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Climate change:
overview and update

        Andy Reisinger
   Climate Change Research Institute




                      New Zealand Climate
                      Change Research Institute
Warming is unequivocal and widespread
•   Global average atmospheric temperatures increasing
•   Extreme temperatures increasing
•   Ocean heat content increasing …
•   … now directly linked to sea level rise
•   Greenland and Antarctic Ice Sheets losing mass
•              Unequivocal
    Glaciers and snow cover declining
•   Arctic sea ice extent decreasing
•   Area of seasonally frozen ground decreasing
•   Atmospheric water vapour content increasing
•   More intense and longer droughts
•   More frequent heavy precipitation events over land
•   Tropical cyclone intensity increasing (in North Atlantic)
                                                                2
Recent warming is due to greenhouse gases

                                                   Models reproduce
                                                   observed changes
                                                   only if we include the
                                                   warming effect of
                                                   greenhouse gases




                                                   Combination of
                                                   volcanic eruptions
                                                   and solar change
                                                   would have resulted
                                                   in small cooling over
                                                   the last 50 years




            Figure source: IPCC WGI Figure SPM.4                            3
Future warming depends on emissions




    Figure source: based on IPCC WGI Figure SPM.5 and Third Assessment Report   4
Projected warming – does it matter?


 Even at the lower end of future scenarios, the global
 rate of change over the 21st century will almost
 certainly be greater than experienced by human
 civilisation over the past 10,000 years

 Changes greater over land and more variable

 We can no longer stop global warming, but reducing
 emissions would reduce its rate and magnitude




          Figure source: based IPCC WGI Figures 6.10 and Figure SPM.5   5
Global impacts of climate change




Source: IPCC WGII Table TS.5
                                            6
Settingemissions targets
                            reductions: policy
                            Stringent



                               450ppm CO2-eq

                               2° relative to pre-
                                 C
                               industrial temperatures



Adaptation is necessary:                                 Mitigation is necessary:
manage unavoidable change                                avoid unmanageable change




Source: IPCC WGII Table TS.5
                                                                                     7
Global greenhouse gas emissions




         Figure source: IPCC WGII Figure 1.1   8
Emissions reductions

• Each sector has options to reduce emissions

• The more we want to reduce emissions, the more
  we have to include all sectors and all
  opportunities

• Achieving emissions reductions requires:
   • a price on emissions that makes the use of
     alternative technologies attractive
   • policies that support change in behaviour and the
     development and deployment of new technologies


                                                         9
Example electricity sector




Emissions of CO2 eventually have to reduce to zero to
      stabilise greenhouse gas concentrations.
This requires research to develop new technologies,
     reduce costs and increase feasibility/scale.


    Figure: based on data from IPCC WGIII Figures 4.29, 4.30 and Tables 4.6, 6.7, 7.5   10
How does NZ compare? – income growth
35.00%

                   World
30.00%             United States of America
                   European Union (27)

25.00%             New Zealand



20.00%


15.00%


10.00%


5.00%


0.00%
     1990   1992           1994          1996   1998         2000         2002         2004   2006

-5.00%


            Income in purchasing power parity relative to 1990. Source: cait.wri.org             11
How does NZ compare? – CO2 emissions
70.00%


60.00%          World
                United States of America
                European Union (27)
50.00%
                New Zealand


40.00%


30.00%


20.00%


10.00%


 0.00%
      1990   1992          1994        1996        1998        2000         2002    2004   2006

-10.00%


                    Domestic CO2 emissions relative to 1990. Source: cait.wri.org             12
Scale of emissions reductions
• Stabilising concentrations at 450ppm CO2-eq:
   • Developed countries reduce their emissions by 25-40% by
     2020, and 80-95% by 2050, relative to 1990 emissions
   • Developing countries reduce their emissions by 10-30%
     below business-as-usual by 2020 and much more
     substantial reductions by 2050. The most advanced
     developing countries would need to do more.

• Stabilising concentrations at 450ppm CO2-eq gives
  us only a 50/50 chance of not exceeding 2° !
                                            C

• Delays or less stringent targets increase greenhouse
  gas concentrations further and increase the risk of
  serious and irreversible climate damages
                                                               13
Latest updates
• Failure to make international progress would mean that we
  are about to loose the chance to limit warming to 2°C.

• If everybody on the planet were allowed the same per capita
  emissions, and we wish to limit global warming to 2° then
                                                      C,
  New Zealanders will exhaust their emissions allowance
  (even counting CO2 only !) by about 2020

• Polar ice sheets are loosing ice faster than predicted by ice
  sheet models. Glaciers that drain the ice sheets are
  accelerating with warming, leading to faster sea level rise.

• Recent studies suggest that sea level could rise by more
  than 1m by 2100, and even 2m cannot be ruled out entirely
  for scenarios without stringent emissions reductions

                                                                  14

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Climate change overview and impacts

  • 1. Climate change: overview and update Andy Reisinger Climate Change Research Institute New Zealand Climate Change Research Institute
  • 2. Warming is unequivocal and widespread • Global average atmospheric temperatures increasing • Extreme temperatures increasing • Ocean heat content increasing … • … now directly linked to sea level rise • Greenland and Antarctic Ice Sheets losing mass • Unequivocal Glaciers and snow cover declining • Arctic sea ice extent decreasing • Area of seasonally frozen ground decreasing • Atmospheric water vapour content increasing • More intense and longer droughts • More frequent heavy precipitation events over land • Tropical cyclone intensity increasing (in North Atlantic) 2
  • 3. Recent warming is due to greenhouse gases Models reproduce observed changes only if we include the warming effect of greenhouse gases Combination of volcanic eruptions and solar change would have resulted in small cooling over the last 50 years Figure source: IPCC WGI Figure SPM.4 3
  • 4. Future warming depends on emissions Figure source: based on IPCC WGI Figure SPM.5 and Third Assessment Report 4
  • 5. Projected warming – does it matter? Even at the lower end of future scenarios, the global rate of change over the 21st century will almost certainly be greater than experienced by human civilisation over the past 10,000 years Changes greater over land and more variable We can no longer stop global warming, but reducing emissions would reduce its rate and magnitude Figure source: based IPCC WGI Figures 6.10 and Figure SPM.5 5
  • 6. Global impacts of climate change Source: IPCC WGII Table TS.5 6
  • 7. Settingemissions targets reductions: policy Stringent 450ppm CO2-eq 2° relative to pre- C industrial temperatures Adaptation is necessary: Mitigation is necessary: manage unavoidable change avoid unmanageable change Source: IPCC WGII Table TS.5 7
  • 8. Global greenhouse gas emissions Figure source: IPCC WGII Figure 1.1 8
  • 9. Emissions reductions • Each sector has options to reduce emissions • The more we want to reduce emissions, the more we have to include all sectors and all opportunities • Achieving emissions reductions requires: • a price on emissions that makes the use of alternative technologies attractive • policies that support change in behaviour and the development and deployment of new technologies 9
  • 10. Example electricity sector Emissions of CO2 eventually have to reduce to zero to stabilise greenhouse gas concentrations. This requires research to develop new technologies, reduce costs and increase feasibility/scale. Figure: based on data from IPCC WGIII Figures 4.29, 4.30 and Tables 4.6, 6.7, 7.5 10
  • 11. How does NZ compare? – income growth 35.00% World 30.00% United States of America European Union (27) 25.00% New Zealand 20.00% 15.00% 10.00% 5.00% 0.00% 1990 1992 1994 1996 1998 2000 2002 2004 2006 -5.00% Income in purchasing power parity relative to 1990. Source: cait.wri.org 11
  • 12. How does NZ compare? – CO2 emissions 70.00% 60.00% World United States of America European Union (27) 50.00% New Zealand 40.00% 30.00% 20.00% 10.00% 0.00% 1990 1992 1994 1996 1998 2000 2002 2004 2006 -10.00% Domestic CO2 emissions relative to 1990. Source: cait.wri.org 12
  • 13. Scale of emissions reductions • Stabilising concentrations at 450ppm CO2-eq: • Developed countries reduce their emissions by 25-40% by 2020, and 80-95% by 2050, relative to 1990 emissions • Developing countries reduce their emissions by 10-30% below business-as-usual by 2020 and much more substantial reductions by 2050. The most advanced developing countries would need to do more. • Stabilising concentrations at 450ppm CO2-eq gives us only a 50/50 chance of not exceeding 2° ! C • Delays or less stringent targets increase greenhouse gas concentrations further and increase the risk of serious and irreversible climate damages 13
  • 14. Latest updates • Failure to make international progress would mean that we are about to loose the chance to limit warming to 2°C. • If everybody on the planet were allowed the same per capita emissions, and we wish to limit global warming to 2° then C, New Zealanders will exhaust their emissions allowance (even counting CO2 only !) by about 2020 • Polar ice sheets are loosing ice faster than predicted by ice sheet models. Glaciers that drain the ice sheets are accelerating with warming, leading to faster sea level rise. • Recent studies suggest that sea level could rise by more than 1m by 2100, and even 2m cannot be ruled out entirely for scenarios without stringent emissions reductions 14