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Chairman, Intergovernmental 
Panel on Climate Change 
Media Training Workshop in Preparation for the 
COP20 
Understanding the Science of Climate Change 
R. K. Pachauri 
16 October 2014, Lima, Perú
Human influence on the climate system is 
clear and has been detected in warming of 
the atmosphere and the ocean, in changes 
in the global water cycle, in reductions in 
snow and ice, in global mean sea level rise, 
and in changes in some climate extremes. 
- IPCC AR5 Working Group I 
Source : IPCCAR5
3 
The IPCC Fifth Assessment Report 
A clear and up to date view of the current state of scientific knowledge relevant to 
climate change. 
Working group I 
The Physical Science Basis 
 259 authors 
 39 countries 
 54,677 comments 
 2 million gigabytes of 
numerical data from 
climate model 
simulations 
 Over 9200 scientific 
publications cited 
Working Group II 
Impacts, Adaptation and 
Vulnerability 
 309 authors 
 70 countries 
 50,444 comments 
 Over 12,000 scientific 
references cited 
Working Group III 
Mitigation of Climate 
Change 
 235 authors 
 57 countries 
 38,315 comments 
 Close to 1200 scenarios 
of socioeconomic 
development analyzed 
 Close to 10,000 
references to literature 
The Synthesis Report will be released in Copenhagen on 2nd November 
2014 
Source : IPCC AR5
4 
Observed changes in the climate system 
Climate change is unequivocal 
Source : IPCC AR5 
• The oceans have warmed and risen 
• The amounts of snow and ice have 
diminished 
• Sea level has risen 
• The concentrations of greenhouse 
gases have increased
5 
Human influence of the climate system is clear 
Understanding the causes 
• 95% certainty that human influence 
has been the dominant cause of the 
observed warming since the mid-20th 
century 
• Since the 1950s, many of the 
observed changes are unprecedented 
over decades to millennia. 
• Limiting climate change will require 
sustained and substantial reductions 
in greenhouse gas emissions 
Source : IPCC AR5 
Source : IPCC AR5
6 
Trends in GHGs and their drivers 
Total anthropogenic GHG emissions were the highest in human history from 
2000 to 2010 
Greenhouse gas emissions by economic sectors 
Source : IPCC AR5 
• Globally, economic and 
population growth continue 
to be the most important 
drivers of increases in CO2 
emissions from fossil fuel 
combustions 
• These are expected to 
continue to drive emissions 
growth without additional 
efforts to reduce GHG 
emissions.
7 
Observed climate change in Perú 
In CA and SA, decadal variability and changes in extremes have been affecting large sectors 
of the population, especially those more vulnerable and exposed to climate hazards. 
• Strong negative precipitation trends and 
warming detected in the Mantaro Valley, 
Perú 
• Air temperature increases in the southern 
Andes of Perú (1964-2006) 
• In the Peruvian western Amazonia, mean 
rainfall for 1964–2003 has decreased 
• Rapid retreat and melting of the tropical 
Andes glaciers of Venezuela, Colombia, 
Ecuador, Perú and Bolivia 
• 7 out of 9 river basins have probably 
crossed a critical threshold, exhibiting a 
decreasing dry-season discharge in the 
Cordillera Blanca of Perú 
Source : IPCC AR5
Extreme events during and by the end of the 21st Century 
• It is very likely that the length, frequency, and/or 
Source : IPCC SREX 
intensity of warm spells or heat waves will increase over 
most land areas 
• Under some scenarios, a 1-in-20 year hottest day is likely 
to become a 1-in-2 year event in most regions 
• It is likely that the frequency of heavy precipitation or the 
proportion of total rainfall from heavy falls will increase 
over many areas of the globe
9 
Future changes in the climate system 
Warming will continue beyond 2100 under all RCP scenarios except RCP2.6. 
Global surface 
temperature 
change for the end 
of the 21st century: 
 is likely to exceed 1.5°C relative to 1850 to 
1900 for all RCP scenarios except RCP2.6. 
 is likely to exceed 2°C for RCP6.0 and 
RCP8.5 
 is more likely than not to exceed 2°C for 
Source : IPCC AR5 RCP4.5.
10 
Abrupt and irreversible impacts 
Most aspects of climate change will persist for many centuries even if emissions of CO2 
are stopped. 
• Sustained mass loss by ice sheets 
(some of which irreversible) would 
cause larger sea level rise. 
• Sustained warming greater than some 
threshold (greater than about 1°C but 
less than about 4°C global mean 
warming with respect to pre-industrial) 
would lead to the near-complete 
loss of the Greenland ice 
sheet over a millennium or more, 
causing a global mean sea level rise of 
up to 7 m. 
Source : IPCC AR5
11 
Impacts on food security 
All aspects of food security are potentially affected by climate change, including food access, 
utilization, and price stability. Impacts will occur in the context of rapidly rising crop demand. 
• Projected negative 
impacts for production of 
wheat, rice and maize for 
local temperature 
increases of 2°C or more 
above late-20th-century 
levels, without adaptation. 
• Redistribution of marine 
fisheries catch potential 
poses risk of reduced 
supplies, income, and 
employment. 
Source : IPCC AR5
12 
Impacts on human health 
Throughout the 21st century, climate change is expected to lead to increases in ill-health 
in many regions and especially in developing countries with low income. 
Increased likelihood of: 
• Injury, disease, and 
death due to more 
intense heat waves and 
fires. 
• Under-nutrition from 
diminished food 
production in poor 
regions. 
• Risks from food- and 
water- and vector-borne 
diseases. 
Source : IPCC AR5
13 
Impacts on human security 
Climate change over the 21st 
century can increase: 
• Displacement of people, 
particularly in developing 
countries with low income. 
• Risks of violent conflicts by 
amplifying poverty and 
economic shocks. 
• Rivalry among states due to 
potential transboundary 
impacts of climate change, 
such as changes in sea ice, 
shared water resources, and 
pelagic fish stocks. 
Source : IPCC AR5
14 
Impacts of climate change on urban areas 
Climate change will have profound impacts on a broad spectrum of city functions, 
infrastructure and services and will interact with and may exacerbate many existing stresses. 
Source : IPCC AR5 
• The risks: rising sea levels, 
storm surges, heat stress, 
extreme precipitation, flooding, 
landslides, drought, increased 
aridity, water scarcity and air 
pollution. 
• Risks can have widespread 
negative impacts on people, 
economies and ecosystems 
• Risks are amplified for those 
who live in informal settlements 
with inadequate provision for 
adaptation
15 
Projected impacts in Perú 
• 2%–30% annual discharge decrease in 
the Santa River once the glaciers are 
completely melted 
• Projections estimate impacts of 
glacier melt to between US$212 
million to US$ 1.5 billion due to losses 
of hydropower generation 
• Perú is one of the most vulnerable 
countries to climate change impacts 
on fisheries (due to warming, species 
shift, importance of fisheries to the 
national economy and diet) 
• Climate change may alter plant 
diseases and potato late blight 
severity is expected to increase in 
Perú 
Source : IPCC AR5
16 
Implications for development 
Climate-related hazards exacerbate other stressors, often with negative outcomes for 
livelihoods, especially for people living in poverty. 
Throughout the 21st century, 
climate-change impacts are 
projected to: 
• Slow down economic growth 
• Make poverty reduction more 
difficult 
• Further erode food security 
• Prolong existing and create 
new poverty traps, particularly 
in urban areas and emerging 
hotspots of hunger 
Source : IPCC AR5
17 
Fatalities are higher in developing countries 
From 1970-2008, over 95% of natural-disaster-related deaths occurred in 
developing countries 
Source : IPCC SREX
18 
Adaptation and Mitigation 
“Climate-resilient pathways 
combine adaptation and 
mitigation to reduce climate 
change and its impacts. Since 
mitigation reduces the rate 
and magnitude of warming, 
it also increases the time 
available for adaptation to a 
particular level of climate 
change, potentially by 
several decades.” 
IPCC Fifth Assessment Report 
Source : IPCC AR5
19 
There are strategies that can help manage disaster risk now and 
also help improve people’s livelihoods and well-being 
The most effective strategies offer development benefits in the relatively near 
term and reduce vulnerability over the longer term 
Source : IPCC SREX
20 
Effective risk management and adaptation are tailored to local and 
regional needs and circumstances 
• Changes in climate extremes vary across regions 
• Each region has unique vulnerabilities and exposure to hazards 
• Effective risk management and adaptation address the factors contributing to exposure and 
vulnerability 
Source : IPCC SREX
21 
Adaptation experience in Perú 
• Constitutional and legal reforms for more 
efficient water resources management in 
coordination between 7 countries in SA 
and CA including Perú; but further 
implementation is required 
• The management of ENSO-related events 
in Perú via participatory or risk reduction 
approaches 
• Crop diversification in the Peruvian Andes 
to suppress pest outbreaks and pathogen 
transmission 
• Address constraints on access to key 
resources for reducing vulnerability, as 
shown by studies with indigenous farmers 
in highland Perú 
Source : IPCC AR5
22 
Impacts of mitigation on GDP growth 
Delaying additional mitigation further increases mitigation costs in the 
medium to long term 
2030 Time 
GDP 
Current 
GDP without 
mitigation 
GDP with stringent 
mitigation (reaching ≈ 
450 ppm CO2eq in 
2100) 
Loss in global 
consumption 
in 2030: 1.7% 
(median) 
Source : IPCC AR5 
Loss in 
global 
consumption 
in 2050: 
3.4% 
(median) 
Loss in global 
consumption 
in 2100: 4.8% 
(median) 
2050 2100
23 
Stringent mitigation scenarios 
Characteristics of scenarios reaching levels of about 450 ppm CO2eq by 2100 (likely 
chance to keep temperature change below 2C relative to preindustrial levels): 
• Lower global GHGs in 2050 than in 2010 (40% 
to 70% lower globally) 
• Emissions levels near zero GtCO2eq or below 
in 2100 
• More rapid improvements in energy 
efficiency 
• A tripling to nearly a quadrupling of the share 
of energy supply from renewables by 2050 
• Many scenarios reaching 450, 500 and 550 
ppm CO2eq by 2100 require widespread 
deployment of BECCS, afforestation, and 
other CDR technologies post 2050 
Source : IPCC AR5
24 
RE costs are still higher than existing energy prices but in various 
settings RE is already competitive. 
Source : IPCC SRREN
25 
Co-benefits 
The intersections of mitigation and adaptation with other societal goals, if well managed, 
can strengthen the basis for undertaking climate action: 
• Improved energy efficiency and 
security 
• Cleaner energy sources 
• Air quality and human health 
• Reduced energy and water 
consumption in urban areas 
• Sustainable agriculture and forestry 
• Protection of ecosystems for carbon 
storage 
Source : IPCC AR5
26 
Integration of climate change into policies 
• C40 Cities- Climate Leadership 
Group (ICLEI) and Lima’s 
Metropolitan Strategy to CCA 
• Growing awareness of CA and SA 
governments on the need to 
integrate climate change and 
future climate risks in their 
policies 
• 18 regional Non-Annex countries, 
including Perú have already 
published their 1st and/or 2nd 
National Communication to the 
UNFCCC allowing to measure 
their emissions and to assess their 
present and future vulnerability. 
Source : IPCC AR5
27 
Climate change and sustainable development 
Governing a transition toward an effective climate response and sustainable 
development pathway is a challenge involving rethinking our relation to nature. 
• A stable climate is one component 
of sustainable development. 
• Designing an effective climate policy 
involves “mainstreaming” climate in 
the design of sustainable 
development strategies. 
• Behaviour, lifestyle and culture can 
substantially contribute to lowering 
emissions: 
• Changes in consumption 
patterns 
• Dietary changes 
• Reduction in food wastes 
Source : IPCC AR5
28 
Climate change and equity 
Limiting the effects of climate change is necessary to achieve SD and equity, including 
poverty eradication. 
Issues of equity, justice, and fairness arise with 
respect to mitigation and adaptation: 
• Different past and future contributions to the 
accumulation of GHGs in the atmosphere 
• Varying challenges and circumstances 
• Different capacities to address mitigation and 
adaptation. 
Options for equitable burden-sharing can reduce 
the potential for the costs of climate action to 
constrain development. 
Equitable outcomes can lead to more effective 
cooperation 
Source : IPCC AR5
“A technological society has two choices. 
First it can wait until catastrophic failures 
expose systemic deficiencies, distortion and 
self-deceptions… 
Secondly, a culture can provide social checks 
and balances to correct for systemic 
distortion prior to catastrophic failures.” 
- Mahatma Gandhi 
“Speed is irrelevant if you are going in the 
wrong direction” 
- Mahatma Gandhi
Media Information 
• 2nd November: press conference to present the Synthesis Report in 
Copenhagen, with UN Secretary-General Ban Ki Moon, IPCC Chairman R 
K Pachauri, WMO Secretary-General Michel Jarraud, IPCC Secretary 
Renate Christ, and Peruvian Environment Minister Manuel Pulgar-Vidal 
• The press conference will be webcast live at 5:00AM PET 
• The Synthesis Report and the press release will be available under 
embargo one day before the press conference – registration online 
• After the press conference IPCC authors and officials will be available 
for interview, 7:00 AM PET onwards, in person or by phone. Requests 
for interviews can be made online. 
Contact: Mr Jonathan Lynn, IPCC Senior Communications Officer, 
jlynn@wmo.int and Ms Noemie Leprince-Ringuet, Synthesis Report 
Technical Support Unit, noemie.ringuet@teri.res.in

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Entendiendo la Ciencia del Cambio Climático - Dr. Rajendra Kumar Pachauri

  • 1. Chairman, Intergovernmental Panel on Climate Change Media Training Workshop in Preparation for the COP20 Understanding the Science of Climate Change R. K. Pachauri 16 October 2014, Lima, Perú
  • 2. Human influence on the climate system is clear and has been detected in warming of the atmosphere and the ocean, in changes in the global water cycle, in reductions in snow and ice, in global mean sea level rise, and in changes in some climate extremes. - IPCC AR5 Working Group I Source : IPCCAR5
  • 3. 3 The IPCC Fifth Assessment Report A clear and up to date view of the current state of scientific knowledge relevant to climate change. Working group I The Physical Science Basis  259 authors  39 countries  54,677 comments  2 million gigabytes of numerical data from climate model simulations  Over 9200 scientific publications cited Working Group II Impacts, Adaptation and Vulnerability  309 authors  70 countries  50,444 comments  Over 12,000 scientific references cited Working Group III Mitigation of Climate Change  235 authors  57 countries  38,315 comments  Close to 1200 scenarios of socioeconomic development analyzed  Close to 10,000 references to literature The Synthesis Report will be released in Copenhagen on 2nd November 2014 Source : IPCC AR5
  • 4. 4 Observed changes in the climate system Climate change is unequivocal Source : IPCC AR5 • The oceans have warmed and risen • The amounts of snow and ice have diminished • Sea level has risen • The concentrations of greenhouse gases have increased
  • 5. 5 Human influence of the climate system is clear Understanding the causes • 95% certainty that human influence has been the dominant cause of the observed warming since the mid-20th century • Since the 1950s, many of the observed changes are unprecedented over decades to millennia. • Limiting climate change will require sustained and substantial reductions in greenhouse gas emissions Source : IPCC AR5 Source : IPCC AR5
  • 6. 6 Trends in GHGs and their drivers Total anthropogenic GHG emissions were the highest in human history from 2000 to 2010 Greenhouse gas emissions by economic sectors Source : IPCC AR5 • Globally, economic and population growth continue to be the most important drivers of increases in CO2 emissions from fossil fuel combustions • These are expected to continue to drive emissions growth without additional efforts to reduce GHG emissions.
  • 7. 7 Observed climate change in Perú In CA and SA, decadal variability and changes in extremes have been affecting large sectors of the population, especially those more vulnerable and exposed to climate hazards. • Strong negative precipitation trends and warming detected in the Mantaro Valley, Perú • Air temperature increases in the southern Andes of Perú (1964-2006) • In the Peruvian western Amazonia, mean rainfall for 1964–2003 has decreased • Rapid retreat and melting of the tropical Andes glaciers of Venezuela, Colombia, Ecuador, Perú and Bolivia • 7 out of 9 river basins have probably crossed a critical threshold, exhibiting a decreasing dry-season discharge in the Cordillera Blanca of Perú Source : IPCC AR5
  • 8. Extreme events during and by the end of the 21st Century • It is very likely that the length, frequency, and/or Source : IPCC SREX intensity of warm spells or heat waves will increase over most land areas • Under some scenarios, a 1-in-20 year hottest day is likely to become a 1-in-2 year event in most regions • It is likely that the frequency of heavy precipitation or the proportion of total rainfall from heavy falls will increase over many areas of the globe
  • 9. 9 Future changes in the climate system Warming will continue beyond 2100 under all RCP scenarios except RCP2.6. Global surface temperature change for the end of the 21st century:  is likely to exceed 1.5°C relative to 1850 to 1900 for all RCP scenarios except RCP2.6.  is likely to exceed 2°C for RCP6.0 and RCP8.5  is more likely than not to exceed 2°C for Source : IPCC AR5 RCP4.5.
  • 10. 10 Abrupt and irreversible impacts Most aspects of climate change will persist for many centuries even if emissions of CO2 are stopped. • Sustained mass loss by ice sheets (some of which irreversible) would cause larger sea level rise. • Sustained warming greater than some threshold (greater than about 1°C but less than about 4°C global mean warming with respect to pre-industrial) would lead to the near-complete loss of the Greenland ice sheet over a millennium or more, causing a global mean sea level rise of up to 7 m. Source : IPCC AR5
  • 11. 11 Impacts on food security All aspects of food security are potentially affected by climate change, including food access, utilization, and price stability. Impacts will occur in the context of rapidly rising crop demand. • Projected negative impacts for production of wheat, rice and maize for local temperature increases of 2°C or more above late-20th-century levels, without adaptation. • Redistribution of marine fisheries catch potential poses risk of reduced supplies, income, and employment. Source : IPCC AR5
  • 12. 12 Impacts on human health Throughout the 21st century, climate change is expected to lead to increases in ill-health in many regions and especially in developing countries with low income. Increased likelihood of: • Injury, disease, and death due to more intense heat waves and fires. • Under-nutrition from diminished food production in poor regions. • Risks from food- and water- and vector-borne diseases. Source : IPCC AR5
  • 13. 13 Impacts on human security Climate change over the 21st century can increase: • Displacement of people, particularly in developing countries with low income. • Risks of violent conflicts by amplifying poverty and economic shocks. • Rivalry among states due to potential transboundary impacts of climate change, such as changes in sea ice, shared water resources, and pelagic fish stocks. Source : IPCC AR5
  • 14. 14 Impacts of climate change on urban areas Climate change will have profound impacts on a broad spectrum of city functions, infrastructure and services and will interact with and may exacerbate many existing stresses. Source : IPCC AR5 • The risks: rising sea levels, storm surges, heat stress, extreme precipitation, flooding, landslides, drought, increased aridity, water scarcity and air pollution. • Risks can have widespread negative impacts on people, economies and ecosystems • Risks are amplified for those who live in informal settlements with inadequate provision for adaptation
  • 15. 15 Projected impacts in Perú • 2%–30% annual discharge decrease in the Santa River once the glaciers are completely melted • Projections estimate impacts of glacier melt to between US$212 million to US$ 1.5 billion due to losses of hydropower generation • Perú is one of the most vulnerable countries to climate change impacts on fisheries (due to warming, species shift, importance of fisheries to the national economy and diet) • Climate change may alter plant diseases and potato late blight severity is expected to increase in Perú Source : IPCC AR5
  • 16. 16 Implications for development Climate-related hazards exacerbate other stressors, often with negative outcomes for livelihoods, especially for people living in poverty. Throughout the 21st century, climate-change impacts are projected to: • Slow down economic growth • Make poverty reduction more difficult • Further erode food security • Prolong existing and create new poverty traps, particularly in urban areas and emerging hotspots of hunger Source : IPCC AR5
  • 17. 17 Fatalities are higher in developing countries From 1970-2008, over 95% of natural-disaster-related deaths occurred in developing countries Source : IPCC SREX
  • 18. 18 Adaptation and Mitigation “Climate-resilient pathways combine adaptation and mitigation to reduce climate change and its impacts. Since mitigation reduces the rate and magnitude of warming, it also increases the time available for adaptation to a particular level of climate change, potentially by several decades.” IPCC Fifth Assessment Report Source : IPCC AR5
  • 19. 19 There are strategies that can help manage disaster risk now and also help improve people’s livelihoods and well-being The most effective strategies offer development benefits in the relatively near term and reduce vulnerability over the longer term Source : IPCC SREX
  • 20. 20 Effective risk management and adaptation are tailored to local and regional needs and circumstances • Changes in climate extremes vary across regions • Each region has unique vulnerabilities and exposure to hazards • Effective risk management and adaptation address the factors contributing to exposure and vulnerability Source : IPCC SREX
  • 21. 21 Adaptation experience in Perú • Constitutional and legal reforms for more efficient water resources management in coordination between 7 countries in SA and CA including Perú; but further implementation is required • The management of ENSO-related events in Perú via participatory or risk reduction approaches • Crop diversification in the Peruvian Andes to suppress pest outbreaks and pathogen transmission • Address constraints on access to key resources for reducing vulnerability, as shown by studies with indigenous farmers in highland Perú Source : IPCC AR5
  • 22. 22 Impacts of mitigation on GDP growth Delaying additional mitigation further increases mitigation costs in the medium to long term 2030 Time GDP Current GDP without mitigation GDP with stringent mitigation (reaching ≈ 450 ppm CO2eq in 2100) Loss in global consumption in 2030: 1.7% (median) Source : IPCC AR5 Loss in global consumption in 2050: 3.4% (median) Loss in global consumption in 2100: 4.8% (median) 2050 2100
  • 23. 23 Stringent mitigation scenarios Characteristics of scenarios reaching levels of about 450 ppm CO2eq by 2100 (likely chance to keep temperature change below 2C relative to preindustrial levels): • Lower global GHGs in 2050 than in 2010 (40% to 70% lower globally) • Emissions levels near zero GtCO2eq or below in 2100 • More rapid improvements in energy efficiency • A tripling to nearly a quadrupling of the share of energy supply from renewables by 2050 • Many scenarios reaching 450, 500 and 550 ppm CO2eq by 2100 require widespread deployment of BECCS, afforestation, and other CDR technologies post 2050 Source : IPCC AR5
  • 24. 24 RE costs are still higher than existing energy prices but in various settings RE is already competitive. Source : IPCC SRREN
  • 25. 25 Co-benefits The intersections of mitigation and adaptation with other societal goals, if well managed, can strengthen the basis for undertaking climate action: • Improved energy efficiency and security • Cleaner energy sources • Air quality and human health • Reduced energy and water consumption in urban areas • Sustainable agriculture and forestry • Protection of ecosystems for carbon storage Source : IPCC AR5
  • 26. 26 Integration of climate change into policies • C40 Cities- Climate Leadership Group (ICLEI) and Lima’s Metropolitan Strategy to CCA • Growing awareness of CA and SA governments on the need to integrate climate change and future climate risks in their policies • 18 regional Non-Annex countries, including Perú have already published their 1st and/or 2nd National Communication to the UNFCCC allowing to measure their emissions and to assess their present and future vulnerability. Source : IPCC AR5
  • 27. 27 Climate change and sustainable development Governing a transition toward an effective climate response and sustainable development pathway is a challenge involving rethinking our relation to nature. • A stable climate is one component of sustainable development. • Designing an effective climate policy involves “mainstreaming” climate in the design of sustainable development strategies. • Behaviour, lifestyle and culture can substantially contribute to lowering emissions: • Changes in consumption patterns • Dietary changes • Reduction in food wastes Source : IPCC AR5
  • 28. 28 Climate change and equity Limiting the effects of climate change is necessary to achieve SD and equity, including poverty eradication. Issues of equity, justice, and fairness arise with respect to mitigation and adaptation: • Different past and future contributions to the accumulation of GHGs in the atmosphere • Varying challenges and circumstances • Different capacities to address mitigation and adaptation. Options for equitable burden-sharing can reduce the potential for the costs of climate action to constrain development. Equitable outcomes can lead to more effective cooperation Source : IPCC AR5
  • 29. “A technological society has two choices. First it can wait until catastrophic failures expose systemic deficiencies, distortion and self-deceptions… Secondly, a culture can provide social checks and balances to correct for systemic distortion prior to catastrophic failures.” - Mahatma Gandhi “Speed is irrelevant if you are going in the wrong direction” - Mahatma Gandhi
  • 30. Media Information • 2nd November: press conference to present the Synthesis Report in Copenhagen, with UN Secretary-General Ban Ki Moon, IPCC Chairman R K Pachauri, WMO Secretary-General Michel Jarraud, IPCC Secretary Renate Christ, and Peruvian Environment Minister Manuel Pulgar-Vidal • The press conference will be webcast live at 5:00AM PET • The Synthesis Report and the press release will be available under embargo one day before the press conference – registration online • After the press conference IPCC authors and officials will be available for interview, 7:00 AM PET onwards, in person or by phone. Requests for interviews can be made online. Contact: Mr Jonathan Lynn, IPCC Senior Communications Officer, jlynn@wmo.int and Ms Noemie Leprince-Ringuet, Synthesis Report Technical Support Unit, noemie.ringuet@teri.res.in