22
Paleoclimate & Climate Change

Paleoclimate & Climate Change

  • Upload
    ward

  • View
    33

  • Download
    0

Embed Size (px)

DESCRIPTION

Paleoclimate & Climate Change. The Geologic Time Scale. Low Resolution past 600 million. Vostok Data Past ½ million years. Younger Dryas Event = Big Freeze. The Younger Dryas Event. - PowerPoint PPT Presentation

Citation preview

Page 1: Paleoclimate & Climate Change

Paleoclimate & Climate Change

Page 2: Paleoclimate & Climate Change

The Geologic Time Scale

Page 3: Paleoclimate & Climate Change

Low Resolution past 600 million

Page 4: Paleoclimate & Climate Change

Vostok Data Past ½ million years

Page 5: Paleoclimate & Climate Change

Younger Dryas Event = Big Freeze

Page 6: Paleoclimate & Climate Change

The Younger Dryas Event In the transition from the last glacier

ice age which ended 16,000 years ago to our present day, there was a short period of intense cold.

This event occurred 11,000 years ago and is known as the Younger Dryas event.

The event lasted 1000 years and temperatures dropped 7 degrees Celsius!

Page 7: Paleoclimate & Climate Change

A Dramatic Temp Decline

Page 8: Paleoclimate & Climate Change

Younger Dryas Event

The Younger Dryas caused the extinction of many large mammals across N. America including Saber Toothed Cats, Mammoths, and Mastodons.

One possible explanation is that warming temperatures shut down the Atlantic Conveyor creating a dramatic climate event lowering global temperatures.

Page 9: Paleoclimate & Climate Change

The Atlantic Conveyor

Page 10: Paleoclimate & Climate Change

Recent Events

Page 11: Paleoclimate & Climate Change

The Maunder Minimum

Page 12: Paleoclimate & Climate Change

1650 – 1720 Maunder Minimum

Page 13: Paleoclimate & Climate Change

The Future

We are currently in an interglacial period. Past data would suggest that we should be heading into a cooling period however….

Page 14: Paleoclimate & Climate Change

The Keeling Curve

Page 15: Paleoclimate & Climate Change

Future CO2 Projections

Page 16: Paleoclimate & Climate Change

Future Temperature Projections

Page 17: Paleoclimate & Climate Change

Sea Level Projections

Page 18: Paleoclimate & Climate Change

Gases Contributing to the Greenhouse EffectGas Formula Contribution

Water Vapor H2O 36 – 72%

Carbon Dioxide CO2 9 – 26%

Methane CH4 4 – 9%

Ozone O3 3 -7%

Page 19: Paleoclimate & Climate Change

Carbon Dioxide

The atmospheric lifetime of CO2 is estimated to be between 30 to 95 years.

An increase in CO2 causes an increase in temperature resulting in an increase in water vapor . It is this water vapor that contributes to most of the warming.

Methane is 72 times stronger than CO2 at absorbing heat however it is present in smaller concentrations and has a shorter life in the atmosphere

Page 20: Paleoclimate & Climate Change

Future Climate Maps for US

Page 21: Paleoclimate & Climate Change

Global Climate Precip. Forecast

Page 22: Paleoclimate & Climate Change

Final Summary

Climate change means different “things” for different regions of the world.

Higher latitudes will experience greater temperature changes.

Computer models forecast drier conditions for much of the western and central United States.