Global Climates Weather is what happens over a short period;

Slides:



Advertisements
Similar presentations
Global Winds Winds that blow steadily from specific directions over long distances.
Advertisements

Heating of the Earth. Temperature Layers of the Atmosphere.
Global and Local Winds.
Topic: Ocean Systems Essential Question: How does energy from the Sun drive wind and ocean currents?
Do Now For Monday, October 22, 2012 Imagine you are flying from Seattle to San Francisco which is almost exactly due south of Seattle. Should the pilot.
Chapter 12 Section 6 Wind.
Wind Causes of Wind.
6.4.8: Explain how convection affects weather patterns and climate.
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.
Lesson 3 Reading Guide - Vocab wind trade winds westerlies polar easterlies Air Currents jet stream sea breeze land breeze.
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.
[ORIGIN from Greek anemos ‘wind’][ORIGIN from Greek baros ‘weight’]
Wind & Climate Wind – the horizontal movement of air. Low pressure – warm air rising. High pressure – cold air falling. Winds always blow from high pressure.
16-3 Winds(pages 552–558) 1. State how scientists describe and explain winds. 2. Distinguish between local winds and global winds. 3. Identify where the.
Wind John Harris - Head of Geography - Radley College - UK
Atmospheric movements We learned that energy is transferred from the Sun to the Earth creating convection currents. But, what type of currents???
The Coriolis Effect on Winds and Currents. Consider This: The Coriolis force has been observed since at least the 1650’s. Italian military officers wrote.
Convection Regions, Global Winds, Jet Streams. Atmospheric Convection Regions Since earth is unevenly heated, climate zones occur (different convection.
Key Idea #15 The warming of the Earth by the sun produces winds and ocean currents.
1.2 ATMOSPHERIC CIRCULATION Atmospheric circulation : global-scale movement of the layer of air surrounding the Earth. Hot air rises (low density) Cold.
Solar Energy & The Greenhouse Effect The driving energy source for heating of Earth and circulation in Earth’s atmosphere is solar energy (AKA the Sun).
Warm air near the Earth’s surface rises and then cools as it goes back up. Convection happens on a global scale in the atmosphere and causes global winds,
Heating of the Earth. Temperature Layers of the Atmosphere.
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.
Ocean Current s.  Warm currents flow away from the equator.  Cold currents flow toward the equator. Ocean Currents.
The unequal heating of the Earth's Atmosphere and Surface CAUSES Changes in air pressure WHICH CAUSES WIND.
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 Winds and Jet Stream. Global Winds The trade winds blow from east to west in the tropical region. Westerly winds blow west to east in the temperate.
Wind. What causes wind? Differences in heat and pressure cause winds. Cold air is more dense and creates more pressure. Different parts of the Earth receive.
Wind John Harris - Head of Geography - Radley College - UK
Solar Energy 6-4.7, Solar Energy Comes from the sun Causes the atmosphere to move (wind) Can be absorbed or bounced off the atmosphere Without.
Solar Radiation Powers all life Albedo  The reflectance of solar energy off earth’s surface  Dark colors = low albedo  Forests and ocean  Light colors.
Air Circulation. Air-Sea Interface The atmosphere and the ocean act as one independent system. Solar energy causes winds. Atmospheric winds create most.
• At the poles (areas which receive less solar radiation), the air is cold and descends towards the equator through the lower layers of the atmosphere.
Chapter 15 Section 3 Global and Local Winds.
Lesson 1 Earth’s Atmosphere Lesson 2 Energy Transfer in the Atmosphere
Whooosh!!!!! When you open the valve on a bicycle tube, the air rushes out. Why? The air inside the tube is at a higher pressure than the air outside the.
Atmosphere and Climate
4.3 Air Currents.
Global Winds Eric Angat Teacher.
Weather Patterns and Climate Bates
OCEAN SURFACE CURRENTS
Global Winds.
Global and Local Winds.
14.3 Air Movement and Wind.
Handout (green) Atmospheric Circulation
MYP 1 Air Currents.
Global Winds.
Ocean Currents & Climate
Wind & Climate Wind – the horizontal movement of air.
Winds.
Wind Causes of Wind.
Wind Causes of Wind.
Global and Local Winds.
Global Winds.
Currents and Climates Notes.
AIR currents Chapter 12 Lesson 3.
Weather Notes Part 3.
Wind Notes.
Wind Causes of Wind.
Wind Wind is created by solar energy. More specifically wind is created by the uneven heating of the Earth. Reasons why the Earth heats unevenly: 1)
Unit 1 Structure and Motion Part 2
14.3 Air Movement and Wind.
Global air circulation is influenced by the Coriolis Effect
Title: Atmosphere in Motion; Wind Bands Page #: 75 Date: 2/25/2013
Unit 6: Meteorology Take out your ESRT
Ocean Currents and Climate
Global and Local Winds Why does Air Move ?
Energy / Convection 6.E.2.B.3.
Topic: Ocean Systems Essential Question: How does energy from the Sun drive wind and ocean currents?
Presentation transcript:

Global Climates Weather is what happens over a short period; Climate includes conditions in an area over a long time.

Convection in the Atmosphere

Air Pressure Belts

Rainfall

The World’s Deserts

The Great Boreal Forests Why are there no great austral (southern) forests?

Prevailing Wind Direction - Remember Coriolis

How did Colombus sail to the New World?

Figure 3.17 Right turn in the northern hemisphere, and left turn in the southern hemisphere.

Coriolis causes surface currents to move at a 45 angle from the wind. Figure 3.19 Coriolis causes surface currents to move at a 45 angle from the wind.

Figure 3.21 Look at how high the pink (warm) is on the east coast and how low pink is on the west coast. This warms poles and cools tropics. Studies indicate that changes in circulation may cause climate change

Figure 3.24 The ocean has three main layers, the thin warm surface layer, the intermediate layer (main thermocline), and cold deep bottom layer.

There are other currents in the ocean. The great conveyer belt. Figure 3.25 There are other currents in the ocean. The great conveyer belt.

Figure 3.26

Figure 3.27

Figure 3.28

Figure 3.29