Notes: Global Wind Patterns 11/19 p. 62

Slides:



Advertisements
Similar presentations
Do Now – In Binders Describe how wind is created. What is the relationship between density and pressure? What happens to air pressure as I hike up a mountain?
Advertisements

Bell work Write a poem about moving air. The poem should include an explanation of why air moves.
What is wind?.
Global Winds Winds that blow steadily from specific directions over long distances.
Global and Local Winds Chapter 16 Section 3.
Global and Local Winds.
Global and Local Winds.
Chapter 22 Section 3 Handout
Aim: What are some of Earth’s wind patterns? I. Winds and Pressure Belts A. Convection cell – when air circulates by rising in one place and sinking at.
WIND Wind is movement of air caused by differences in air pressure.
Global Wind Patterns and Weather & Weather Basic
Atmospheric Pressure and Wind
Do you know your Winds? Raise your hand and no foldables!
Wind Causes of Wind.
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 15 Global Winds and Local Winds.
Global and Local Winds.
Key Ideas Explain the Coriolis effect.
J. Shevlin April 11, 2012 Eastern Illinois University.
Global Wind Patterns. Remember… When we talked about air pressure we said that cold air sinks and warm air rises. This movement causes air to move.
What causes wind? The uneven heating of Earth’s surface by the sun causes temperature differences in air. Warm air rises, creating areas of low pressure.
Global Wind Patterns.
Chapter 4 Section 3 Air Movement
Wind Why air moves Pressure Belts Moving air Wind is created by differences in air pressure  The greater the difference, the faster the wind moves  The.
Winds. Wind is the horizontal movement of air from an area of high pressure to an area of low pressure. All winds are caused by differences in air pressure.
Please take out your Skills WS and check your work with a desk partner. Be ready to ask any questions on 15.2.
22.3 Atmospheric Circulation. It all starts with unequal heating of Earth that cause differences in pressure Warm air is less dense, rises and creates.
15-3 Atmospheric Pressure and Winds pgs IN: What causes winds?
Global Winds Chapter17. Formation of Wind warmer air = less dense = rising air warmer air = less dense = rising air (lower pressure) colder air = more.
C. 22 Section 3 Atmospheric Circulation Air near Earth’s surface generally flows from the poles toward the equator.
Global and Local Winds. Why Air Moves Winds blow from areas of high pressure to areas of low pressure. The greater the pressure difference, the faster.
Air Pressure/Winds Air Pressure –weight of the atmosphere pushing down on Earth (we don’t feel it because air is pushing on all sides, not just down from.
The Ozone Problem  O3 O3 O3 O3.  CFC’s Chlorofluorocarbons Chlorofluorocarbons  Methyl bromide  Results More UV radiation More UV radiation Growth.
Global Winds. Air Movement Wind is the movement of air caused by differences in air pressure Wind is the movement of air caused by differences in air.
Air rises at the equator and sinks at the poles The equator receives more direct sun than other areas so the air is less dense and rises to create low.
Heating the Earth Weather is the daily conditions of the atmosphere The factors that interact to cause weather are heat energy, air pressure, winds, and.
Atmospheric Circulation The Coriolis Effect, Winds and Breezes Chapter 22.3.
Wind the movement of air by differences in air pressure Air moves from areas of high pressure to areas of low pressure Air moves in small circular patterns.
Global and Local Winds.
Topic: Global Winds PSSA: C / S8.D.2.1. Objective: TLW identify the basic characteristics of each of the major global wind belts and their effect.
Global and Local Winds. What is Wind? The movement of air caused by differences in air pressure. These differences in air pressure are generally caused.
Bell work Write a poem about moving air. The poem should include an explanation of why air moves.
Global winds.
Major global wind belts Trade winds Polar easterlies
What is wind?.
Global Winds Eric Angat Teacher.
Global Winds What roles do composition, structure, and properties play in our atmosphere?
Global Winds.
Global and Local Winds.
Global and Local Winds Chapter 16 Section 3.
Handout (green) Atmospheric Circulation
Atmospheric Circulation
Global Winds.
Global Winds Earth Science Fall 2017.
Global and Local Winds.
Global and Local Winds.
Global and Local Winds Chapter 16 Section 3.
Global & Local Winds.
15.3 Global Winds and Local Winds
Global Winds Chapter17.
Global and Local Winds.
Wind Causes of Wind.
Wind Causes of Wind.
Global and Local Winds.
Wind circulation through the atmosphere
Global Winds and Local Winds
Wind Causes of Wind.
Global Winds and Local Winds
Global and Local Winds.
Warm up What is the difference between conduction, convection, and radiation? What is wind?
Global and Local Winds.
Presentation transcript:

Notes: Global Wind Patterns 11/19 p. 62

Notes: Global Wind Pattern 11/19 p. 62 Pressure differences in atmosphere cause movement of air worldwide. Air near surface flows from poles to equator, because it moves from high pressure (where cold air sinks) to low pressure areas (where warm air rises).

Notes: Global Wind Pattern 11/19 p. 62 Pressure differences in atmosphere cause movement of air worldwide. Air near surface flows from poles to equator, because it moves from high pressure (where cold air sinks) to low pressure areas (where warm air rises). Each hemisphere has three cells of air (air moving in circular direction) that circulate through the entire depth of the troposphere. These are the Hadley cell, Ferrel cell and Polar cell.

Each hemisphere has three cells of air (air moving in circular direction) that circulate through the entire depth of the troposphere. These are the Hadley cell, Ferrel cell and Polar cell. Jet streams- high speed winds blow in upper troposphere and lower stratosphere. There is a polar and a subtropical jet stream.

Glue to p. 63 sideways (don’t cut it) Each hemisphere has three cells of air (air moving in circular direction) that circulate through the entire depth of the troposphere. These are the Hadley cell, Ferrel cell and Polar cell. Jet streams- high speed winds blow in upper troposphere and lower stratosphere. There is a polar and a subtropical jet stream. Air moves in curved direction due to Earth’s Rotation (the Coriolis Effect). Glue to p. 63 sideways (don’t cut it)

300 - 600 latitude 300 - 600 latitude

300 - 600 latitude Horse latitudes=300 latitude= weak winds Horse latitudes=300 latitude= weak winds 300 - 600 latitude

Horse latitudes=300 latitude= weak winds *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s 300 - 600 latitude Horse latitudes=300 latitude= weak winds 00-300 latitude * 00-300 latitude Horse latitudes=300 latitude= weak winds 300 - 600 latitude

Horse latitudes=300 latitude= weak winds *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s 300 - 600 latitude Horse latitudes=300 latitude= weak winds 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Horse latitudes=300 latitude= weak winds 300 - 600 latitude

Horse latitudes=300 latitude= weak winds *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s Low Pressure 300 - 600 latitude Horse latitudes=300 latitude= weak winds 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Horse latitudes=300 latitude= weak winds 300 - 600 latitude Low Pressure

Horse latitudes=300 latitude= weak winds *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s Low Pressure 300 - 600 latitude High Pressure Horse latitudes=300 latitude= weak winds 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Horse latitudes=300 latitude= weak winds High Pressure 300 - 600 latitude Low Pressure

Horse latitudes=300 latitude= weak winds *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s Polar Cells= smallest and weakest cells Low Pressure 300 - 600 latitude High Pressure Horse latitudes=300 latitude= weak winds 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Horse latitudes=300 latitude= weak winds High Pressure 300 - 600 latitude Low Pressure Polar Cells

Horse latitudes=300 latitude= weak winds *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s Polar Cells= smallest and weakest cells Low Pressure Ferrel Cells move in opposite direction as other cells 300 - 600 latitude High Pressure Horse latitudes=300 latitude= weak winds 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Horse latitudes=300 latitude= weak winds High Pressure 300 - 600 latitude Ferrel Cells Low Pressure Polar Cells

Horse latitudes=300 latitude= weak winds Polar Cells= smallest and weakest cells *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s Low Pressure Ferrel Cells move in opposite direction as other cells 300 - 600 latitude High Pressure Horse latitudes=300 latitude= weak winds Hadley Cells= largest cells 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Hadley Cells Horse latitudes=300 latitude= weak winds High Pressure 300 - 600 latitude Ferrel Cells Low Pressure Polar Cells

Horse latitudes=300 latitude= weak winds Polar Cells= smallest and weakest cells *Trade Winds used by trade ships sailing from Europe to Americas in 1700-1800s Low Pressure Ferrel Cells move in opposite direction as other cells 300 - 600 latitude High Pressure Horse latitudes=300 latitude= weak winds Hadley Cells= largest cells 00-300 latitude Intertropical Convergence Zone = “Doldrums” at equator= weak winds Low Pressure 00-300 latitude Hadley Cells Horse latitudes=300 latitude= weak winds High Pressure 300 - 600 latitude Ferrel Cells Low Pressure Polar Cells