Atmosphere and Climate

Slides:



Advertisements
Similar presentations
22.3 Atmospheric Circulation
Advertisements

Wind Notes.
Wind Notes.
Air Movement on Earth.
Wind Causes of Wind.
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.
Movement of Air in Earth’s Atmosphere. What is wind? The movement of air from an area of higher pressure to an area of lower pressure. The movement of.
Air Movement Chapter 4 – Section 3 Pages
Welcome to Class Define radiation, convection, and conduction.
Chapter 15: Atmosphere Section 3: Air movement Study Guide.
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.
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.
Section 3: Atmospheric Circulation
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 and the Coriolis Effect
C. 22 Section 3 Atmospheric Circulation Air near Earth’s surface generally flows from the poles toward the equator.
Convection Regions, Global Winds, Jet Streams. Atmospheric Convection Regions Since earth is unevenly heated, climate zones occur (different convection.
Wind and Wind Patterns Chapter 2.2 Guided Notes
Welcome to Class Define radiation, convection, and conduction.
Air Movement (53) Areas of Earth receive different amounts of radiation from the Sun because Earth is curved.
JOURNAL #7 – AIR MOVEMENT 1. What is wind? 2. How does the Coriolis Effect play a role in air movement? 3. What are the doldrums?
Heat Transfer, Sea/Land Breezes, Winds, Coriolis Effect,
Global Wind Belts & the Jet Stream
Notes on “Air Movement”
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.
Energy Transfer in the Environment & Air Movement
Chapter 15 Section 3 Global and Local Winds.
Lesson 1 Earth’s Atmosphere Lesson 2 Energy Transfer in the Atmosphere
Energy Transfer in the Environment & Air Movement
4.3 Air Currents.
Weather Patterns and Climate Bates
Global and Local Winds.
Global and Local Winds i.
Air Currents Chapter 16 Section 3.
The Coriolis Effect.
Wind and Wind Patterns Chapter 2.2 Guided Notes
14.3 Air Movement and Wind.
Wind and Wind Patterns.
Handout (green) Atmospheric Circulation
Energy Transfer in the Environment & Air Movement
MYP 1 Air Currents.
Wind and the Coriolis Effect
Atmospheric Circulation
Global Winds.
More air pressure at Earth’s surface. Warm air is less dense & rises.
Global and Local Winds i Kinsey
Global and Local Winds Why does Air Move ?
Today’s Agenda… Get your clickers! Water Cycle Review Quiz
Global & Local Winds.
Wind.
Wind and Wind Patterns Chapter 2.2 Guided Notes
Wind Causes of Wind.
Wind Causes of Wind.
Section 3: Atmospheric Circulation
Global and Local Winds Why does Air Move ?
Wind circulation through the atmosphere
Global Winds.
Wind Notes 2012.
Winds.
AIR currents Chapter 12 Lesson 3.
Weather Notes Part 3.
Wind Notes.
Atmosphere & Weather All About Winds.
Wind Causes of Wind.
14.3 Air Movement and Wind.
14-4 Movement of Air Wind – caused by the uneven heating of Earth’s atmosphere. *heats unevenly due to its tilt and curved surface *difference in pressure.
Global and Local Winds.
Movement of Air.
Global and Local Winds Why does Air Move ?
Presentation transcript:

Atmosphere and Climate

Objective and Key Concepts How does uneven heating of Earth's surface result in air movement? How are air currents on Earth affected by Earth's spin? What are the main wind belts on Earth?

THE SUN! Global Winds Wind patterns can be global or local. There are great wind belts that circle Earth. The energy that causes this large movement of air comes from.... ? THE SUN!

Unequal Heating of Earth's Surface Not all areas on Earth receive the same amount of energy from the sun because it depends on the sun's angle.

light Areas near the equator are known as the tropics. Sunlight strikes Earth's surface there at a 90 degree angle all year-round. They receive more sunlight, which causes the land, water, and air at the equator to be warm. Near the poles, sunlight strikes Earth at a low angle. It is spread over more surface area and it is colder.

Air Density Warm air rises and cold air sinks. Warm air is less dense than cold air, just like warm water is less dense than cold water.

Wind Knowing that warm air is less dense than cold air, which do you think puts more pressure on Earth? Air pressure is usually low over the tropics because it's warm there... Air pressure is high over colder areas such as the poles. This difference in pressure creates wind. WIND- movement of air from areas of high pressure to areas of low pressure.

Coriolis Effect Because the Earth spins, wind does not move in perfectly straight lines!

Earth’s Rotation Affects Wind Direction Because Earth rotates, scientists are able to tell the directions wind will flow. The Coriolis Effect is the influence of Earth’s rotation on wind patterns. Global winds curve as the Earth turns beneath them. Winds in the northern hemisphere curve right and winds in the southern hemisphere curve left.

Prevailing Wind Types Trade winds Steady winds that flow east to west polar easterlies Cold winds that blow from east to west near the poles prevailing westerlies Steady winds that flow west to east

Jet Streams Near the top of the troposphere is a narrow band of high winds called the jet stream. Jet streams flow around Earth from west to east and influence weather. They move cold air toward the equator, and warm air toward the poles as fast as 300 km/hour, and have a strong influence on our weather.

Sea and Land Breezes Sea breeze- wind that blows from the sea to the land due to local temperature and pressure differences. Because land warms faster than water, the differences in pressure over the warm land and the cooler water results in a cool wind that blows from the sea onto land.

Land Breezes Land breeze- wind that blows from the land to the sea due to local temperature differences. At night, the land cools more quickly than the water. An area of low pressure forms over the warm water. Cool air over land moves toward low pressure over the water.