Title: THE HUMAN FOOTPRINT
1THE HUMAN FOOTPRINT
2Tragedy of the Commons
- Garrett Haudin
- commonly held resource
- each individual will attempt to maximize personal
gain - self interests gt public interests
- degradation of resource
- cost shared by all
3Only 18 of the earths wild lands remain
The human population economy grow while the
ecosphere shrinks
- Only 18 of the earths wildlands remain
4Can we create another Earth?
- Biosphere II
- ecotechnological experiment
- different ecoregions
- 1991-1993
- 8 people
- sustainable?
5Biosphere II Results
- drop in atmospheric oxygen
- high species losses (including pollinators)
- weedy species flourished
- low crop productivity
- water quality degraded
- costs 25 mil/person
6How many earths do we need?
- E. O. Wilson estimates that we would need 3-4
earths if all 6 billion people had the same
standard of living as Americans
7Climate Change
8The Greenhouse Effect
- natural process
- enhanced greenhouse effect due to human
activities
9Climate Change Through the Ages
- climatic fluctuations during Earths history
- since Industrial revolution burning of fossil
fuels has increased levels of greenhouse gases by
30
10Human Enhancement of Greenhouse Effect
Mauna Loa Observatory, Hawaii
11(No Transcript)
12Carbon Dioxide Trends
- before the Industrial Era (c.1750), atmospheric
carbon dioxide (CO2) concentration was 280 10
ppm for several thousand years - CO2 has risen continuously since then, reaching
367 ppm in 1999 - recent data from ice cores show current levels of
atmospheric CO2 unprecedented in last 675,000
years of Earths history (Siegenthaler et al.
2005)
13Human Enhancement of Greenhouse Effect
14Carbon Dioxide Trends
15Contributions of Greenhouse Gases to Global
Warming
16Human activities that contribute to Global Warming
17Temperature Trends
- global temperature increasing currently 0.5
degrees C annually worldwide
18Temperature trends in the lower US1901 to 1998
19Relationship between temperature and carbon
dioxide over the past 160,000 years
20Ice Melting and Glacial Retreat
21Snow, Ice Hydrological ChangesGangotri
Glacier, India
22Ice Sheets and SLR
calving front along edge of Greenland Ice Sheet
- Greenland Ice Sheet has 7 m of sea level
equivalence - West Antarctic Sheet has 5 m of sea level
equivalence - if both melt, a combined 12 m rise in sea level
23Historical Changes in Sea Level
- direct cause of sea level rise is input of
additional water currently locked up in polar
ice sheets - rapid shifts in sea level in the past due to
melting of glacial ice sheets - sea level rose at an average rate of 10 mm/year
between 15,000 and 6,000 years ago - indirectly through thermal expansion of water
24Recent Sea Level Rise
- IPCC found that melting of polar ice caps
contributed 0.2-0.4 mm/year to sea level rise in
the 20th century - average annual rates of increase from long-term
tidal gauges indicate that eustatic sea level
(overall mean global water level) rose 1-2
mm/year in the 20th century - SLR predicted to accelerate from the total of
20-30 cm seen in the 20th century to 35-90 cm
during the 21st century as a result of thermal
ocean water expansion and loss of land ice in
response to global warming (IPCC 2001 Michener
et al. 1997 Leatherman 2001 Kearney, 2001
Douglas 1992 Scavia et al. 2002)
25Sea Level Rise Scenarios - Louisiana
26Sea Level Rise Scenarios - Louisiana
27Sea Level Rise Scenarios - Louisiana
28Sea Level Rise Scenarios - Louisiana
29Sea Level Rise Scenarios - Louisiana
30Sea Level Rise Scenarios - Louisiana
31Sea Level Rise Scenarios - Louisiana
32Sea Level Rise Scenarios - Florida