Air currents lesson outline
[PDF File]Air Currents - Weebly
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Air Currents A. Global Winds 1. ... Lesson Outline LESSON 3. ... Key Concept Builder LESSON 3 Air Currents Key Concept How does uneven heating of Earth’s surface result in air movement? Directions: On each line, write the term that correctly completes each sentence. Each term is used only once.
[PDF File]Chapter 13 Unit Notes - Moore Public Schools
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w-w-. Lesson 3: Air Currents jet stream narrow band of high winds land breeze wind that blows from the land to the sea polar easterlies cold winds that blow from the east to the west near the North and South Poles sea breeze wind that blows from the sea to the land trade winds steady winds that flow toward the equator from east to west westerlies steady winds that flow from west to east
[PDF File]Convection Currents in the Air - Holbrook Science
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Think back to Lesson 4. What did you dis-cover about how the temperature of air affects the way air moves? Discuss this with your class. 2.Look back to the reading selection, “Air Masses,” on page 49 in Lesson 4. Where do you think air masses with different temperature and humidity conditions are most likely to meet in the United States ...
[PDF File]Chapter Twelve: Earth’s Atmosphere Lesson 3: Air Currents - Weebly
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Lesson 3: Air Currents The Sun’s energy warms Earth and depends greatly on its angle Poles are cooler because the Sun is at a lower angle oEquator strikes it nearly at a 90 angle therefore making it warmer Wind: the movement of air from areas of high pressure to areas of low pressure Polar easterlies Westerlies Trade Winds Equator –
[PDF File]Air Currents
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The first belt begins with warm air rising at the equator and dropping back to Earth near 30˚ latitude. The third cell, at the lowest latitude, is also a convection cell. Explai n the Coriolis effect. Coriolis effect: Global Winds I found this on page . I found this on page . Global Winds Belts I found this on page .
[PDF File]Chapter Resource Files Editable Air Currents
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Title: Microsoft Word - Chapter_Resource_Files_Editable_Air_Currents Author: mccunew Created Date: 11/21/2016 9:19:21 AM
[PDF File]Air Currents Notes - Leon County Schools
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Lesson Outline Air Currents A. Global Winds Date Class LESSON 3 1. The amount of energy an area receives is affected by the Sun's 2. More poles. reaches Earth's surface at the equator than at the ; high air 3. Low air pressure is usually located over the pressure is usually located over the is the movement of air from areas of high pressure
[PDF File]Lesson 8: Currents National Science - NOAA
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Lesson 8: Currents Overview Lesson 8 presents the mechanisms that drive surface and deep ocean currents. The process of global ocean circulation is presented, emphasizing the importance of this process for climate regulation. In the activity, students play a game focused on the primary surface current names and locations. Lesson Objectives
[PDF File]20141015101132771 - Weebly
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Lesson Outline Air Currents Global Winds I. The amount of energy an area receives is by the Date Class LESSON 3 Sun's 2. More poles. reaches Barth's surface at the equator than at the ; high air 3, Low air pressure is usually located over the pressure is usually located over the is the movement of air from areas of high pressure
[PDF File]20141015101132771
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Lesson Outline Air Currents Global Winds I. The amount of energy an area receives is by the Date Class LESSON 3 Sun's 2. More poles. reaches Barth's surface at the equator than at the ; high air 3, Low air pressure is usually located over the pressure is usually located over the is the movement of air from areas of high pressure
[PDF File]www.leonschools.net
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Air Currents Date Class LESSON 3 Directions: Write the conect term in the boxes to the right of each definition. Then unscramble the letters in the shaded boxes to spell a seventh term. jet stream trade winds land breeze westerlies polar easterlies wind sea breeze 1. the movement of air 2. a narrow band of high winds in the troposphere
[PDF File]ORISE Lesson Plan: Convection Currents
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Convection Currents . Submitted by: Veronica Carter, Science . Hairston Middle School, Greensboro, NC . Target Grade: Grades 6-12 . Time Required: 10 minutes . Standards/Topics Covered: NGSS Standards • HS-ESS2-3. Develop a model based on evidence of Earth’s interior to describe the cycling of matter by thermal convection. Central Focus:
Key Concept Builder Lesson 3 Air Currents Answers (PDF)
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[PDF File]Lesson Outline for Teaching
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Lesson Outline for Teaching Lesson 3: Biological Evidence of Evolution A. Evidence for Evolution 1. Evolution does not occur in a straight line with one species replacing another in a series of orderly steps. a. Living species that are closely related share a common ancestor. b.
[PDF File]Warren Hills Regional School District
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Air Currents Date Class LESSON 3 Directions: Write the correct term in the boxes to the right of each definition. Then unscramble the letters in the shaded boxes to spell a seventh term. polar easterlies wind sea breeze jet stream trade winds land breeze westerlies 1. the movement of air 2. a narrow band of high winds in the troposphere
[PDF File]Lesson 3 | Air Currents
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Air Currents A. Global Winds 1. The amount of energy an area receives is affected by the Sun’s . 2. More reaches Earth’s surface at the equator than at the poles. 3. Low air pressure is usually located over the ; high air ... Lesson Outline continued 8. A(n) is a narrow band of high winds that are commonly near the top of the troposphere. ...
[PDF File]Deep Ocean Currents and Air Convection Currents Fall 2018
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Deep Ocean Currents & Air Convection Currents 2018-2019– VINSE/VSVS Goal: To teach students about deep ocean currents by allowing them to visualize and understand how and why the currents form. To introduce students to convection in liquids and gases. Fits Tennessee standards Lesson Outline: 1. Introduction to Ocean Currents 2.
[PDF File]Chapter 15 Lecture Outline - LTCC Online
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Convection Currents • Releasing latent heat causes air to rise, cool, and lose more water vapor as precipitation. • Warm air close to equator vs. cold air at poles also produces pressure differences that cause weather. Air near surface warms and becomes less dense than the air above it; rises above cool air creating vertical convection ...
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