind and Pressure Features at.
Robert W. Christopherson Charlie Thomsen Chapter 6 Atmospheric and Oceanic Circulations.
Chapter 5: Atmospheric Pressure and Wind
Robert W. Christopherson Tim Schultz Chapter 6 Atmospheric and Oceanic Circulations.
Winds and Global Circulation
AIR PRESSURE FORCES AND WIND. HL km Pressure Gradient Force= 2.4 kPa / 600 km = 0.4 kPa / 100 km Definition: The difference in.
Atmospheric Circulation
Class 3b: Winds (global and local)
ATMOSPHERIC CIRCULATION. Atmospheric and Oceanic Circulation Wind Essentials Driving Forces Within the Atmosphere Atmospheric Patterns of Motion Oceanic.
Chapter 4 Atmospheric and Oceanic Circulation
Atmospheric Pressure and Wind. Atmospheric pressure: –force exerted by a column of air per unit area –Normal atmospheric pressure at sea level = 1013.
Atmospheric Circulations Meteorology 10 - Weather and Climate Fall 2008 CHAPTER 7 FOCUS: air circulation patterns on Earth.
Air Pressure and Winds Chapter 6. Mercury Barometer.
Atmospheric Pressure and Wind
UPPER-LEVEL WINDS Atmospheric pressure, temperature and winds at surface.
Chapter 7: Atmospheric Circulations
Winds and the Global Circulation System
GEOG 1112: Weather and Climate
Chapter 4 Atmospheric and Oceanic Circulation
Chapter 7: Atmospheric circulations Scales of atmospheric motions Scales of atmospheric motions Eddies - big and small Eddies - big and small Local wind.
Global-scale Winds Courtesy: U. of Alaska General Circulation > Global wind systems General circulation 1-cell, 3-cell models, comparison to.
Subtropical High-pressure Cells Westerlies Bermuda high Azores high Figure 6.14.
UNIT 3: Earth-Sun Relationships
Chapter 7 Circulation of the Atmosphere A Synoptic-scale Event.
The Atmosphere in Motion Chapter 18
Robert W. Christopherson Charlie Thomsen Chapter 6 Atmospheric and Oceanic Circulations.
Chapter 6 Atmospheric and Oceanic Circulations
Lecture 14 4 February 2005 Atmospheric and Oceanic Circulations (continued) Chapter 6.
A2 Module 4: Global Change
Lecture 14 7 February 2005 Atmospheric and Oceanic Circulations (continued) Chapter 6.
Chapter 7: Atmospheric Circulations Scales of atmospheric motion Eddies of different sizes  Microscale- chimney smoke, leaves in a corner of a building.
CIRCULATION OF THE ATMOSPHERE
Fundamentals of Physical Geography 1e
© 2007, John Wiley and Sons, Inc. Physical Geography by Alan Arbogast Chapter 6 Atmospheric Pressure, Wind, & Global Circulation Lawrence McGlinn Department.
Air Pressure & Wind Chapter 19 “The Atmosphere in Motion”
Chapter 4 Atmospheric and Oceanic Circulation. Atmospheric & Oceanic Circulation Major things you need to know: What causes wind to happen Global pressure.
MET 10 1 The General Circulation of the Atmosphere.
Global Circulation and World Climates Weather vs. Climate Weather vs. Climate Climate Controls Climate Controls Idealized Global Circulation Model Idealized.
Chapter 5 Atmospheric Pressure and Wind
PLANETARY WIND SYSTEM.
The Atmosphere in Motion
Atmospheric Circulation. The Earth’s energy is partly redistributed by atmospheric circulation. 1.Factors in the Cirulation of Air include; Pressure Gradient.
Chapter 4 © Oxford University Press, All rights reserved. 1 CHAPTER 4 ATMOSPHERIC CIRCULATION.
Department of Training AUXWEA CHAPTER FOUR WINDS AND EFFECTS OF EARTH’S ROTATION prepared by Weather Branch Copyright  2004 U.S. Coast Guard Auxiliary.
Atmospheric Pressure Ch The atmosphere has weight (14.7 lb/sq in.) 2.We don’t notice b/c we have air and water inside us (blood, tissue, and cells)
19 Chapter 19 Air Pressure and Wind. Air Pressure Defined 19.1 Understanding Air Pressure  Air pressure is the pressure exerted by the weight of air.
Class #17 Monday, February 16, Class #17: Monday, February 16 Surface pressure and winds Vertical motions Jet streams aloft.
PRESSURE & WIND, GENERAL CIRCULATION, JET STREAMS.
© 2014 Pearson Education, Inc. Chapter 2 Lecture McKnight's Physical Geography 11e Lectures Chapter 5 Atmospheric Pressure and Wind © 2014 Pearson Education,
Chapter 19: The Atmosphere in Motion
Ch 19: Atmosphere in Motion (aka: the Wind Chapter)
1. What does “stability” mean in the atmosphere. 2
General Circulation of the Atmosphere
Elevation (meters) Air Pressure (percent of sea level)
Global Average Barometric Pressure: January
PRESSURE & WIND, GENERAL CIRCULATION, JET STREAMS
Atmospheric Circulation
Presentation transcript:

Chapter 6 Atmospheric and Oceanic Circulations Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen

Atmospheric and Oceanic Circulations Wind Essentials   Driving Forces Within the Atmosphere   Atmospheric Patterns of Motion   Oceanic Currents  

Wind Essentials Air Pressure and Its Measurement Mercury barometer Aneroid barometer Wind: Description and Measurement   Wind Anemometer Wind vane Global Winds  

Barometers Figure 6.2

Air Pressure Readings Figure 6.3

Wind Vane and Anemometer Figure 6.4

Wind Portrait of the Pacific Ocean Figure 6.6

Driving Forces Within the Atmosphere Gravity Pressure Gradient Force   Coriolis Force   Friction Force  

Pressure Gradient Figure 6.7

Pressure + Coriolis + Friction Figure 6.8

Coriolis Force Figure 6.9

500 mb Pressure Map Figure 6.10

Atmospheric Patterns of Motion Primary High-Pressure and Low-Pressure Areas   Upper Atmospheric Circulation   Local Winds   Monsoonal Winds  

Global Barometric Pressure Figure 6.11

Global Barometric Pressure Figure 6.11

Primary High-Pressure and Low-Pressure Areas Equatorial low-pressure trough Polar high-pressure cells Subtropical high-pressure cells Subpolar low-pressure cells

Equatorial Low-pressure Trough Intertropical convergence zone (ITCZ) Trade winds

Polar High-pressure Cells Polar easterlies Antarctic high

Subtropical High-pressure Cells Westerlies Bermuda high Azores high Pacific high Figure 6.14

Subpolar Low-pressure Cells Aleutian low Icelandic low Polar front

General Atmospheric Circulation Figure 6.13

General Atmospheric Circulation Figure 6.13

Constant Isobaric Surface Figure 6.16

Upper Atmospheric Circulation Rossby waves Jet stream

Rossby Waves Figure 6.17

Jet Streams Figure 6.18

Local Winds Land-sea breezes Mountain-valley breezes Katabatic winds

Land-Sea Breezes Figure 6.19

Mountain-Valley breeze Figure 6.20

Monsoonal Winds Figure 6.21

Oceanic Currents Surface Currents   Deep Currents  

Major Ocean Currents Figure 6.22

Deep Currents Figure 6.23

Geosystems 5e An Introduction to Physical Geography End of Chapter 6 Geosystems 5e An Introduction to Physical Geography Robert W. Christopherson Charlie Thomsen