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Global Warming of 1.5°C
Valérie Masson-Delmotte
Co-Chair of IPCC Working Group I
valmasdel
Global Warming of 1.5°C
An IPCC special report on the impacts of
global warming of 1.5°C above pre-industrial
levels and related global greenhouse gas
emission pathways, in the context of
strengthening the global response to the
threat of climate change, sustainable
development, and efforts to eradicate
poverty.
The report in numbers
91 Authors from 40 Countries
133 Contributing authors
6000 Studies 1 113 Reviewers
42 001 Comments
Cumulative emissions of CO2 and future non-CO2 radiative forcing
determine the probability of limiting warming to 1.5°C
Faster immediate CO2 emission
reductions limit cumulative CO2
emissions
Maximum temperature rise is determined by cumulative net
CO2 emissions and net non-CO2 radiative forcing due to
methane, nitrous oxide, aerosols and other anthropogenic
forcing agents.
Spatial patterns of changes in mean temperature
26 CMIP5 models; hatching : 66% model agreement
Global warming of 1.5°C 2°C
Spatial patterns of changes in mean temperature and precipitation
26 CMIP5 models; hatching : 66% model agreement
Global warming of 1.5°C 2°C
Spatial patterns of changes in mean temperature and precipitation
26 CMIP5 models; hatching : 66% model agreement
Global warming of 1.5°C 2°C Difference
Spatial patterns of changes in extreme temperature
Number of hot days
(days)
Temperature of
hottest days (°C)
Temperature of
coldest nights (°C)
Global warming of 1.5°C 2°C
Spatial patterns of changes in extreme temperature and precipitation
Number of hot days
(days)
Temperature of
hottest days (°C)
Temperature of
coldest nights (°C)
Extreme
precipitation (%)
Global warming of 1.5°C 2°C
Spatial patterns of changes in extreme temperature and precipitation
Number of hot days
(days)
Temperature of
hottest days (°C)
Temperature of
coldest nights (°C)
Extreme
precipitation (%)
Global warming of 1.5°C 2°C Difference
Confidence level : M, medium; H, high; VH; very high
How do climate-related risks change
as a function of the level of global warming?
Confidence level : M, medium; H, high; VH; very high
How do climate-related risks for “Reasons For Concern” change
as a function of the level of global warming?
At 1.5°C compared to 2°C
• Up to several hundred million fewer people
exposed to climate-related risk and
susceptible to poverty by 2050
• Disproportionately high risk for Arctic,
dryland regions, small island developing
states and least developed countries
• Lower risks for health, livelihoods, food
security, water supply, human security and
economic growth
Jason Florio / Aurora Photos
• Wide range of adaptation options which can
reduce climate risks; less adaptation needs at
1.5°C
14
What are greenhouse gas emission pathways
compatible with limiting warming to 1.5°C?
https://data.ene.iiasa.ac.at/iamc-1.5c-explorer/
15
What are greenhouse gas emission pathways
compatible with limiting warming to 1.5°C?
16
What are greenhouse gas emission pathways
compatible with limiting warming to 1.5°C?
Limiting warming to 1.5°C
Would require rapid, far-reaching and
unprecedented changes in all systems
A range of technologies and behavioural changes
Scale up in annual investment in low carbon energy
and energy efficiency by factor of five by 2050
Mint Images / Aurora Photos
Renewables supply 70-85% of electricity in 2050
Coal declines steeply, ~zero in electricity by 2050
Deep emissions cuts in transport and buildings
Changes in land use and urban planning
Year
BilliontonsCO2peryear(GtCO2/yr)
Four illustrative model pathways
Agriculture, forestry, land use
Bioenergy with CCS
Fossil fuels and industry
Where are we?
• National pledges are not enough to limit
warming to 1.5°C
10
• Avoiding warming of more than 1.5°C
would require carbon dioxide emissions to
decline substantially before 2030
Peter Essick / Aurora Photos
• Different pathways have different synergies
and trade-offs with UN Sustainable
Development Goals (SDGs)
• Careful mix of measures to adapt to climate
change and reduce emissions can help
achieve SDGs
12
Ashley Cooper/ Aurora Photos
• Ethical and fair transitions
• Low energy demand, low material
consumption and low carbon food carry
highest benefits• Cooperation, governance, innovation and
mobilisation of finance key for feasibility
Climate change and sustainability
ipcc.ch/report/sr15 :
Summary for Policy Makers
10 Frequently Asked Questions
5 Chapters
Glossary
Chapter 1: Framing and context (integration WGI-WGII-III)
Chapter 2: Mitigation pathways compatible with 1.5°C in the context of
sustainable development (integration WGI-WGIII, pathways)
Chapter 3: Impacts of 1.5°C global warming on natural and human
systems (integration WGI-WGII, global – regional)
Chapter 4: Strengthening and implementing the global response to the
threat of climate change (systems transitions, dimensions of feasibility)
Chapter 5: Sustainable development, poverty eradication and reducing
inequalities (ethics, equity, societal transformation, SDGs)
Global warming of 1.5°C (SR1.5)

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4 December - From SR15 to Synthesis Report - Global Warming of 1.5°C

  • 1. Global Warming of 1.5°C Valérie Masson-Delmotte Co-Chair of IPCC Working Group I valmasdel
  • 2. Global Warming of 1.5°C An IPCC special report on the impacts of global warming of 1.5°C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change, sustainable development, and efforts to eradicate poverty.
  • 3. The report in numbers 91 Authors from 40 Countries 133 Contributing authors 6000 Studies 1 113 Reviewers 42 001 Comments
  • 4. Cumulative emissions of CO2 and future non-CO2 radiative forcing determine the probability of limiting warming to 1.5°C Faster immediate CO2 emission reductions limit cumulative CO2 emissions Maximum temperature rise is determined by cumulative net CO2 emissions and net non-CO2 radiative forcing due to methane, nitrous oxide, aerosols and other anthropogenic forcing agents.
  • 5. Spatial patterns of changes in mean temperature 26 CMIP5 models; hatching : 66% model agreement Global warming of 1.5°C 2°C
  • 6. Spatial patterns of changes in mean temperature and precipitation 26 CMIP5 models; hatching : 66% model agreement Global warming of 1.5°C 2°C
  • 7. Spatial patterns of changes in mean temperature and precipitation 26 CMIP5 models; hatching : 66% model agreement Global warming of 1.5°C 2°C Difference
  • 8. Spatial patterns of changes in extreme temperature Number of hot days (days) Temperature of hottest days (°C) Temperature of coldest nights (°C) Global warming of 1.5°C 2°C
  • 9. Spatial patterns of changes in extreme temperature and precipitation Number of hot days (days) Temperature of hottest days (°C) Temperature of coldest nights (°C) Extreme precipitation (%) Global warming of 1.5°C 2°C
  • 10. Spatial patterns of changes in extreme temperature and precipitation Number of hot days (days) Temperature of hottest days (°C) Temperature of coldest nights (°C) Extreme precipitation (%) Global warming of 1.5°C 2°C Difference
  • 11. Confidence level : M, medium; H, high; VH; very high How do climate-related risks change as a function of the level of global warming?
  • 12. Confidence level : M, medium; H, high; VH; very high How do climate-related risks for “Reasons For Concern” change as a function of the level of global warming?
  • 13. At 1.5°C compared to 2°C • Up to several hundred million fewer people exposed to climate-related risk and susceptible to poverty by 2050 • Disproportionately high risk for Arctic, dryland regions, small island developing states and least developed countries • Lower risks for health, livelihoods, food security, water supply, human security and economic growth Jason Florio / Aurora Photos • Wide range of adaptation options which can reduce climate risks; less adaptation needs at 1.5°C
  • 14. 14 What are greenhouse gas emission pathways compatible with limiting warming to 1.5°C? https://data.ene.iiasa.ac.at/iamc-1.5c-explorer/
  • 15. 15 What are greenhouse gas emission pathways compatible with limiting warming to 1.5°C?
  • 16. 16 What are greenhouse gas emission pathways compatible with limiting warming to 1.5°C?
  • 17. Limiting warming to 1.5°C Would require rapid, far-reaching and unprecedented changes in all systems A range of technologies and behavioural changes Scale up in annual investment in low carbon energy and energy efficiency by factor of five by 2050 Mint Images / Aurora Photos Renewables supply 70-85% of electricity in 2050 Coal declines steeply, ~zero in electricity by 2050 Deep emissions cuts in transport and buildings Changes in land use and urban planning
  • 18. Year BilliontonsCO2peryear(GtCO2/yr) Four illustrative model pathways Agriculture, forestry, land use Bioenergy with CCS Fossil fuels and industry
  • 19. Where are we? • National pledges are not enough to limit warming to 1.5°C 10 • Avoiding warming of more than 1.5°C would require carbon dioxide emissions to decline substantially before 2030 Peter Essick / Aurora Photos
  • 20. • Different pathways have different synergies and trade-offs with UN Sustainable Development Goals (SDGs) • Careful mix of measures to adapt to climate change and reduce emissions can help achieve SDGs 12 Ashley Cooper/ Aurora Photos • Ethical and fair transitions • Low energy demand, low material consumption and low carbon food carry highest benefits• Cooperation, governance, innovation and mobilisation of finance key for feasibility Climate change and sustainability
  • 21. ipcc.ch/report/sr15 : Summary for Policy Makers 10 Frequently Asked Questions 5 Chapters Glossary
  • 22. Chapter 1: Framing and context (integration WGI-WGII-III) Chapter 2: Mitigation pathways compatible with 1.5°C in the context of sustainable development (integration WGI-WGIII, pathways) Chapter 3: Impacts of 1.5°C global warming on natural and human systems (integration WGI-WGII, global – regional) Chapter 4: Strengthening and implementing the global response to the threat of climate change (systems transitions, dimensions of feasibility) Chapter 5: Sustainable development, poverty eradication and reducing inequalities (ethics, equity, societal transformation, SDGs) Global warming of 1.5°C (SR1.5)

Editor's Notes

  1. This figure uses stylized emission and forcing pathways to show key factors affecting the prospects of temperatures remaining below 1.5°C. Panel b) CO2 emissions decline from 2020 to reach net zero in 2055 (grey) or 2040 (blue). Faster immediate CO2 reductions limit cumulative CO2 emissions shown in (c) Panel c) Cumulative CO2 emissions in pathways reaching net zero in 2055 (grey) and 2040 (blue) Panel d): Non-CO2 radiative forcing reduced after 2030 (grey) or not reduced after 2030 (purple)
  2. Revised upward risk for Arctic sea ice loss / level of warming. Particularly high risk of major ecosystems (biome shifts) (tundra). Permafrost. Benefits for Arctic fisheries productivity but risk of loss of habitat (seals, sea birds, whales, polar bears). Over land 0.5°C global mean 2-2.5°C local.Risks over land : fire, permafrost, biome shifts, tree cover increase. Cold extremes (winter, night) warm by 4-8°C for 2°C global warming over Arctic land.
  3. Investments in infrastructures for adaptation and mitigation