Wind Coriolis Effect (p. 516) Prevailing Winds (p. 516-519)

Slides:



Advertisements
Similar presentations
What we now know: Difference between weather and climate.
Advertisements

Weather.
Chapter 16 Section 3: Winds.
Mrs. Wharton’s Science Class
Global and Local Winds Chapter 16 Section 3.
Global and Local Winds.
Convection, Global Winds, and Jet Stream
Global and Local Winds.
WIND Wind is movement of air caused by differences in air pressure.
Wind and the Coriolis Effect
Coriolis Effect.
Prevailing Winds.
13.6 Wind and Ocean Currents Science 10. A Little Background … Atmospheric Pressure is the force of the air pressing down on the earth’s surface –Atmospheric.
Global Wind Patterns Science Lesson Objectives ► using scientific theory, describe and explain heat transfer and its consequences in both the atmosphere.
Winds
Convection in Our Atmosphere
Winds.   at home  
Atmosphere & Weather All About Winds.
Wind Causes of Wind.
“ I. What Causes Our Weather” 1. Weather-Is the present state of our atmosphere. 2. The interaction between the earth’s air, water, land and the sun causes.
Physical Geography Wind And Ocean Currents
Global and Local Winds.
Worldwide Wind and Ocean Currents Science 10. Global Warming and Cooling of Air Air is warmest at the equator and coolest at poles Air is warmest at the.
Meteorology: the study of Earth’s atmosphere Meteor – In ancient Greek – meant “High in the air” Current meanings still apply Meteor – astronomical entity.
Guided Notes for Weather Systems
Air Movement Chapter 4 – Section 3 Pages
Winds Chapter 2, Section 3 p What causes wind? Wind: The horizontal movement of air from an area of high pressure to an area of lower pressure.
Global Wind Patterns.
Welcome to Class Define radiation, convection, and conduction.
SCIENCE 10 Wind and Ocean Currents. A Little Background … Atmospheric Pressure is the pressure the air exerts as gravity pulls it towards the earth’s.
Chapter 15: Atmosphere Section 3: Air movement Study Guide.
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.
Energy Transfer in the Atmosphere. A. Some energy from the Sun is reflected back into space, some is absorbed by the atmospshere, and some is absorbed.
Chapter 2 Weather Factors Section 3 Winds. What causes wind? Wind: The horizontal movement of air from an area of high pressure to an area of lower pressure.
Wind Read each slide carefully. Make sure pay attention to any diagrams. Complete the questions when finished! 3 3 Air Movement.
Air Currents in the Atmosphere. Why is it warmer at the equator?
Wind John Harris - Head of Geography - Radley College - UK
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.
Atmospheric movements We learned that energy is transferred from the Sun to the Earth creating convection currents. But, what type of currents???
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.
WIND Movement of air in the atmosphere.. Remember Convection Principles Solar energy strikes the _____________________, heating the air, land and water.
Global Wind Patterns. What is Wind? Wind is the movement of air from an area of higher pressure to an area of lower pressure. Warmer air expands, becoming.
Wind and the Ocean. Wind Currents of air Develop when two adjacent bodies of air have different densities. Denser air sinks, pushing less dense air upward.
Heating of the Earth. Temperature Layers of the Atmosphere.
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.
Section 1.2 The Causes of Weather
Welcome to Class Define radiation, convection, and conduction.
Meteorology Regents Earth Science St. Martin de Porres School Mrs. Canfield.
TOC: Winds I STARTER: Think back to the demos, does air move from low pressure to high pressure or the other way around?? Explain…..
Fact Statements.  Surface currents are mainly caused by prevailing winds.  Their flow is controlled by the winds, Earth’s rotation and location of the.
Global Wind Belts & the Jet Stream
Local and Global Winds. Wind Wind is created by the unequal warming of the Earth (convection currents) Differences in atmospheric pressure cause the movement.
Global and Local Winds.
Wind John Harris - Head of Geography - Radley College - UK
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.
Warm up  Your warm up is at your desk  Remember, warm up time is a time to be quiet (below the music), be seated, and working  Phones need to be away.
Energy Transfer in the Environment & Air Movement
Atmosphere and Climate
Section 1.2 The Causes of Weather
Global Winds.
Global and Local Winds.
Dynamics in Earth’s Atmosphere
Global Winds.
Movement of Air Atmosphere.
Wind Causes of Wind.
Wind Causes of Wind.
The Transfer of Heat Outcomes:
Global Winds.
Wind Causes of Wind.
Presentation transcript:

Wind Coriolis Effect (p. 516) Prevailing Winds (p )

Coriolis Effect The spinning of the Earth creates an effect on any item that is in the air for a long period of time The spinning of the Earth creates an effect on any item that is in the air for a long period of time –Winds are therefore affected Was discovered by Gustave Coriolis when working with the army Was discovered by Gustave Coriolis when working with the army –They couldn’t figure out why their carefully aimed canons weren’t hitting their target

Coriolis Effect In the Northern hemisphere, the rotation is to the East (counterclockwise) In the Northern hemisphere, the rotation is to the East (counterclockwise) –Objects will ‘drift’ to the right In the Southern hemisphere, the rotation is to the West (clockwise) In the Southern hemisphere, the rotation is to the West (clockwise) –Objects will ‘drift’ to the left The Coriolis effect is noticed the least at the equator and the most at the poles The Coriolis effect is noticed the least at the equator and the most at the poles

Winds Some winds are small and regional Some winds are small and regional Many are major wind patterns that cover large areas Many are major wind patterns that cover large areas –These winds are called Prevailing Winds

Wind Patterns (Surface) Between 60° latitude and the poles Between 60° latitude and the poles –Winds move from East to West –They are called the Polar Easterlies W E

Wind Patterns (Surface) Between 30° and 60° latitude Between 30° and 60° latitude –Winds flow from West to East –They are called the Westerlies W E

Wind Patterns (Surface) Between the equator and 30° latitude Between the equator and 30° latitude –Wind flows from East to West –North of the equator they are called the Northeast Trade Winds –South of the equator they are called the Southeast Trade Winds

Jet Streams Jet streams are high speed winds in the upper troposphere Jet streams are high speed winds in the upper troposphere They flow from West to East and steer the weather like highs and lows They flow from West to East and steer the weather like highs and lows

Causes of Prevailing Wind Solar energies (the ones that make it through the atmosphere) strike close to the equator Solar energies (the ones that make it through the atmosphere) strike close to the equator Here, hot air rises and expands leaving a LOW pressure area behind Here, hot air rises and expands leaving a LOW pressure area behind When the rising air reaches the tropopause it moves North When the rising air reaches the tropopause it moves North

Causes of Prevailing Winds #2 Once the air reaches 30° latitude it has become colder and more dense so it sinks Once the air reaches 30° latitude it has become colder and more dense so it sinks –A HIGH pressure area is created Air at the surface then moves away from the HIGHpressureLOW at the equator that was created previously Air at the surface then moves away from the HIGH pressure towards the LOW at the equator that was created previously –As it moves it twists to the right THE NORTHEAST TRADE WINDS!!! THE NORTHEAST TRADE WINDS!!!

Causes of Prevailing Winds #3 Not all of the air goes back to the equator once it has reached the surface Not all of the air goes back to the equator once it has reached the surface Some of it is deflected North towards the LOW pressure area at 60° latitude Some of it is deflected North towards the LOW pressure area at 60° latitude –Twists to the right and creates the mid- latitude Westerlies At 60° latitude polar air creates a LOW when it pushes warmer air up to the jet stream At 60° latitude polar air creates a LOW when it pushes warmer air up to the jet stream

Causes of Prevailing Winds #4 At the North pole the air is cold and dense so it sinks creating a HIGH pressure area at the surface Surface air moves South, away from this high pressure area –I–I–I–It twists to the right creating polar easterlies Air rising at the 60° latitude can go North or South once it reaches the tropopause

Effects of Prevailing Winds The high and low pressure areas that are created by the prevailing winds allow heat to be transferred throughout the world The high and low pressure areas that are created by the prevailing winds allow heat to be transferred throughout the world They also cause precipitation and affect the climate of different regions They also cause precipitation and affect the climate of different regions –Rising air is warm and moist –Falling air is cold and dry Can you point out some of the climates? Can you point out some of the climates?

Prevailing winds and jet streams change with the seasons –T–T–T–They follow the sun!! The Northeast trade winds move south, closer to the equator during the winter