+ All Categories
Home > Documents > Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more...

Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more...

Date post: 22-Dec-2015
Category:
Upload: stephen-atkins
View: 232 times
Download: 4 times
Share this document with a friend
Popular Tags:
18
Review
Transcript
Page 1: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Review

Page 2: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

A- Albedo• Is the % of solar radiation reflected by an object or

surface• Higher albedo = more radiation reflected by the surface

• Albedo, together with reflection by the atmosphere, thus decreases the amount of incoming radiation that actually absorbed by Earth

• High or low albedo?

a. A mirror : ___________b. A lawn : ___________c. A sidewalk : ___________d. An asphalt driveway : ____________

Page 3: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Albedo• Is the % of solar radiation reflected by an object or

surface• Higher albedo = more radiation reflected by the

surface

• Albedo, together with reflection by the atmosphere, thus decreases the amount of incoming radiation that actually absorbed by Earth

• High or low albedo?

a. A mirror : highb. A lawn : lowc. A sidewalk : lowd. An asphalt driveway : low

Page 4: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

8.8 Global Energy Transfer

Page 5: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

• The equator receives more radiation than the poles Earth is not heated evenly.

• Energy is transferred from equator to the poles

• Water in the hydrosphere and air in the atmosphere act as heat sinks, storing a great deal of thermal energy

• Comparing the same volumes, liquid water can hold more thermal energy than air

8.8 Global Energy Transfer Intro

Page 6: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

How is energy transferred in the atmosphere?

https://www.youtube.com/watch?v=WXuGYSM2D8k

Page 7: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Atmospheric circulation• Air at equator heats up, moves up

in the atm and becomes less dense creating areas of low pressure underneath (less matter)

• Air cools and sinks towards the poles creating areas of high pressure

•Air flows from high to low pressure creating wind.•Earth has permanent bands of high and low air pressure, thus there are prevailing winds that blow in the same direction almost all the time. •Due to Earth’s rotation, prevailing winds curve instead of moving directly north or south. They also push warm ocean water to the poles

Page 8: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Energy transferred in the atmosphere

• Convection currents: - a circular current in fluid

(e.g. air, water) caused by rising of warm fluids as cold fluids sinks

- Cold air holds less moisture and is drier than warm air

https://www.youtube.com/watch?v=WXuGYSM2D8k

Page 9: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

https://www.youtube.com/watch?v=i2mec3vgeaI

•The Coriolis Effect

•Air a the equator is rotating faster than air near the poles

•Faster air moving towards the poles “gets ahead” of the surface and appears to shift eastwards (as viewed from space).

•Slower air moving towards the equator (from poles) “lags behind” the rotating surface and appears to shift westwards (as view from space)

Page 10: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

ENERGY TRANSFER IN OCEANS

Page 11: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

How prevailing winds influence climate?

• Origin of prevailing winds (PW) influence whether climate is moist or dry

• As PW pass over ocean, H2O vapour is picked up, When reaches land, it becomes rain

• If PW come from poles, it’s cold and dry

Page 12: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Oceans- the driving forces of climate and weather

• https://www.youtube.com/watch?v=6vgvTeuoDWY

Page 13: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

• Generally moves warm water from the equator to the poles and cold water from the poles to the equator

• Ocean currents are driven by

1. surface winds (i.e. prevailing winds)

2. differences in salinity and temperature of ocean water.

How is energy transferred in the ocean?

Page 14: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Demo

• https://www.youtube.com/watch?v=4V5cOPKGEyE ( a more ideal version if we have the equipment)

• https://www.youtube.com/watch?v=_Ww6BIy3nc0 ( we did)

Page 15: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

2. Ocean Current caused by different in density and temp. of water

• Different seawater densities due to

a. Cold water is denser than warm water

b. Near the poles, ice is formed from fresh water leaving behind more salt in the remaining water (i.e. increasing sea water’s salinity)

• Different seawater temperature:

• Warm currents float while cold currents sink

Page 16: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

The Ocean Conveyor Belt

Thermohaline circulation: the continuous flow of water around the world, driven by temperature and salinity differences

https://www.youtube.com/watch?NR=1&v=SdgUyLTUYkg&feature=endscreens

Page 17: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

Examples of effects of Ocean currents

• Brazil receives a warm ocean current making the climate warm and moist allowing rainforest to flourish

• At the same latitude, Peru receives a cold ocean current, making the climate cool and dry (Atacama Desert in Peru)

Page 18: Review. A- Albedo Is the % of solar radiation reflected by an object or surface Higher albedo = more radiation reflected by the surface Albedo, together.

• http://oceanexplorer.noaa.gov/edu/learning/player/lesson08.html


Recommended