Coriolis Effect and Wind Patterns 3 rd factor that affects weather (Wind Speed and Direction)

Slides:



Advertisements
Similar presentations
What is wind?.
Advertisements

Winds Global Winds Chapter 16 Section 3 Pages Chapter 16 Section 3 Pages
Wind Notes.
Global Winds Winds that blow steadily from specific directions over long distances.
Weather.
Chapter 16 Section 3: Winds.
Mrs. Wharton’s Science Class
Heat & Wind by: Mrs. Wisher WRITE EVERYTHING IN BLUE!
Global and Local Winds.
Global and Local Winds.
Global and Local Winds i.
Wind and the Coriolis Effect
Wind.
Convection in Our Atmosphere
Weather Patterns Mr. Latzos. Starter Match the word with the definition Densityatmospherealtitude The distance above sea level The amount of mass in a.
Wind Causes of Wind.
Global Winds.
Global and Local Winds.
Wind coulter.
Wind Patterns.
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.
Unit 10 Lesson 4 Wind in the Atmosphere Copyright © Houghton Mifflin Harcourt Publishing Company.
Today’s Agenda… Quiz Review Water Cycle Anticipation Guide Air Movement Notes.
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.
WIND The horizontal movement of air from an area of high pressure to an area of low pressure.
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.
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.
Atmospheric Circulation
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 and the Coriolis Effect
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.
Coriolis Effect Global Winds Chapter 2.3 Pages Chapter 2.3 Pages
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.
Daily Weather Information
Global Winds. Air Movement Wind is the movement of air caused by differences in air pressure Wind ALWAYS moves from areas of high air pressure to areas.
Hour.3 By: Sam Hurwitz, Alex Payne, and Joey Peirick.
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.
Global and Local Winds i. What causes wind? Caused by a difference in air pressure due to unequal heating of the atmosphere.
Air Movement (53) Areas of Earth receive different amounts of radiation from the Sun because Earth is curved.
Unit 3 Lesson 3 Wind in the Atmosphere Copyright © Houghton Mifflin Harcourt Publishing Company.
Global Winds Chapter A. Global Winds and Local Winds What causes wind? What causes wind? 1. Wind is caused by the movement of air which is caused.
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.
Wind Atmospheric Circulation (22:39min). Wind The horizontal movement of air from an area of high pressure to an area of lower pressure. Caused by the.
Unit 3 Lesson 3 Wind in the Atmosphere
Global Winds, Jet Stream, Gulf Stream, and El Nino
Chapter 15 Section 3 Global and Local Winds.
Atmosphere and Climate
4.3 Air Currents.
Global and Local Winds.
Handout (green) Atmospheric Circulation
MYP 1 Air Currents.
Atmospheric Circulation
Global Winds.
Convection Notes.
Wind Causes of Wind.
Wind Causes of Wind.
Global and Local Winds.
Unit 3 Lesson 3 Wind in the Atmosphere
AIR currents Chapter 12 Lesson 3.
Weather Notes Part 3.
Wind Notes.
Wind Causes of Wind.
Presentation transcript:

Coriolis Effect and Wind Patterns 3 rd factor that affects weather (Wind Speed and Direction)

Wind What is wind? Wind is moving air. It moves from areas of high pressure to areas of low pressure. What is the main source that drives the winds? The SUN!!!

What causes wind? Winds are caused by the uneven heating and cooling of the earth. When warm air rises, cooler air flows underneath creating a convection current, thus causing wind!

The results from the earth’s rotation causing freely moving objects (such as airplanes) to veer toward the right in the Northern Hemisphere and to the left in the Southern Hemisphere. Affects things like wind, ocean currents, airplanes, and missiles. Coriolis Effect

4page01.cfm

Another example of the Coriolis Effect is a merry- go-round. If you tried to pass a ball across to someone on the other side, the ball would be deflected instead of moving in a straight line. fw/gifs/coriolis.mov fw/gifs/coriolis.mov

Without the Coriolis Effect, wind and weather patterns would be more stabilized because they would move in a straight line instead of “deflecting” to the right or left. This means there would be fewer changes in the atmosphere (weather patterns)—this would be boring!

Global Winds Wind patterns on Earth. Helped early sailors navigate the oceans 4 Types of Global Winds: 1.Polar Easterlies 2.Westerlies 3.Trade Winds 4.Doldrums

Polar Easterlies In the far north and south poles Cold, dense air sinks and moves away from the poles.

Westerlies Above the subtropical highs in the Northern Hemisphere and below the subtropical highs in the Southern Hemisphere, winds blow from the West towards the East.

Trade Winds Air movements toward the equator. Warm, steady breezes that blow almost continuously. The Coriolis Effect makes the trade winds appear to be curving to the west, whether they are traveling to the equator from the south or north.

Doldrums Area of calm weather near the equator Converging trade winds produce general upward winds as they are heated, so there are no steady surface winds. Cloudy, rainy weather develops most afternoons (tropical rainforests)

GGlobal Winds