Heating the Earth Investigation 4, Part 1

Slides:



Advertisements
Similar presentations
The Atmosphere: Structure and Temperature
Advertisements

Investigation 4 Weather and Water
Inv. 4 “Heat Transfer” FOSS Weather and Water Grade 6
Heat Transfer. Review Marshmallow and flame Pancakes and feet What am I talking about when I use these words?
The Sun.
Chapter 2 Weather Factors
Chapter 22 Section 2 Review Page 560 #’s 1-9
Conduction Investigation 4, Part 2
Handout (yellow) Solar Energy and the Atmosphere Standard 3 Objective 1 Indicators a, b, and c Standard 3 Objectives 1, 2, and 3 Workbook Pages 3,
ENERGY FROM THE SUN Chapter 14.3 Pages Energy in the Atmosphere The sun is the source of ALL energy in our atmosphere. Three things that can.
Solar Energy and Heating the Atmosphere. Radiation Energy comes from the sun as radiant energy Radiation from the Sun can be visible (light) or invisible.
Abiotic Factors.
Objectives Explain how radiant energy reaches Earth.
Energy and Change CHAPTER the BIG idea CHAPTER OUTLINE Waves and heat flow transfer energy. Change occurs as energy is transferred. 1.1 Radiation transfers.
Climate Long time, Large Area. Weather short term, small area.
Unit 3 Lesson 3 Energy Transfer
Unit 10 Lesson 3 Energy Transfer
10.1 Temperature, Thermal Energy, and Heat The kinetic molecular theory explains that all matter is made up of tiny particles.  These atoms and molecules.
Sun Controls Earth’s Climate System Earth has a global climate system that includes air, land, liquid water, ice, and living things.climate system The.
Energy in the Atmosphere Heat Transfer Global Winds Local Winds
Warm Up 3/6/08 More solar energy reaches the equatorial regions than the polar regions because the equatorial regions a. are covered by a greater area.
Chapter 2 Weather Factors Section 2 Heat Transfer.
Heat Transfer in the Atmosphere Essential Question: How is heat transferred in the atmosphere?
Investigation 8 part 2 What Causes Wind
Compare Radiation & Conduction (Part 2) Contrasting Case Activity 4b Weather & Water, Investigation 4.
Heat Transfer Conduction, Convection, Radiation. Three Main Processes of Heat Transfer  Conduction  Convection  Radiation.
Chapter 22 Section 2 Handout
EARTH’S ENERGY. Energy from the Sun Nearly all of Earth’s atmosphere energy comes from the sun as electromagnetic waves. Most of the energy comes from.
Air. What’s in air? The atmosphere is made up mostly of nitrogen gas. Oxygen makes up a little more than 20% of the atmosphere. Air Composition.
Weather and Climate Unit Investigative Science. * All materials are made of particles (atoms and molecules), which are constantly moving in random directions.
Warm-Up What would happen if there was no more ozone? What would happen if there was no more ozone? –We would die. What are the four layers of the atmosphere?
ATMOSPHERIC HEATING Day 1. All matter is made of atoms Matter: anything that has mass and occupies space Atom: the smallest particle of a substance that.
Heat Transfer. Investigation 4- Heat Transfer Enduring Understanding: The movement of heat energy in and out of the atmosphere is an important element.
Heating of Different Earth Materials
Energy Budget The amount of energy arriving at the Earth and leaving the Earth must be in balance. If more energy arrives than leaves, the Earth will warm.
Conduction. There is NO cold… Only heat. What we perceive as cold is actually low levels of heat. When you hold an ice cube in your hand, cold doesn’t.
What is Energy? Energy – the ability to do work Everything that is done in the universe requires the use or transfer of energy. Most of the surface processes.
1. Which of these features is a landform associated with karst topography? Sinkholes Streams Natural levees Deltas 2. What are the major environmental.
Unit 3 Lesson 2 Energy Transfer Copyright © Houghton Mifflin Harcourt Publishing Company.
Thermal Energy 11/1/2011. What is thermal energy? Thermal energy is also known as heat and is the kinetic energy of all the molecules in a material. If.
Section 3.2 The Atmosphere
Earth Materials Lab Explanation. Why did water take so long to heat? Water has an important property. It takes five time more heat energy to raise an.
Heat Transfer Investigation 4. What are Earth Materials? Sand Air; different layers of the atmosphere (troposphere, mesosphere, etc) Dirt, soil Water;
Unit 9 Section 2: Solar Energy and the Atmosphere
Heat Transfer Investigation 4 Part 1.
Unit 3 Lesson 2 Energy Transfer
Heat Transfer.
What is heat? -Heat is energy that flows from an object with a higher temperature to an object with a lower temperature. High Temperature Low Temperature.
Atmospheric MOTION SC.6.E.7.5 Explain how energy provided by the Sun influences global patterns of atmospheric movement and the temperature differences.
Unit 3 Lesson 2 Energy Transfer
Conduction Investigation 4, Part 2
13.2 Energy Systems.
Solar Energy and the Atmosphere
The Atmosphere Weather and Climate
Earth’s Spheres & Atmospheric layers
Atmospheric Heating Chapter 15 section 2
Heating the Earth Investigation 4, Part 1
Energy Transfer In the atmosphere.
17.2 Heating the Atmosphere
Heating the Atmosphere
Atmospheric Heating Notes
17.2 Heating the Atmosphere.
Energy transfer in the atmosphere
What is HEAT? What do “hot” and “cold” really mean?
Unit 3 Lesson 2 Energy Transfer
15.3 energy in the atmosphere
Chapter 11 Section 4 How does heat move through the atmosphere?
17.2 – Heating the atmosphere – Part I
Atmospheric Pressure.
The Sun is the source of energy for the Earth.
Presentation transcript:

Heating the Earth Investigation 4, Part 1 Heat Transfer Heating the Earth Investigation 4, Part 1 TG-P.113-124

Objectives * I can explain how radiant energy from the Sun heats solid and liquid materials. * I can describe how heat transfers through multiple materials. I can describe how the atmosphere heated. I can determine how to conduct a fair experiment.

Weather Report What are the main elements of weather? Pressure TG- P.125 Pressure Movement of Air Heat Moisture

Weather Report What are we finding the temperature of? Air or atmosphere Hottest during the day? Afternoon When is it coldest? Just before daybreak TG- P.125

Energy Source? What energy source heats things up during the day? TG- P.125

Solar Heating Copy into ISN: Today we’re going to investigate what happens to different earth materials when the sun shines on them. Copy into ISN: Focus Question is: Which material absorbs the most heat? -soil, rock, water or air Make a prediction in your ISN. Explain why you chose your answer.

Solar Heating Investigation What happens to different earth materials when the Sun shines on them Turn to “Earth Material Temperatures Lab”page 14 and 15 of your lab book. TG- P.125 Student Lab Notebooks P.14-15

The Setup Monitor the temperature changes Each group will set up four earth material containers Soil Water Sand TG- P.125 Student Lab Notebooks P.14-15 Air Newspaper Monitor the temperature changes

Thermometer Make sure the thermometer is below the surface of the material in the container. Why is this important? TG- P.125-126 Student Lab Notebooks P.14-15 Water

Starting Temperature = 22˚C Temperature change Starting Temperature = 22˚C After 3 minutes, temperature = 26˚C 26˚ - 22˚ = 4˚C Temperature change is 4˚C After 3 more minutes, temperature = 29˚C 29˚ - 22˚ = 7˚C Temperature change is 7˚C TG- P.125-126 Student Lab Notebooks P.14-15

Graph the Data Turn to the “Earth-Material Temperatures Graph” Graph the temperature changes for each of the earth materials TG- P.127 Student Lab Notebooks P.14-15

Graphing Reminders Use a different color to identify the different materials (Include a key) Start numbers at 0, 0 Make uniform intervals Independent variable? Dependent Variable? Dependent TG- P.127 Student Lab Notebooks P.14-15 Time

Here is what SHOULD have happened: Water heats up the slowest and cools the slowest. Air and/or soil should have heated up the most and cooled the fastest as well.

Did You Notice? Increased the least Went down the slowest Water TG- P.127 Student Lab Notebooks P.14-15 If each earth material received the same amount of solar energy, how can you explain the differences in temperature?

Water Has important property Takes 5 times as much energy to heat water compared to soil or sand TG- P.128 Student Lab Notebooks P.14-15

Faster? Same amount of heat energy is absorbed equally by all materials Which heats up faster? Soil TG- P.128 Student Lab Notebooks P.14-15 Water Sand

Faster? Same amount of heat energy is absorbed equally by all materials Which heats up faster? Soil TG- P.128 Student Lab Notebooks P.14-15 The solid earth materials heat up faster than water Sand

Water vs. Soil Both absorb the same amount of solar energy Temperature of soil will be much higher than the water TG- P.128 Student Lab Notebooks P.14-15

Question If the sun heated the earth materials, how did it do that? How did the energy get from the Sun to the sand, soil, water and air? TG- P.129 Student Lab Notebooks P.14-15

Radiant Energy Energy comes from the Sun as radiant energy Travels as waves through space and air TG- P.129-130 Student Lab Notebooks P.14-15

Radiation Transfer of energy by electromagnetic waves Standing in sunshine, you are receiving energy from 150 million km away Transfer of energy by electromagnetic waves Visible light, Infrared, ultraviolet, microwaves, X-rays, and radio TG- P.129-130 Student Lab Notebooks P.14-15

Radiation Energy can travel over great distances or short distances Energy transfer at a distance without direct contact between the energy source and the energy receiver

Radiation When radiant energy strikes an atom or molecule, like a water molecule, or a molecule in soil, or air, the molecule gains energy and begins to move faster or vibrate more. We say the molecule absorbed the radiant energy. Absorbing radiant energy is one way energy transfers to matter.

Radiation Radiant energy strikes an atom or molecule H Radiant energy strikes an atom or molecule Molecule gains energy and begins to move faster TG- P.129-130 Student Lab Notebooks P.14-15

Molecular Motion Molecular Motion IS HEAT More motion in molecules = the hotter it is LIQUIDS TG- P.129-130 Student Lab Notebooks P.14-15 SOLIDS

Differential Heating Different materials heat up at different rates Accounts for the difference in temperature of water and soil Soil Water TG- P.129-130 Student Lab Notebooks P.14-15 Sand Air

Oceans and Lakes Can store more heat than landmasses, even though the temperature of the water may be lower. Can store more heat than can land Even though the temperature TG- P.130 Student Lab Notebooks P.14-15

Multimedia Show “Heat and Energy” animation on the Weather and Water CD-Rom. Focus on energy transfer through radiation. TG- P.130 Student Lab Notebooks P.14-15

Reading Page 20 Read “Thermometer: A Device to Measure Temperature” TG- P.130 Student Resource Book - P.20