Do Now for Wednesday, October 10th Which is cooler on a hot, sunny day, a parking lot or a field of grass? EXPLAIN WHY!!!

Slides:



Advertisements
Similar presentations
2.1 Energy in the Atmosphere
Advertisements

Heat Transfer.
Chapter 22 Section 2 Review Page 560
Chapter 2 Weather Factors
The Movement of Heat Chapter 4 Lesson 19 TCAP Coach.
Remember! Heat is transferred in three different ways:
Chapter 22 Section 2 Review Page 560 #’s 1-9
The atmosphere S6E4a: Demonstrate that land and water absorb and lose heat at different rates and explain the resulting effects on weather patterns.
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,
Chapter 2: Weather Factors
Energy Transfer EARTH SCIENCE.
Key Words radiation budget electromagnetic spectrum albedo Understand the concept of radiation and heat exchange Outline factors that control incoming.
Heat Transfer.
The Atmosphere B3: Weather Factors Part 1 – Energy in the Atmosphere.
Chapter 2; Section 2 Atmospheric Heating
16-2 Heat Transfer. (pages 548–551) 1
Do Now For Thursday, October 18, 2012 Explain the positions of the Earth, moon and sun during a solar eclipse. Explain the positions of the Earth, moon.
Objectives Explain how radiant energy reaches Earth.
Heating of the Atmosphere
CHAPTER 14 Energy in the Atmosphere Section 1, pages
Transmission of Heat. Conduction n Heat transfer due to direct contact n Either between different materials in thermal contact or different parts of the.
Chapter 10, Section 2 Chapter 22, Section 2. Solar Energy Key Terms: Create a flashcard for each. The words can be found starting on page 555 or use the.
Heat Transfer Chapter 2, Section 2 p How Heat is Transferred Heat: the energy transferred from a hotter object to a cooler one.
Key Idea #14 There is a relationship between the warming of the Earth’s atmosphere by the sun and convection within the atmosphere and oceans.
Energy in the Atmosphere
Heat Transfer. Heat transfer Everything is made of molecules. When molecules gain energy they move faster and create more heat. (The faster the molecules.
Chapter 2 Weather Factors Section 2 Heat Transfer.
Solar Energy Heat and Light. Energy Can take many different forms –____________ –Heat –____________.
The Atmosphere Preview Section 2 Atmospheric Heating Concept Mapping.
Air Pressure Ch. 15. Air Pressure Review Air has mass. Air takes up space. Air has density. Air pressure is the weight of a column of air pressing down.
C HAPTER 2; S ECTION 2 A TMOSPHERIC H EATING Heat transfer.
Bell work How is food heated in an oven? How is food heated on a range top?
Chapter 22 Section 2 Handout
Energy in the Atmosphere Chapter 16 Section 1 Pages Chapter 16 Section 1 Pages
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.
Energy in the Atmosphere. Electromagnetic Waves Electromagnetic waves are energy from the sun that can travel through space The transfer of energy by.
Heat Transfer.
Chapter 16 : Weather Factors Section1 : Energy in the Atmosphere By : Katelyn Angers.
TA12A –Teach About Heating Earth’s Air Use with BrishLab ES12A Done By: Coach – Period All This material is CC by StarMaterials.com.
On a hot sunny day, did you ever see cars, buildings, or other objects appear to shimmer or waver on the other side of a street or parking lot? What causes.
HEAT TRANSFER SC Standard Tuesday, January 4, 2011 Complete planner Get out a sheet of paper and entitle HEAT TRANSFER NOTES…complete header &
23.2 Solar Radiation & the Atmosphere Electromagnetic Radiation The EM spectrum Radiation is energy that does no require matter to travel. It travels as.
CHAPTER 19 HEAT TRANSFER IN THE ATMOSPHERE. WHAT IS THE ATMOSPHERE? Earth’s atmosphere is heated by the transfer of energy from the sun. Some heat comes.
Atmospheric Heating.
Transfer of Energy.
Unequal Heating, Air Pressure and Winds
Unequal Heating, Air Pressure and Winds
Chapter 2; Section 2 Atmospheric Heating
ENERGY IN THE BIOSPHERE
Do Now # 4 Do you think a bottle of water sitting on the desk has thermal energy? Explain. 2. Do you think a bottle of water sitting on the desk has kinetic.
Energy Transfer in the Atmosphere
Chapter 2; Section 2 Atmospheric Heating
Heat Transfer.
Heat Transfer.
Atmospheric Heating Chapter 15 section 2
Heat Transfer.
Section 2: Solar Energy and the Atmosphere
Section 2 Atmospheric Heating.
Heating the Atmosphere
17.2 Heating the Atmosphere.
The Transfer of Heat Ms. De Los Rios 7th Grade
Chapter 2; Section 2 Atmospheric Heating
Energy and Heat Transfer in the Atmosphere
Climate Earth’s Energy Budget.
Heat in the Atmosphere.
Solar Energy and the Atmosphere
15.2 Atmospheric Heating Weather Factors
Heat Transfer.
The Sun is the source of energy for the Earth.
Heat Transfer.
Presentation transcript:

Do Now for Wednesday, October 10th Which is cooler on a hot, sunny day, a parking lot or a field of grass? EXPLAIN WHY!!!

Do Now for 10 – 11 – 12! It’s the middle of winter and the heat has stopped working in your house. DISCUSS three ways you could stay warm in this situation.

“Do Now” for Monday, Oct. 15 Hypothesize: Which would heat up faster on a warm sunny day, the water in a lake or the sandy beach around it? Which will cool off faster after the sun goes down?

Do Now for Tuesday, October 16 Mr. Van Etten has three machines he is using to make popcorn. Use science terms from chapter 16 to describe what types of heat is each one producing in the process of making this treat?

Thermal (heat) Energy We are learning to: describe how thermal energy transfers occur in the atmosphere an ocean. We are looking for how energy from the sun is transferred by radiation, conduction and convection to the atmosphere and ocean. Energy Transfer We are learning to: explain the relationship between thermal energy to the formation of both atmospheric and ocean currents. We are looking for; explain how currents form from thermal energy transfers that occur in the atmosphere and oceans. Week 8 – Heat Energy and Energy Transfer Ch

Convection-Conduction-Radiation

Electromagnetic waves travel through space and deliver energy to our atmosphere. Most heat energy travels to Earth as radiation! *

The term “RADIATION” is used to describe electromagnetic energy..

In the middle of the day, the sky appears blue due to “scattered visible light.” Gas molecules in our atmosphere help to scatter short wavelength light so the afternoon sky looks blue or violet.

At dawn or dusk, the sky and clouds can look orange or red because the blue light spectrum is removed at these times

Much of this infrared energy in our atmosphere is absorbed by water vapor (clouds), CO 2 and other gases. This heat is held around Earth in a “GREENHOUSE EFFECT.”

The Greenhouse Effect is a natural process that has kept temperatures suitable to support life on Earth for thousands and millions of years!

Human impact over the past 200 years has added more and more CO 2 to our atmosphere causing global temperatures to increase.

Heat travels from hotter objects to cooler objects in three ways. Radiation! Heat transfer by electromagnetic waves. Examples include the sun, a campfire, microwave oven or nuclear radiation. Similar to the sun, the Earth gives off or radiates heat. Do living things radiate heat?

Conduction! The direct transfer of heat from one substance to another (touching).Examples include feet on hot sand, a hand warmer, a pot on a stove, heat passing through the Earth.

Convection! The transfer of heat through a fluid (gas or liquid). Hot air vent (furnace blower), hair dryer, clothes dryer, “convection oven – stove,” hot air popcorn popper.

All three processes are at work in our troposphere. Most of the heat transfer in our troposphere as well as our oceans comes from CONVECTION. Closer to the ground, the air gets warmer. The warm air rises and becomes denser and then sinks back. A cycle of warming and cooling occurs.

In our oceans, CONVECTION is responsible for causing currents!

Even under ground, CONVECTION currents are at work!

The Gulf Stream is an ocean current created by convection currents!