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Electromagnetic waves Can travel through Space (no air in space) radiation Is the DIRECT transfer of energy through electromagnetic waves. 3 ways sun’s energy reaches the Earth 1. visible light 2. infrared radiation (heat) 3. ultraviolet

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Page 1:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

Electromagnet icwaves

Can travel through Space

(no air in space)

radiationIs the DIRECT

transfer of energy through

electromagnetic waves.

3 ways sun’senergy reaches the

Earth

1. visible light

2. infrared radiation (heat)

3. ultraviolet radiation

Page 2:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

visible light

ROY-G-BIV

ultravioletradiation

UV raysCauses sunburn

SMALLEST amount of radiation reaching

Earth

What happens to sun’s energy when it reaches

Earth?

RARAS

R Reflected back into space by clouds

A Absorbed by the earth’s surface (water,land)R Reflected back the earth’s surface

A Absorbed by atmosphere/clouds

S Scattered by dust

Page 3:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

Greenhouse effect Like a blanket

Keeps Earth warm

thermometer

Measurestemperature

2 most common temperature scales

Celsius Fahrenheit

Freeze 0 C 32 FBoil 100 C 212 F

Page 4:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

HEAT

Definition:

Energy transferredfrom a hotter

to a colderobject

to

+ Greenhouse -Effect

Helpful Harmful

Protects plants and

people from harmful UV rays; keeps planet warm

enough

Traps too much carbon

dioxide; warms up

planet

UNITS for TEMPERATURE?

Degrees

Page 8:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

3 KINDSOF

LOCAL WIND

1. SEA BREEZE

2. LAND BREEZE

3. MONSOON

monsoonSea / land breeze

over a LARGE AREA that changes with

the season.

Monsoon season

monsoon

Like in Forrest Gump movie

Rained, rained, rained …

Page 9:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

Coriolis Effect

HINT

CORIOLIS

CURVIOLIS

Coriolis Effect

Wind in northern hemispshere curve RIGHT

Wind in southern hemisphere curve LEFT

4Global Wind

Belts

1. Doldrums

2. Trade Winds

3. Prevailing Westerlies

4. Polar Easterlies

Page 15:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

Thermal energy

Vs.

Temperature

Tot al amount of energy

Vs.Average amount

of energy

FLUIDS(like air)

&AIR PRESSURErelationship

HIGH TOWARD Low

High to Low

psychrometerInstrument that

measuresRelative humidity

Moves

Page 17:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

GreenhouseEffect

the PROCESSby which gases (ozone)

holds HEAT in the ATMOSPHERE

How is the TROPOSPHERE

heated?

Mostly by CONVECTION

troposphere = weatherweather = hot, cold, wet,

dry, windy

WARM AIR

COLD AIR

Warm air is less dense

CONVECTIONhappens because

Cold air is more dense

Page 18:  · Web viewGreenhouse effect Like a blanket Keeps Earth warm thermometer Measures temperature 2 most common temperature scales Celsius Fahrenheit Freeze 0 C 32 F Boil 100 C 212 F

Global WindsVs.

Local Winds

Global winds over very LARGE areas

Local winds over small areas

LandBreeze

Comes from the land

Land cools faster than seaWarmer air over sea rises – cooler air from

land moves toward sea

Sea Breeze

Comes from the sea

Sea heats up slower than land Warmer land air rises – cooler air from sea moves toward the land.