+ All Categories
Home > Documents > Earth’s Changing Environment Lecture 13 Global Warming.

Earth’s Changing Environment Lecture 13 Global Warming.

Date post: 30-Dec-2015
Category:
Upload: mitchell-hardy
View: 217 times
Download: 2 times
Share this document with a friend
Popular Tags:
40
Earth’s Changing Environment Lecture 13 Global Warming
Transcript
Page 1: Earth’s Changing Environment Lecture 13 Global Warming.

Earth’s Changing EnvironmentLecture 13

Global Warming

Page 2: Earth’s Changing Environment Lecture 13 Global Warming.

The Earth is in an Interglacial Period

Last Glacial Maximum was 18,000 years ago and Global temperature was approximately 10 F colder than now

The last ice age ended 11,000 years ago.

Page 3: Earth’s Changing Environment Lecture 13 Global Warming.

Pleistocene: Includes Last Ice AgeHolocene: Since last Ice Age

Page 4: Earth’s Changing Environment Lecture 13 Global Warming.

Average Earth Temperature increased 0.6 oC (1 F) during 20th Century

Page 5: Earth’s Changing Environment Lecture 13 Global Warming.

Temperature Conversions

T (F) = 1.8 T(oC)

Temperature rise of 5 oC is equivalent to a temperature rise of 9 F

T (F) = 1.8 T(C) + 32 F

5 oC is equivalent to 41 F

Page 6: Earth’s Changing Environment Lecture 13 Global Warming.

Current temperature: highest in 1000 years.

Page 7: Earth’s Changing Environment Lecture 13 Global Warming.

Greenhouse Gases

Greenhouse gases are emitted by human activities.

Page 8: Earth’s Changing Environment Lecture 13 Global Warming.

Greenhouse Warming

The surface temperature of the earth is determined by the balance between the energy gain from solar radiation and the energy loss by IR radiation.

Page 9: Earth’s Changing Environment Lecture 13 Global Warming.

Greenhouse Warming:Greenhouse Gases

Greenhouse gases allow sunlight to reach the surface, but absorb IR radiation from the surface. These effects cause the surface of the Earth to get hotter.

Page 10: Earth’s Changing Environment Lecture 13 Global Warming.

Greenhouse Gases

Carbon dioxide – fossil fuel combustion.

Methane – fossil fuel production, decomposition of organic wastes.

Nitrous oxide - agricultural and industrial activities, as well as during combustion of solid waste and fossil fuels.

Page 11: Earth’s Changing Environment Lecture 13 Global Warming.

Impacts

Rising global temperatures are expected to raise sea level,

Change precipitation and other local climate conditions.

Changing regional climate could alter forests, crop yields, and water supplies

Damage ecosystems. Deserts may expand into

existing rangelands.

Page 12: Earth’s Changing Environment Lecture 13 Global Warming.

Sea Level Rise – thermal expansion and melting ice caps and glaciers

Page 13: Earth’s Changing Environment Lecture 13 Global Warming.

Global warming is anthropogenic.

Page 14: Earth’s Changing Environment Lecture 13 Global Warming.

Increasing atmospheric CO2 concentration

Atmospheric increase = Emissions from fossil

fuels 

+ Net emissions from changes in land use 

- Oceanic uptake 

- Terrestrial sinks

Page 15: Earth’s Changing Environment Lecture 13 Global Warming.

Humans emit 24 billion tons per year.

60% stays in atmosphere Increases atmospheric CO2

by 0.4% / year. 25% increase from

280 ppm to 350 ppm

Atmospheric CO2

Page 16: Earth’s Changing Environment Lecture 13 Global Warming.

CO2 550 ppm to 1000 ppm in 2100

Page 17: Earth’s Changing Environment Lecture 13 Global Warming.

Temperature Increase: 1.5 oC – 6 oC by 2100

Page 18: Earth’s Changing Environment Lecture 13 Global Warming.

Extinction of Species

Page 19: Earth’s Changing Environment Lecture 13 Global Warming.

Recent Letter in “Nature”

Extinction risk from climate change

Nature 427, 145 - 148 (08 January 2004); doi:10.1038/nature02121

On the web at www.nature.com

Page 20: Earth’s Changing Environment Lecture 13 Global Warming.

Results of the Study

“ When the average of the three methods and two dispersal scenarios is taken, minimal climate-warming scenarios produce lower projections of species committed to extinction (18%) than mid-range (24%) and maximum-change (35%) scenarios.”

Page 21: Earth’s Changing Environment Lecture 13 Global Warming.

Rapid Temperature Change

Temperature rise over the next 100 years will be so rapid 0.3oC per decade that plants and animals will not be able to migrate north or to higher altitude rapidly enough to survive

Page 22: Earth’s Changing Environment Lecture 13 Global Warming.

Biodiversity

10 million species1.6 million

identified speciesMammals & birds

known Insects & plants

unknown

Page 23: Earth’s Changing Environment Lecture 13 Global Warming.

Biodiversity

Biodiversity increased over the last 600 million years

Occasional mass extinctions

Last major extinction (K-T) 65 million years ago.

Human activities will cause the next mass extinction

Page 24: Earth’s Changing Environment Lecture 13 Global Warming.

Extinctions

Recovery from mass extinctions takes millions of years.

Species are extinct forever.

Page 25: Earth’s Changing Environment Lecture 13 Global Warming.

KT Extinction

All dinosaurs became extinct.

65 million years ago.Caused by meteor

impact.

Page 26: Earth’s Changing Environment Lecture 13 Global Warming.

CO2 effects are long-term

Page 27: Earth’s Changing Environment Lecture 13 Global Warming.

Long term impacts depend on emissions

Page 28: Earth’s Changing Environment Lecture 13 Global Warming.

Adaptation and Mitigation

Page 29: Earth’s Changing Environment Lecture 13 Global Warming.

Mitigation

Reduce CO2 emissions by reducing consumption of fossil fuel.

Protection of rainforests and other CO2 sinks.

Page 30: Earth’s Changing Environment Lecture 13 Global Warming.

Carbon Emission Coefficient(Million Metric Tons of Carbon/QBtu)

Coal 26

Oil 19

Natural Gas 14

Page 31: Earth’s Changing Environment Lecture 13 Global Warming.

Global Carbon Emission

Global Carbon Emission of C in the form of CO2:

6.6 billion metric tons

Convert to CO2:

44/12 x 6.6 billion metric tons

= 24 billion metric tons

Page 32: Earth’s Changing Environment Lecture 13 Global Warming.

Calculate US Carbon Emissions

US Carbon Emission =

26 MMT/QBtu x 22 QBtu

+ 19 MMT/QBtu x 38 Qbtu

+ 14 MMT/QBtu x 23 QBtu

= 1.6 Billion Metric Tons

Page 33: Earth’s Changing Environment Lecture 13 Global Warming.

Calculate US Carbon Emissions

US / Global

= 1.6 BMT / 6.6 BMT

= 24 %

The US emits 24% of Global CO2.

Page 34: Earth’s Changing Environment Lecture 13 Global Warming.

Kyoto Protocol

The US does not support the Kyoto Protocol, an international treaty to reduce global warming.

Page 35: Earth’s Changing Environment Lecture 13 Global Warming.

US Objections to Kyoto

Developing nations not bound, initially.

Reducing fossil fuel use would disrupt US and global economy.

Page 36: Earth’s Changing Environment Lecture 13 Global Warming.

The US has not developed a CO2 Reduction Plan

Bush administration emphasizes energy production and consumption.

                              

Page 37: Earth’s Changing Environment Lecture 13 Global Warming.

Mitigation: Reduce Carbon Emissions

We will address this issue in the next part of the course.

Page 38: Earth’s Changing Environment Lecture 13 Global Warming.

Mitigation: Carbon Sequestration

Page 39: Earth’s Changing Environment Lecture 13 Global Warming.

What are some adaptation steps?

Protect endangered species with larger refuges.Avoid flooding risks.Protect water supplies.Protect grasslands and agricultural lands against overuse.

Page 40: Earth’s Changing Environment Lecture 13 Global Warming.

Global Warming Ice Age?


Recommended