Heat Transfer, Greenhouse Effect, Ozone Layer Notes

Slides:



Advertisements
Similar presentations
2.1 Energy in the Atmosphere
Advertisements

Section 2: The Atmosphere
Jeopardy Life support The Sun’s Energy Gasses in the atmosphere The effect of human activities Lab safety Random facts Final Jeopardy.
Objectives Describe the composition of Earth’s atmosphere.
The atmosphere S6E4a: Demonstrate that land and water absorb and lose heat at different rates and explain the resulting effects on weather patterns.
Thermal Energy Transfer
Earth’s Atmosphere atmosphere water vapor troposphere stratosphere
I’m very HOT! Keep out! It’s very cold here! Ha! Ha! I’m not too cold or too hot! It’s OK here! What makes Earth‘s climate so moderate?
Solar Energy & the Atmosphere
Energy from the Sun Radiation is the transfer of energy by electromagnetic waves. Ninety-nine percent of the radiation from the Sun consists of visible.
Earth’s Changing Atmosphere. Main Topics Definition and Characteristics of the Atmosphere Changes to the Atmosphere composition Layers of the Atmosphere.
Chapter 3 Section 2.
The Dynamic EarthSection 2 Section 2: The Atmosphere Preview Bellringer Objectives The Atmosphere Composition of the Atmosphere Air Pressure Layers of.
Atmosphere “This PowerPoint puts the “phere” in other, lesser PowerPoints” - PPTA.
Radiation in the Atmosphere. Gases can absorb AND give off radiation. Objects around you look bright on a sunny day. Earth’s atmosphere reflects or absorbs.
The Atmosphere. Composition  Nitrogen  Oxygen  Other –Argon –Carbon Dioxide –Methane –Water Vapor  Atmospheric dust.
CHAPTER 14 Energy in the Atmosphere Section 1, pages
Energy in the Atmosphere
Radiation, Conduction, Convection. Heat Transfer Processes 1._____________ - Sun heats Earth’s surface in the form of rays or waves 2._____________.
Solar Energy Heat and Light. Energy Can take many different forms –____________ –Heat –____________.
radiation conduction convection Energy Transfer in the Atmosphere stability temperature inversiontemperature inversion.
Scale for learning – Weather 4 – I am an expert I can explain, in detail, the structure and how the atmosphere supports life and influences weather and.
Earth’s Atmosphere Energy Transfer in the Atmosphere Part Two.
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.
Section 1.3 Gases in the atmosphere absorb radiation.
The Dynamic EarthSection 2 Objective #9 Describe the layers of the Earth’s atmosphere.
The Dynamic EarthSection 2 WATCH?V=RIHRI_Z2KGS&FEA TURE=RELMFU&SAFE=ACTIV E.
The Dynamic EarthSection 2 Section 2: The Atmosphere Preview Bellringer Objectives The Atmosphere Composition of the Atmosphere Air Pressure Layers of.
DAY 1 Chapter 3 The Dynamic Earth Section 2: The Atmosphere.
Section 3.2 The Atmosphere
The atmosphere. The atmosphere vocabulary Altitude- distance above sea level Atmosphere- outer layer of a mixture gases that surrounds the Earth. Cycle-
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.
Section 2: The Atmosphere
Energy from the Sun Radiation is the transfer of energy by electromagnetic waves. Ninety-nine percent of the radiation from the Sun consists of visible.
Energy Transfer in the Atmosphere
3.1 Heat Transfer in the Atmosphere
Objectives Describe the composition of Earth’s atmosphere.
Chapter 3 notes Section 2.
Lesson 1-6.
Earth’s Changing Atmosphere
Section 2: The Atmosphere
The Atmosphere Weather and Climate
Radiation in the Atmosphere
Energy Transfer in the Atmosphere
Gases in the Atmosphere absorb Radiation
Section 2: The Atmosphere
Section 2: The Atmosphere
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. 4 ways the atmosphere affects.
The Atmosphere and Weather
The Dynamic Earth The Atmosphere.
Section 2: The Atmosphere
The atmosphere supporting life
Radiation in the Atmosphere
ATMOSPHERE Science.
Earth’s Changing Atmosphere
17.2 Heating the Atmosphere.
Atmosphere The Basics.
Section 2: The Atmosphere
Section 2: The Atmosphere
Section 2: The Atmosphere
Section 2: The Atmosphere
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. Atmosphere affects light in.
Atmosphere 1.3 RSG-B Answers.
Energy and Heat Transfer in the Atmosphere
Section 2: The Atmosphere
Chapter 1 Atmosphere Test Review
Section 2: The Atmosphere
Presentation transcript:

Heat Transfer, Greenhouse Effect, Ozone Layer Notes

How does the Earth get heated? Energy transfer from the sun

Energy The ability to do work or cause change Temperature Gas The average amount of energy of motion of each molecule (the measure of how hot or cold something is) Gas Moving particles, the hotter they get the faster they move

The atmosphere moves energy Energy moves by heat transfer There are 3 types of heat transfer Conduction Convection Radiation

Conduction The transfer of heat energy from one substance to another through DIRECT contact The Earth’s surface heats the air (gas) molecules directing above it Molecules of air gain energy when they collide with the molecules in grains of hot sand.

Convection Transfer of energy from place to place by the motion of gas or liquid (fluids) Up and down movement of molecules not the side to side movement

Density and Convection The atmosphere gets less dense at higher altitudes Warm air is less dense than cold air Warm air has more energy, so molecules move faster than cold ones This makes them collide more, then they spread out More space between molecules = less dense

Radiation The transfer of the Sun’s energy to the Earth’s surface Solar radiation heats both the surface and the air Includes visible light Earth’s surface gives off a type of invisible radiation called Infrared radiation

Earth’s absorption of Radiation 30% of incoming solar energy is reflected by clouds 70% is absorbed and becomes different forms of energy Absorbed by oceans, landforms, and living things (photosynthesis and respiration) This absorbed energy heats the Earth’s surface

Transfer of Energy

Gases Absorb and Give Off Radiation The Atmosphere affects light in 4 ways. Absorbs Light Reflects Light Lets Light Pass Through Emits (Gives Off) Light On sunny days more visible light gets to the earths surface. On cloudy days clouds reflect and absorb most of the sunlight

Forms of Radiation We Cant See Ultraviolet Radiation More energy than the light you can see Can cause sunburns and other damage Infrared Radiation Less energy than the light you can see Warms the materials that absorb it

Ozone Layer Protects Life Ozone - O3 Ozone in stratosphere is called the ozone layer Protects life on Earth Absorbs harmful ultraviolet radiation from sun Too much can cause sunburn, skin cancer, and can harm crops, plastic or paint Lets other types of radiation like visible light through

Greenhouse Effect Animation Keeps Earth Warm Slow the movement of energy away from the Earth’s surface Greenhouse gases Includes carbon dioxide, methane, water vapor, and nitrous oxide Gases mix with gases in the air like nitrogen and oxygen. Not its own layer Found in the troposphere Absorbs and emits infrared radiation Animation