Title: Future climate projections, Climate Sensitivity, and the "dangerous climate change"
1Future climate projections, Climate Sensitivity,
and the "dangerous climate change"
The IPCC AR4 2006 Report
V1003 - Science and Society
2Take away ideas
- Who What is the IPCC?
- What is Radiative Forcng?
- How much will climate warm from GHG emissions?
- Whats in the pipeline? Why?
- What is Climate Sensitivity?
- IPCC Scenarios and Projections
- How much CO2 emission is too much?
3Intergovernmental Panel on Climate Change (IPCC)
- Established by the UN and World Meteorological
Organization in 1988. - Role of the IPCC to assess the scientific,
technical, and socio-economic information
relevant for the understanding of the risks of
human-induced climate change. - Assessments based on published and peer-reviewed
literature
4IPCC Reports
- 2,500 of the worlds leading climate scientists
and technical experts contribute to reports - Provides comprehensive and balanced assessments
of climate change science, impacts, and
adaptation and mitigation options - Extensive peer-review and governmental review
ensures scientific credibility and policy
relevance - 1st report (FAR 1990)
- 2nd Report (SAR 1995)
- 3rd Report (TAR 2001)
- 4th Report (AR4 2007)
5IPCC Assessment report foci
1990
1995
2001
2007
6IPCC ReportsWriting, Review, Publication
7IPCC AR4 (2007)
1) GW Basis, 2) Impacts, 3) Mitigation
AR4 Volume 1 has the GW story - what did it say?
8An aside Skeptics on the offensive
- ExMo Offered 10,000 to scientists and economists
to discredit / challenge the IPCC AR4 report. - Skeptic IPCC report published at same time,
similar layout/appearance. - Sen. Inhofe (R, OK) Climate Hoax.
- Michael Crighton Climate of Fear conspiracy.
- Rep. Joe Barton (R, TX) Senate hearing /
intimidation of climate scientists (2006).
9Atmospheric CO2
CO2 (ppm)
CO2 has increased by about 30 Long term
average growth rate is 1.4 per year Last
decade growth rate is 2.0 per year What is
current CO2 level? When will CO2 double?
10What is Radiative Forcing?
- Radiative forcing is a measure of how the energy
balance of the Earth-atmosphere system is
influenced when factors that affect climate are
altered. - Radiative because these factors change the
balance between incoming solar radiation and
outgoing infrared radiation within the Earths
atmosphere. This radiative balance controls the
Earths surface temperature. - Forcing to indicate that Earths radiative
balance is being pushed away from its normal
state. - Measured in Watts per square meter (W/m2)
11All Radiative Forcing factors (1750-2005)
Sum 1.6 W/m2
12Radiative Forcing Contributions
- GHGs warm (CO2, CH4, N2O)
- H2O (vapor) warms
- Tropospheric O3 warms, Strat O3 cools
- Human and natural Aerosols cool
- Solar irradiance warms
- Net Effect 1.6 W/m2
13Current RF is equivalent to 1-2 mini-lights on
every square meter of the planet
Today 1.6 W/m2 Committed 1.6 0.7 2.3
W/m2 By 2100 6 to 7 W/m2
Jim Hansen 2004
14Natural and Human RF Forcing
15Why is there additional warming already in the
pipeline?
- The Earths energy balance, isnt.
- Earth isnt at equilibrium.
- Imbalance is 0.7 W/m2 (or about 0.4C), adds to
existing 1.6 W/m2 - This addl warming is there even if we shut off
emissions today.
16What is Climate Sensitivity?
- The equilibrium temperature change (in C) for
given radiative forcing (in W/m2) change. - Estimates based on basic radiative equations as
well as climate model - CS is about 0.5 C per W/m2 - But very uncertain
- Current climate 0.8C for 1.6 W/m2
- Future climate (2xCO2) _3_C for _6_ W/m2
17IPCC Emission Scenarios
- The A1 storyline and scenario family describes a
future world of very rapid economic growth, low
population growth, and the rapid introduction of
new and more efficient technologies. Major
underlying themes are convergence among regions,
capacity building, and increased cultural and
social interactions, with a substantial reduction
in regional differences in per capita income. - The A2 storyline and scenario family describes a
very heterogeneous world. The underlying theme is
self-reliance and preservation of local
identities. Fertility patterns across regions
converge very slowly, which results in high
population growth. Economic development is
primarily regionally oriented. - The B1 storyline and scenario family describes a
convergent world with the same low population
growth as in the A1 storyline, but with rapid
changes in economic structures toward a service
and information economy, with reductions in
material intensity, and the introduction of clean
and resource-efficient technologies. Global
solutions to economic, social, and environmental
sustainability, including improved equity, but
without additional climate initiatives. - The B2 storyline and scenario family describes a
world in which the emphasis is on local solutions
to economic, social, and environmental
sustainability. It is a world with moderate
population growth, intermediate levels of
economic development, and less rapid and more
diverse technological change than in the B1 and
A1 storylines. While the scenario is also
oriented toward environmental protection and
social equity, it focuses on local and regional
levels.
18Estimating the Future
- Can estimate future emissions using some
assumptions. - Need to know Climate Sensitivity.
- Use historical ?T and ?RF to estimate CS.
- Use physical models (Climate Models) to calculate
effects of GHGs and their feedbacks on global
climate. - 23 different models.
19SRES - Special Report Emissions Scenarios
2xCO2
450 ppm
20Current and 2xCO2 RF
21Radiative ForcingProjections
- Current (2005) forcing is 1.6 W/m2
- Committed Forcing is 1.6 0.7 2.3 W/m2
- By 2100 (2xCO2) Radiative Imbalance is 6 to 7
W/m2
Longwave forcing (GHG)
Shortwave forcing (Sun)
22IPCC AR4 Climate Projections
2xCO2 3C 2.0 - 4.5 C range
23(No Transcript)
24Dangerous Climate Change
- A future level of warming sufficiently great to
push climate to a tipping point. - What value should this be? A subjective call but
can be estimated. - Level 2C above modern temperatures
- Why? Warmer than any time in last three million
years (Pliocene) when world was considerably
warmer than today.
25Why Dangerous?
- Ice-albedo feedback
- Ice-sea-level feedback
- Salinity-Ocean circulation feedback
- Glacier-water supply link
- Hydrological shifts
- unknowns
26What CO2 level is this?
- Depends of Climate Sensitivity!
- Current estimate for this level is 450 ppm.
- Best guess is about 3010 years from now.
27Some perspective
- 450 ppm 570 Gt carbon
- Weve already emitted 300 Gt
- So only about 300 Gt more until the limit. At
the current emission rate, about 30-40 years. - Business-as-usual scenario 1600 Gt by 2100.
- Emission reductions prudent.
28QUIZ
- Why is Radiative Forcing?
- What is Climate Sensitivity?
- Why do they matter?