the average yearly conditions of temperature and precipitation in a region

24
The average yearly conditions of temperature and precipitation in a region Climate

Upload: randall-singleton

Post on 19-Jan-2016

221 views

Category:

Documents


4 download

TRANSCRIPT

Page 1: The average yearly conditions of temperature and precipitation in a region

The average yearly conditions of temperature and precipitation in a region

Climate

Page 2: The average yearly conditions of temperature and precipitation in a region

Why do the leaves of plants change color and fall in the autumn?

What is hibernation and why do some animals engage in it? What types of animals, generally, hibernate?

Think about it…

Page 3: The average yearly conditions of temperature and precipitation in a region

Weather is the daily condition of Earth’s atmosphere at a particular place and time.

Climate is the average yearly conditions of temperature and precipitation in a region.

Climate is caused by:Trapping of heat in the atmosphereLatitudeTransport of heat by winds and ocean currentsAmount of precipitationShape and elevation of landmasses

Weather and Climate

Page 4: The average yearly conditions of temperature and precipitation in a region

The greenhouse gases are atmospheric gases that trap infrared radiation (heat energy) that has been reflected off the Earth’s surface thus maintaining Earth’s temperature range.

The natural event in which heat is retained by this layer of greenhouse gases is called the greenhouse effect.

The Greenhouse Effect

Sunlight

Earth’s Surface

Atmosphere

Some heat escapes into space

Greenhouse gases trap some heat

Greenhouse gases trap some heat

Page 5: The average yearly conditions of temperature and precipitation in a region

Could we survive without the greenhouse effect?No, Earth would be too cold for many organisms to

survive, including human beings.Can you name any greenhouse gases?

Think about cycles of matter…Water Vapor – evaporation (water cycle)Carbon Dioxide (CO2) – burning fossil fuels,

deforestation, volcanic eruptionsMethane (CH4) – decomposition/decay, livestock

wasteNitrous Oxide (N2O) – fertilizer, fossil fuels,

denitrificationSynthetic gases (e.g. CFCs) – industrial processes

The Greenhouse Effect

Page 6: The average yearly conditions of temperature and precipitation in a region

Earth is a sphere tilted on it axis.Therefore, solar radiation strikes different parts

of Earth at an angle that varies throughout the year. This leads to the seasons we have here.

The equator receives nearly direct sunlight all year.

The polar regions receive sunlight at a lower angle.

The three main climate regions of the earth are:TropicalTemperatePolar

Latitude

Page 7: The average yearly conditions of temperature and precipitation in a region

Earth’s Main Climate Zones

Sunlight

Most direct sunlight

90°N North Pole

Temperate

Tropical

Temperate

Polar

Arctic Circle

Tropic of Cancer

Equator

Tropic of Capricorn

Antarctic Circle

90°S South Pole

66.5°S

23.5°S

23.5°N

66.5°N

Polar

Sunlight

Sunlight

Sunlight

Page 8: The average yearly conditions of temperature and precipitation in a region

Unequal heating of Earth’s surface drives winds and ocean currents, which transport heat throughout the biosphere.

Warm air over the equator rises, while cooler air over the poles sinks toward the ground.

The upward and downward movement of air creates air currents, or winds, that move heat throughout the atmosphere.

Heat Transfer in Biosphere

Page 9: The average yearly conditions of temperature and precipitation in a region

Earth’s WindsWINDS

66.5°N

23.5°N

23.5°S

66.5°S Prevailingwinds

Southeast Trade WindsWesterlies

Polar Easterlies

Equator

Northeast Trade WindsWesterlies

Polar Easterlies

Page 10: The average yearly conditions of temperature and precipitation in a region

Similar patterns of heating and cooling occur in Earth’s oceans. Cold water near the poles sinks, then flows parallel to the ocean bottom, and rises in warmer regions.

Water is also moved at the surface by winds.Movement of the water creates ocean

currents, which transport heat energy throughout the biosphere.

Surface ocean currents warm or cool the air above them, affecting the weather and climate of nearby landmasses.

Heat Transport in the Biosphere

Page 11: The average yearly conditions of temperature and precipitation in a region

Ocean Currents

OCEAN CURRENTS

66.5°N

23.5°N

23.5°S

66.5°S

Equator

Warm currentsCold currents

Page 12: The average yearly conditions of temperature and precipitation in a region

Remember from our last class that carbon dioxide is released from a variety of sources. A major contributor to atmospheric CO2 is human activity.

Levels of CO2 in the atmosphere have risen dramatically sense the advent of the industrial revolution.Why do you think this is the case?

In 1850, just before the industrial revolution the [CO2] in the atmosphere is estimated at about 274 ppm.

In 2005, the [CO2] in the atmosphere was over 370 ppm, an increase of over 25%.

Atmospheric Carbon Dioxide

Page 13: The average yearly conditions of temperature and precipitation in a region

What do you think are some potential effects of increased CO2 in the atmosphere?

Atmospheric Carbon Dioxide

Page 14: The average yearly conditions of temperature and precipitation in a region

Some potential effects of increased [CO2] could be:Increased growth/productivity by vegetation

(increased levels of photosynthesis). Why? (Hint: last class)

C3 plants (rice, wheat, soybeans) are more limited by CO2 availability than C4 plants (sugarcane, corn) so C3 plants may spread into C4 areas.

A link between increased CO2 and increased temperature exists. So when [CO2] rises, temperature rises. Why? (Hint: this class)

What are some potential results, globally and locally, from rising temperatures?

Atmospheric Carbon Dioxide

Page 15: The average yearly conditions of temperature and precipitation in a region
Page 16: The average yearly conditions of temperature and precipitation in a region

The Holocene Extinction is the present, widespread, ongoing extinction during the current Holocene Epoch.

This is the Sixth Great Extinction, the largest since the one that killed off the last of the terrestrial dinosaurs.

The Holocene Extinction has been going on since about 11,000 BCE and has been attributed to anthropogenic causes by a majority of biologists.

Human-induced climate change, overexploitation, deforestation, and the introduction of non-native species may have all played a role.

Holocene Extinction

Page 17: The average yearly conditions of temperature and precipitation in a region

Because all species are interdependent upon one another, what is the potential impact of losing any one species?

The brazil nut, the tree from which the name of the edible nut is derived, is one of the most massive and important trees in the Amazon.

Only one creature, a rodent called the Agouti, can crack the shell, thus allowing the tree to reproduce.

Video: http://www.arkive.org/brazil-nut-tree/bertholletia-excelsa/video-11.html

Video: http://www.youtube.com/watch?v=HURyGlOksR0

Importance of Diversity

Page 18: The average yearly conditions of temperature and precipitation in a region

There are literally thousands of examples of species’ interdependence.

Many flowers have evolved to be dependent upon insects for pollination.Can you think of an example?

The Holocene Extinction is generally thought to have begun with the extinction of the megafauna at the end of the last Ice Age.

Many of these species were hunted to extinction, while others lost their sources of food due to human overexploitation.

Interdependence

Page 19: The average yearly conditions of temperature and precipitation in a region

The Wooly mammoth (Mammuthus primigenius)

The theory of its extinction is controversial.

Most scientists believe it was due to climate change, overhunting, or a combination of the two.

Megafauna

Page 20: The average yearly conditions of temperature and precipitation in a region

The Saber-toothed Cat (Smilodon populator)

Extinction causes thought to be similar to mammoth’s.

Likely due to overhunting by humans.

Megafauna

Page 21: The average yearly conditions of temperature and precipitation in a region

Baiji (Lipotes vexillifer)

Freshwater river dolphin from China

‘Effectively Extinct’ 2006

Caused by humans: pollution in rivers, habitat destruction (dams), fishing, collisions with boats.

Recent Extinctions

Page 22: The average yearly conditions of temperature and precipitation in a region

Javan Tiger (Panthera tigris sondaica)

Subspecies of tiger on Indonesian island of Java.

Extinct in 1980s due to hunting and habitat destruction.

Recent Extinctions

Page 23: The average yearly conditions of temperature and precipitation in a region

If trends continue, what species will most likely survive? Why?

If trends continue, what species will most likely go extinct? Why?

How is this related to global climate change?

Holocene Extinction

Page 24: The average yearly conditions of temperature and precipitation in a region

1. The Earth’s polar regions remain cold becauseA. they are never heated by the sun.B. the sun’s rays are at a very low angle at the poles.C. the greenhouse effect does not occur at the poles.D. heat is transported from the poles to the equator.

2. Earth’s temperature range is maintained byA. ocean currents and wind.B. latitude differences.C. the greenhouse effect.D. climate zones.

3. The Holocene ExtinctionA. is when the dinosaurs died.B. led to the Cambrian Explosion.C. resulted from photosynthesis evolution.D. is occurring right now.

Bell Ringer