Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC...

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Climate change: The latest Climate change: The latest science science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology

Transcript of Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC...

Page 1: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Climate change: The latest scienceClimate change: The latest scienceClimate change: The latest scienceClimate change: The latest science

David KarolySchool of Earth Sciences, University of Melbourne

TC Larry, 2006From Bureau of Meteorology

Page 2: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Introduction• Different perspectives on climate change

• The latest assessment of climate change and its

causes - IPCC 2007

• Updates since 2007

• Climate change misinformation

• International agreements and stabilising climate

change

Page 3: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Global warming alarmism?

Page 4: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Garnaut Climate Change Review (2008) concluded

• Climate change is a diabolical policy problem • Australia has a larger interest in a strong mitigation

outcome than other developed countries

• We are already a hot and dry country; small variations in climate are more damaging to us than to other developed countries.

Page 5: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Senator Fielding’s views• “The Rudd Government is yet to prove that man-made

carbon dioxide emissions are the main driver behind climate change”

Page 6: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

?

Page 7: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Intergovernmental Panel on Climate Change (IPCC)

• Joint body of UN Environment Program and World Meteorological Organization, established in 1988

• Every 5-6 years, carries out a comprehensive assessment of climate change science, impacts, and approaches for mitigation and adaptation to climate change

• Includes representatives from all countries• Fourth Assessment Report prepared by more than 500

scientists over the last three years• Summaries for Policy Makers approved by consensus

(including representatives of the Australian govt) at meetings in Paris (Feb 07), Brussels (Apr 07) and Bangkok (May 07)

• Received the 2007 Nobel Peace Prize jointly with Al Gore

Page 8: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

‘Warming of the climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global average sea level.’ (IPCC 2007)

Fi gure SPM. 3

WGI Fig SPM.3

Page 9: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

‘Global atmospheric concentrations of carbon dioxide, methane and nitrous oxide have increasedmarkedly as a result of human activities since 1750 and now far exceed pre-industrial valuesdetermined from ice cores spanning many thousands of years.

The global increasesin carbon dioxide concentration are due primarily to fossil fuel use and land-use change, while those ofmethane and nitrous oxide are primarily due to agriculture.’

Fi gure SPM. 1WGI Fig SPM.1

Page 10: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Causes of climate changeIn 2005, greenhouse gas concentration was 455 ppm CO2-eq. A large part of the warming influence is masked by aerosols.

WGI Fig SPM.2

Page 11: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Climate modelling• Physically-based tools for studying climate variability

and change • Use mathematical representations of physical laws,

including Newton's second law of motion, the laws of conservation of mass and energy, laws of thermodynamics, and the ideal gas law

• Represent important processes in atmosphere, ocean, land surface and ice, as well as coupling between them

• More than twenty different models developed independently around the world

Page 12: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Annual mean precipitation

Observations 1980-99

Multi-model ensemble mean, 1980-99

WGI Fig 8.4

Page 13: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

‘Most of the observed increase in global average temperatures since the mid-20th century is very likely (more than 90% certain) due to the observed increase in anthropogenic greenhouse gas concentrations.’ IPCC(2007)

Fi gure TS. 23

WGI Fig TS.23

Page 14: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.
Page 15: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

‘Continued greenhouse gas emissions at or above current rates would cause further warming and induce many changes in the global climate system during the 21st century that would very likely be larger than those observed during the 20th century.’

WGI Fig SPM.5

Page 16: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

‘There is now higher confidence in projected patterns of warming and other regional-scale features, including changes in circulation patterns, precipitation, and some aspects of extremes and of ice.’

• It is very likely that hot extremes, heat waves, and heavy precipitation events will continue to become more frequent.

• Snow cover is projected to contract. Sea ice is projected to shrink in both the Arctic and Antarctic.

• Storm tracks are projected to move poleward, with changes in wind, precipitation, and temperature patterns.

• Increasing atmospheric CO2 concentrations lead to increasing acidification of the ocean.

• 21st century anthropogenic CO2 emissions will contribute to warming and sea level rise for more than a millennium, due to the long timescales required for removal of this gas.

Page 17: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Projected climate change hotspots in Australia (from IPCC AR4 WGII, chapt 11)

Page 18: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.
Page 19: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

From Stroeve et al, GRL, 2007

Observations to 2005

Page 20: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Sea ice in Sept 2007

From Stroeve et al, GRL, 2007

Sept 2005

Page 21: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Observed and projected Australian rainfall

Best estimate projected rainfall change for 2070(from “Climate change in Australia”)

Observed trend in annual rainfall

1960-2008

Page 22: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Recent emissions

1990 1995 2000 2005 2010

5

6

7

8

9

10Actual emissions: CDIACActual emissions: EIA450ppm stabilisation650ppm stabilisationA1FI A1B A1T A2 B1 B2

1850 1900 1950 2000 2050 2100

0

5

10

15

20

25

30Actual emissions: CDIAC450ppm stabilisation650ppm stabilisationA1FI A1B A1T A2 B1 B2

Global CO2 emissions from fuel consumptionComparison of IPCC emission scenarios and new growth path

From Raupach et al. 2007, PNAS

SRES (2000) growth rates in % y -1 for 2000-2010:

A1B: 2.42 A1FI: 2.71A1T: 1.63A2: 2.13B1: 1.79B2: 1.61

20062005

Observed

2000-2006 3.3%/yr

Page 23: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Causes of climate changeMyth: The observed warming has been due to variations in solar forcing

1. Increases in solar irradiance would cause warming in the upper atmosphere and lower atmosphere, but cooling in the upper atmosphere has been observed

From the Hadley Centre (UK) www.hadobs.org

Page 24: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Fi gure 3. 2

Causes of climate changeMyth: The observed warming has been due to variations in solar forcing

2. Increases in solar irradiance would cause more warming in summer than winter, and in daytime than nighttime, but the opposite is observed

IPCC AR4 WGI Fig 3.2

Page 25: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Figure 2.16

Causes of climate changeMyth: The observed warming has been due to variations in solar forcing associated with the solar sunspot cycle

Wrong! 1) Satellite observations show significant changes in solar irradiance due to the 11-year sunspot cycle, but no long term trend. However, global temperatures show a warming trend but no 11-year cycle.

IPCC WGI Fig 2.16

Page 26: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Causes of climate changeMyth: Changes in cosmic rays have caused changes in cloudiness, leading to global warming

No! Large 11-year cycle in cosmic ray activity, but no recent trend

No clear link between cosmic rays and clouds, as there are plenty of CCN (cloud condensation nuclei) in many regions

Page 27: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Climate variations over the last milleniumMyth: The medieval warm period was warmer than present

Wrong! Multiple climate reconstructions show “the warmth of the last half century is unusual in at least the previous 1300 years.”

Figure TS.20

WGI Fig TS.20

Reconstructions of NH average temperature

Page 28: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Recent observed global mean temperatureMyth: Global average temperature has cooled since 1998

Wrong! No significant warming or cooling, due to short period. 1998 the hottest year globally, due to El Niño event, and recent cooling due to La Niña in 2007 and 2008. Rapid recent warming.

Long term warming, with the 2000’s the warmest decade

Page 29: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

UN Framework Convention on Climate Change (UNFCCC)

• Established following the United Nations conference on Environment and Development in Rio de Janeiro in 1992

• Objective is “stabilization of greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system”

• “Such a level should be achieved within a time frame sufficient to allow ecosystems to adapt naturally to climate change, to ensure that food production is not threatened, and to enable economic development to proceed in a sustainable manner”

• Ratified by 192 countries, including USA and Australia, and came into force in March 1994

Page 30: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Who has caused the problem?UNFCCC includes principle that: “Parties should protect the climate system...on the basis of equity and in accordance with their common but differentiated responsibilities and respective capabilities. Accordingly, the developed country Parties should take the lead in combating climate change” (UNFCCC, Art.3.1).

Regional greenhouse gas emissions in 2004

SyR Fig 2.2a

Page 31: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Stabilisation scenarios• 455 ppm CO2-eq in 2005, 379 ppm CO2 conc

• I: CO2-eq stabilisation at 445-490 ppm, emissions peak in 2000-2015, global CO2 emissions -85% to -50% in 2050, warming of 2.0 to 2.4C above pre-industrial

• Assuming equal per capita emissions, 50% global emission reduction in 2050 means ~90% emission reduction for Australia

IPCC SyR Fig SPM.11

Page 32: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Probability distribution of committed global warming (relative to preindustrial) for greenhouse gases in the atmosphere in 2005

From Ramanathan and Feng, PNAS, 2008

Page 33: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

From www.nicholsoncartoons.com.au

Page 34: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

Key messages, Climate Change: Global Risks, Challenges & Decisions, Copenhagen in March 2009

• Recent observations confirm that, given high rates of observed emissions, the worst-case IPCC scenario trajectories (or even worse) are being realized

• Recent observations show that societies are highly vulnerable to even modest levels of climate change, with poor nations and communities particularly at risk.

• Rapid, sustained, and effective mitigation based on coordinated global and regional action is required to avoid "dangerous climate change" regardless of how it is defined.

• Delay in initiating effective mitigation actions increases significantly the long-term social and economic costs of both adaptation and mitigation

Page 35: Climate change: The latest science David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.

References• IPCC web site http://www.ipcc.ch/

• US GCRP “Climate literacy: The essential principles of climate sciences” http://www.globalchange.gov/resources/educators/climate-literacy

• Climate change in Australia site http://www.climatechangeinaustralia.gov.au/

• Climate Works Australia FAQ on climate science http://www.climateworksaustralia.com/Q_and_A.pdf

My contact information: Prof David Karoly, School of Earth Sciences, [email protected]