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E - Climate Science
1. Where is the heat going?
The great majority of added energy goes into upper oceans
2007 Mindmap - The science of global warming
2008 How much sensitivity matters
2008 The current bathtub
2009 At what temperature will we stabilize?
2009 Key facts on key GHGs
2009 Snapshot of world GHG emissions by sector, 2000
2009 The right observational timescale for understanding climate change?
2010 An alternative view of temperature vs. cumulative emissions
2010 CO2 and CH4 in the Ice Cores and Today
2010 Correlating CO2 and Temperature in the Vostok Record
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 The 100,000 Year Cycles in the Vostok Cores
2010 The Vostok Temperature Record
2010 Timescale for removing CO2 from the atmosphere
2011 Estimates of climate sensitivity have varied widely
2011 Probability distributions of climate sensitivity
2011 Scientific perception of risk across the board
2011 The timeline for CO2 removals from the atmosphere
2011 Uncertainty in climate sensitivity
2011 Why is the warming so slow to manifest itself?
2013 It takes a long time for CO2 levels to come back down
2014 Estimated Equilibrium climate sensitivity
2014 Implications of climate sensitivity
2014 Transient climate response
2014 Where Climate Sensitivity Estimates Come From
2015/12 Timeline of Global Change Science
2016 650,000 years of CO2 concentrations
2016 Weather Channel_CO2 concentrations
2017 1950 was the turning point for CO2
A tale of CO2 and three planets in our solar system
a. Human development and climate
a. The planetary energy equation
Articles written about climate change
b. The greenhouse effect
Carbon flows in the global carbon cycle
Change in radiative forcing to 2100
Climate change is driving up global heat content
CO2 is only a trace component of the atmosphere
Contribution of individual GHGs to radiative forcing
Estimated positive feedbacks not routinely incorporated into climate estimates
Estimating planetary temperatures based on greenhouse effects
Fossil fuel reserves and potential contribution to CO2
Global carbon cycle 2007 - 2016
Global forcing has expanded rapidly with population
Google Images Page - Global Carbon Cycle
Graphic - How big a change are we talking about?
Graphic - Where's the heat going?
How sensitive a greenhouse?
IPCC Likelihood that observed change is anthropogenic
Residence times of different gases in the atmosphere
Short Term Impacts of Natural Climate Variations - NAS Public
The global carbon cycle
The global carbon cycle
The implications of climate sensitivity
The timelines of weather and climate forecasting
This is what cycles do - but that's not what's happening
We understand greenhouse gases - molecules
What's warming the world? - 2
What's warming the world? - 3
What's warming the world? - 4
What's warming the world? - 5
What's warming the world? - 6
What's warming the world? - 7
E - Climate Sensitivity
2007 Estimates of climate sensitivity vary widely
2007 The long tail of climate sensitivity
2008 How much sensitivity matters
2009 Risk of temperature directly related to concentrations, and varies widely over time
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 Relating emissions trajectories to near-term and long-term warming
2011 Estimates of climate sensitivity have varied widely
2011 Probability distributions of climate sensitivity
2011 The tail of scientific uncertainty is longer than we thought
2011 Uncertainty - Climate sensitivity
2011 Uncertainty in climate sensitivity
2014 Estimated Equilibrium climate sensitivity
2014 Implications of climate sensitivity
2014 Transient climate response
2014 Where Climate Sensitivity Estimates Come From
A wide range of climate sensitivity estimates
Feedbacks with what impact?
Sea Level Rise SLR
Taylor: We just don't know a lot of key things about climate change. It all depends on the planetary sensitivity
The IPCC considers a wide range of values
E - Science Top Level
1. Where is the heat going?
2015/1 Infographic: The Anti-Science Climate Denier Caucus, 114th Congress Edition
Infographic - A review of major milestones in climate science and policy
Infographic - Climate Change Scientific Consensus
Infographic - Climate Change Today
Infographic - Fossil fuels in a historical timeline
Infographic - IPCC Climate Everyones Business
Infographic - The Carbon Budget
Infographic - The-big-questions-of-climate-change
Infographic - Why global carbon emissions fell in 2014
Infographic 2013 Climate by the Numbers
E - Carbon Budget
E - Carbon Cycle
E - Climate Change Fingerprint
E - Climate Feedbacks
E - Climate History
E - Climate Modeling and Forecasting
E - Climate Uncertainty
E - Dangerous Change
E - Doubting Climate Science Knowledgebase
E - GHG Emissions Scenarios/Forecasts
E - Impact Attribution
E - Past and Future Emissions
E - Science Education
E - Topic History
Are disaster scenarios about tipping points like ‘turning off the Gulf Stream’ and release of methane from the Arctic a cause for concern?
2015 IPCC_Infographics Working Group 1
The great majority of added energy goes into upper oceans
2019/X How we know that global warming is real
2007 Mindmap - The science of global warming
2008 How much sensitivity matters
2008 The current bathtub
2009 At what temperature will we stabilize?
2009 Key facts on key GHGs
2009 Snapshot of world GHG emissions by sector, 2000
2009 The right observational timescale for understanding climate change?
2010 An alternative view of temperature vs. cumulative emissions
2010 CO2 and CH4 in the Ice Cores and Today
2010 Correlating CO2 and Temperature in the Vostok Record
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 The 100,000 Year Cycles in the Vostok Cores
2010 The Vostok Temperature Record
2010 Timescale for removing CO2 from the atmosphere
2011 Estimates of climate sensitivity have varied widely
2011 Probability distributions of climate sensitivity
2011 Scientific perception of risk across the board
2011 The timeline for CO2 removals from the atmosphere
2011 Uncertainty in climate sensitivity
2011 Why is the warming so slow to manifest itself?
2013 It takes a long time for CO2 levels to come back down
2014 Estimated Equilibrium climate sensitivity
2014 Implications of climate sensitivity
2014 Transient climate response
2014 Where Climate Sensitivity Estimates Come From
2015/12 Timeline of Global Change Science
2015 Timescales of climate processes and inclusion of feedbacks in climate models
2016 650,000 years of CO2 concentrations
2016 Weather Channel_CO2 concentrations
2017 1950 was the turning point for CO2
2020 Temperature record over last 65 million years
2021 Only 0.17 Percent of Peer-Reviewed Papers Question Global Warming
A tale of CO2 and three planets in our solar system
a. Human development and climate
a. The planetary energy equation
Articles written about climate change
b. The greenhouse effect
Carbon flows in the global carbon cycle
Change in radiative forcing to 2100
Climate change is driving up global heat content
CO2 concentrations are much lower today than in the past
CO2 is only a trace component of the atmosphere
Contribution of individual GHGs to radiative forcing
Estimated positive feedbacks not routinely incorporated into climate estimates
Estimating planetary temperatures based on greenhouse effects
Explaining the climate record with volcanoes and solar spots.
Fossil fuel reserves and potential contribution to CO2
Global carbon cycle 2007 - 2016
Global forcing has expanded rapidly with population
Google Images Page - Global Carbon Cycle
Graphic - How big a change are we talking about?
Graphic - Where's the heat going?
gw 10
How sensitive a greenhouse?
IPCC Likelihood that observed change is anthropogenic
No expert disagrees with fact that anthropogenic emissions are rising and impacting the atmosphere
Residence times of different gases in the atmosphere
Scienstists who established the basis for climate change
Short Term Impacts of Natural Climate Variations - NAS Public
Significant climate influences 1850-2018
SPM1. Total GHG Emissions by Gases
SPM2. GHG emissions by sectors
SPM3. Where Were Changes in CO2 Coming From By Decade
SPM4. GHG Emissions Pathways for AR5 Scenarios
SPM5. GHG Emissions Pathways to 2030
SPM6. Impact of climate policy on air pollution
SPM7. Direct Emissions by Scenario and w/ w/o CCS
SPM8. Demand Reduction and Low-Carbon Energy Shares
SPM9. Changes in Annual Investment Flows
The current GWP of GHGs
The global carbon cycle
The global carbon cycle
The implications of climate sensitivity
The timelines of weather and climate forecasting
This is what cycles do - but that's not what's happening
We understand greenhouse gases - molecules
What's warming the world? - 2
What's warming the world? - 3
What's warming the world? - 4
What's warming the world? - 5
What's warming the world? - 6
What's warming the world? - 7
2. Humble Human Influences
A lot of great EU graphics re climate change
Against the right scale (K) the sensitivity of the atmosphere makes more sense
Black carbon
Changing CO2 concentrations have increased the capture of energy in the atmosphere by less than 1%
Energy in the climate system is expressed as w/m2
Fossil fuel burning was identified as a risk long ago
Modest human impacts on climate can be analogized to slight changes in diet
Scientists have called for dramatic reductions - but no such policy in place
Since human impacts amounts to 1% of global energy flow, everything else has to be understood very well
There is no such thing about scientific certainty in the way it's commonly used
What are some of the risky what-ifs?
What do we know for sure regarding climate change?
What don't we know for sure regarding climate change?
E - Temperature Scenarios and Forecasts
E - 1.5 Degree Target
E - 1 Degree 350 ppm Scenario
E - 2 Degree 450 PPM Pathway
E - 3-4 Degree Scenario
200X Cumulative CO2 emissions and temperature change under AR5 scenarios
200X If unrestrained climate change, what would it really mean?
2009 At what temperature will we stabilize?
2009 Characterizing the IPCC scenarios
2009 Potential climate change feedback loops
2009 Risk of temperature directly related to concentrations, and varies widely over time
2009 Summary of IPCC stabilization scenarios
2009 Temperatures Will Rise - Australia as an Example
2010 Linking temperature to cumulative emissions
2010 Relating emissions trajectories to near-term and long-term warming
2011 Aggregated climate change index shows future change relative to current variability
2011 The 4 climate security scenarios to be planning for
2011 Very good chance we're already committed to >2 degrees C
2011 Why is the warming so slow to manifest itself?
2012 Probabilistic Forecasts to 2100 based on new Representative Concentration Pathways
2012 Showing North American Detail
2012 There's huge uncertainty about really long-term outcomes
2013 Emissions are currently on a 4-6 degree C trajectory
2013 There is a lot of uncertainty re future scenarios
2014/8 Future Temperature and Precipitation Change in Colorado
2014 Average summer temperatures across the U.S.
2014 Average winter temperatures
2014 Global temperature projections different and timelines
2014 Number of extreme cold days
2014 U.S. average temperature projections
2015/5 Longer dry spells in store for U.S. Great Plains
2015 BAU vs. INDCs vs. 2 degrees
2016 1.5 to 4.5 degrees C by 2100 with high degree of confidence
2016 Box plots for temperature change and CO2 concentrations
2016 Current emissions scenarios and temperatures
2016 Potential temperature increase associated with consuming proven fossil fuels
2016 Temperature trend associated with scenarios
2017 Cumulative emissions and warming to 2100 - multiple GHGs
2017 Forecasting Oregon's hottest days to 2069
2017 Probability density function for warming in 2050 and 2100
2017 Projected global mean temperature change and incremental temperature change
2017 The IPCC scenarios for temperature change
2017 Warming probabilities based on feedback uncertainties
2018 Comparing Shell's scenarios in terms of global temperature
2018 Temperature impacts of forestry interventions under the Sky Scenario
2018 The scenario probability distribution
2019 Visualizing average global temperature change 2040-2060
2021 Predictions for near surface temperature anomalies 2021 - 2025
2021 Projected changes in average annual temperatures across the US associated with warming of 2oC and 4oC
2021 Referent - Surface Temperature w/UQ
2021 Two future temperature scenarios which companies might consider
2030-2050 (2020) Regional increase in average annual temperature
2050-2100 (2012) Projected increase 20-year return values of annual maximum daily temperatures
2100 (2012) Expected change in regional extreme temperatures (degrees and SDs)
2100 (2012) Expected regional temperature change (degrees and SDs)
2100 (2012) Percentage of expected to exceed 3, 4, and 5 SDs from current temperatures
2100 100 Degree days in U.S. Under 2 Emissions Scenarios
A 2100 snapshot of climate change for Maryland
AR4 Emissions scenarios and temperature change
Assessment Box SPM.1 Figure 1
Average warming under IPCC Scenarios - NAS Public
Changing U.S. frequency of 1 in 20 year events by 2099
CO2 Levels: Current & Historic Atmospheric Carbon Dioxide
Comparing different scenario types SRES and RCP
Comparing mitigation, non-mitigation, and full stop scenarios to 2100
Comparing SRES and RCP scenarios - carbon emissions
Comparing the temperature projections of different scenarios to 2100
Cumulative global emissions vs. temperature change
Days Above 95 degrees by 2100
Days over 110 degrees in Phoenix by 2100
Decreases in number of frost days per year
Emissions and Temperature Linkage - NAS Public
Emissions vs. temperature for IPCC scenarios to 2100
Emissions vs. temperature to 2100 for IPCC RCP 2.6
Estimated positive feedbacks not routinely incorporated into climate estimates
Figure SPM.4b
Figure SPM.4c
Forecast atmospheric vs. ocean temperature change to 2100
Forecast global temperatures to 2200 by time period
Forecast temperature change by scenario and timeframe to 2100
Forecasted US temp changes
Global average temperature change under differing scenarios
Global mean temperature rise across the three scenarios
Global temperature forecasting
Historical and projected temperature distribution for the U.S.
How different models forecast temperature change to 2100
Key IPCC scenario variables to 2300
Linking global emissions to temperatures - various models
Long term implications of current emissions scenarios
Long-term temperature imlications of IPCC scenarios
Longer Great Plains dry spells by 2100
Maps
New simulations for projected temperature in the U.S.
Patterns of warming in Summer and Winter - NAS Public
Potential global temperature rise by 2026
Probabilities
Projected global temperature change
Projected temperature change of hottest and coldest days
Projected U.S. temperature change
Projecting the ratio of temperature records to 2100
Putting current temperatures in context
Range of possible temperature responses globally to 2100
Regional temperature and precipitation probabilities based on RCP3 and RCP8.5
Regional temperature forecast range
Relating emissions pathway to temperature probabilities
Temperature forecasts comparing IPCC SRES and RCP scenarios
Temperature increases of 10-12 degrees C by 2300
Temperature ranges for IPCC scenarios by 2099
The geographic ratio of local to global temperature change
The implications of climate sensitivity
The IPCC scenarios used in the TAR and FAR
The scenarios used in the NCA:vs. the new IPCC Scenarios
Three paths for responding to climate change
Variability across model runs
Various temperature shifts to 2100 under the IPCC 8.5 scenario
Why black swans are likely
2010-2100 Regional Warming under 3 scenarios
Probability of temperature exceedance curves in 2100 for current IPCC scenarios - there is a lot of uncertainty
2010 NRC_Climate Stabilization Targets
0oC - 3.5oC heating degree days impacts in the U.S.
0oC - 4oC crop yield impacts
1900-2100 (2010) Changes in permafrost coverage to 2100
2010 % of summers warmer than today's 95th percentile, based on 3oC from pre-industrial
2010 1 Meter of Sea Level Rise on the Gulf Coast
2010 Ability of ocean organizations to calcify, related to stabilized CO2 concentrations
2010 An alternative view of temperature vs. cumulative emissions
2010 CO2 and HFC emissions to 2050
2010 Cumulative and projected carbon emissions to 2050
2010 Direct climate impacts, and associated human/ecological impacts
2010 Economics of climate change in Chicago by 2070-2099
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 Potential distances species will have to cover to stay at the same temperature
2010 Relating emissions trajectories to near-term and long-term warming
2010 Relating sea level rise to storm return time for NYC
2010 The Greenland ice sheet under alternative long-term scenarios
2010 Timescale for removing CO2 from the atmosphere
Centigrade vs. Fahrenheit
Per degree changes in precipitation globally
Per degree impacts on hurricane and typhoon intensity
Per degree relative change in runoff globally
I:ConcentrationTemperatureCorrelation
Individual Graphics
2010 Linking temperature to cumulative emissions
2010 NRC Climate Stabilization Targets
Plausible Average Global Temperature in 2100
Under-Estimating Climate Risk
E - Climate Science
1. Where is the heat going?
The great majority of added energy goes into upper oceans
2007 Mindmap - The science of global warming
2008 How much sensitivity matters
2008 The current bathtub
2009 At what temperature will we stabilize?
2009 Key facts on key GHGs
2009 Snapshot of world GHG emissions by sector, 2000
2009 The right observational timescale for understanding climate change?
2010 An alternative view of temperature vs. cumulative emissions
2010 CO2 and CH4 in the Ice Cores and Today
2010 Correlating CO2 and Temperature in the Vostok Record
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 The 100,000 Year Cycles in the Vostok Cores
2010 The Vostok Temperature Record
2010 Timescale for removing CO2 from the atmosphere
2011 Estimates of climate sensitivity have varied widely
2011 Probability distributions of climate sensitivity
2011 Scientific perception of risk across the board
2011 The timeline for CO2 removals from the atmosphere
2011 Uncertainty in climate sensitivity
2011 Why is the warming so slow to manifest itself?
2013 It takes a long time for CO2 levels to come back down
2014 Estimated Equilibrium climate sensitivity
2014 Implications of climate sensitivity
2014 Transient climate response
2014 Where Climate Sensitivity Estimates Come From
2015/12 Timeline of Global Change Science
2016 650,000 years of CO2 concentrations
2016 Weather Channel_CO2 concentrations
2017 1950 was the turning point for CO2
A tale of CO2 and three planets in our solar system
a. Human development and climate
a. The planetary energy equation
Articles written about climate change
b. The greenhouse effect
Carbon flows in the global carbon cycle
Change in radiative forcing to 2100
Climate change is driving up global heat content
CO2 is only a trace component of the atmosphere
Contribution of individual GHGs to radiative forcing
Estimated positive feedbacks not routinely incorporated into climate estimates
Estimating planetary temperatures based on greenhouse effects
Fossil fuel reserves and potential contribution to CO2
Global carbon cycle 2007 - 2016
Global forcing has expanded rapidly with population
Google Images Page - Global Carbon Cycle
Graphic - How big a change are we talking about?
Graphic - Where's the heat going?
How sensitive a greenhouse?
IPCC Likelihood that observed change is anthropogenic
Residence times of different gases in the atmosphere
Short Term Impacts of Natural Climate Variations - NAS Public
The global carbon cycle
The global carbon cycle
The implications of climate sensitivity
The timelines of weather and climate forecasting
This is what cycles do - but that's not what's happening
We understand greenhouse gases - molecules
What's warming the world? - 2
What's warming the world? - 3
What's warming the world? - 4
What's warming the world? - 5
What's warming the world? - 6
What's warming the world? - 7
E - Climate Sensitivity
2007 Estimates of climate sensitivity vary widely
2007 The long tail of climate sensitivity
2008 How much sensitivity matters
2009 Risk of temperature directly related to concentrations, and varies widely over time
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 Relating emissions trajectories to near-term and long-term warming
2011 Estimates of climate sensitivity have varied widely
2011 Probability distributions of climate sensitivity
2011 The tail of scientific uncertainty is longer than we thought
2011 Uncertainty - Climate sensitivity
2011 Uncertainty in climate sensitivity
2014 Estimated Equilibrium climate sensitivity
2014 Implications of climate sensitivity
2014 Transient climate response
2014 Where Climate Sensitivity Estimates Come From
A wide range of climate sensitivity estimates
Feedbacks with what impact?
Sea Level Rise SLR
Taylor: We just don't know a lot of key things about climate change. It all depends on the planetary sensitivity
The IPCC considers a wide range of values
E - Science Top Level
1. Where is the heat going?
2015/1 Infographic: The Anti-Science Climate Denier Caucus, 114th Congress Edition
Infographic - A review of major milestones in climate science and policy
Infographic - Climate Change Scientific Consensus
Infographic - Climate Change Today
Infographic - Fossil fuels in a historical timeline
Infographic - IPCC Climate Everyones Business
Infographic - The Carbon Budget
Infographic - The-big-questions-of-climate-change
Infographic - Why global carbon emissions fell in 2014
Infographic 2013 Climate by the Numbers
E - Carbon Budget
E - Carbon Cycle
E - Climate Change Fingerprint
E - Climate Feedbacks
E - Climate History
E - Climate Modeling and Forecasting
E - Climate Uncertainty
E - Dangerous Change
E - Doubting Climate Science Knowledgebase
E - GHG Emissions Scenarios/Forecasts
E - Impact Attribution
E - Past and Future Emissions
E - Science Education
E - Topic History
Are disaster scenarios about tipping points like ‘turning off the Gulf Stream’ and release of methane from the Arctic a cause for concern?
2015 IPCC_Infographics Working Group 1
The great majority of added energy goes into upper oceans
2019/X How we know that global warming is real
2007 Mindmap - The science of global warming
2008 How much sensitivity matters
2008 The current bathtub
2009 At what temperature will we stabilize?
2009 Key facts on key GHGs
2009 Snapshot of world GHG emissions by sector, 2000
2009 The right observational timescale for understanding climate change?
2010 An alternative view of temperature vs. cumulative emissions
2010 CO2 and CH4 in the Ice Cores and Today
2010 Correlating CO2 and Temperature in the Vostok Record
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 The 100,000 Year Cycles in the Vostok Cores
2010 The Vostok Temperature Record
2010 Timescale for removing CO2 from the atmosphere
2011 Estimates of climate sensitivity have varied widely
2011 Probability distributions of climate sensitivity
2011 Scientific perception of risk across the board
2011 The timeline for CO2 removals from the atmosphere
2011 Uncertainty in climate sensitivity
2011 Why is the warming so slow to manifest itself?
2013 It takes a long time for CO2 levels to come back down
2014 Estimated Equilibrium climate sensitivity
2014 Implications of climate sensitivity
2014 Transient climate response
2014 Where Climate Sensitivity Estimates Come From
2015/12 Timeline of Global Change Science
2015 Timescales of climate processes and inclusion of feedbacks in climate models
2016 650,000 years of CO2 concentrations
2016 Weather Channel_CO2 concentrations
2017 1950 was the turning point for CO2
2020 Temperature record over last 65 million years
2021 Only 0.17 Percent of Peer-Reviewed Papers Question Global Warming
A tale of CO2 and three planets in our solar system
a. Human development and climate
a. The planetary energy equation
Articles written about climate change
b. The greenhouse effect
Carbon flows in the global carbon cycle
Change in radiative forcing to 2100
Climate change is driving up global heat content
CO2 concentrations are much lower today than in the past
CO2 is only a trace component of the atmosphere
Contribution of individual GHGs to radiative forcing
Estimated positive feedbacks not routinely incorporated into climate estimates
Estimating planetary temperatures based on greenhouse effects
Explaining the climate record with volcanoes and solar spots.
Fossil fuel reserves and potential contribution to CO2
Global carbon cycle 2007 - 2016
Global forcing has expanded rapidly with population
Google Images Page - Global Carbon Cycle
Graphic - How big a change are we talking about?
Graphic - Where's the heat going?
gw 10
How sensitive a greenhouse?
IPCC Likelihood that observed change is anthropogenic
No expert disagrees with fact that anthropogenic emissions are rising and impacting the atmosphere
Residence times of different gases in the atmosphere
Scienstists who established the basis for climate change
Short Term Impacts of Natural Climate Variations - NAS Public
Significant climate influences 1850-2018
SPM1. Total GHG Emissions by Gases
SPM2. GHG emissions by sectors
SPM3. Where Were Changes in CO2 Coming From By Decade
SPM4. GHG Emissions Pathways for AR5 Scenarios
SPM5. GHG Emissions Pathways to 2030
SPM6. Impact of climate policy on air pollution
SPM7. Direct Emissions by Scenario and w/ w/o CCS
SPM8. Demand Reduction and Low-Carbon Energy Shares
SPM9. Changes in Annual Investment Flows
The current GWP of GHGs
The global carbon cycle
The global carbon cycle
The implications of climate sensitivity
The timelines of weather and climate forecasting
This is what cycles do - but that's not what's happening
We understand greenhouse gases - molecules
What's warming the world? - 2
What's warming the world? - 3
What's warming the world? - 4
What's warming the world? - 5
What's warming the world? - 6
What's warming the world? - 7
2. Humble Human Influences
A lot of great EU graphics re climate change
Against the right scale (K) the sensitivity of the atmosphere makes more sense
Black carbon
Changing CO2 concentrations have increased the capture of energy in the atmosphere by less than 1%
Energy in the climate system is expressed as w/m2
Fossil fuel burning was identified as a risk long ago
Modest human impacts on climate can be analogized to slight changes in diet
Scientists have called for dramatic reductions - but no such policy in place
Since human impacts amounts to 1% of global energy flow, everything else has to be understood very well
There is no such thing about scientific certainty in the way it's commonly used
What are some of the risky what-ifs?
What do we know for sure regarding climate change?
What don't we know for sure regarding climate change?
E - Temperature Scenarios and Forecasts
E - 1.5 Degree Target
E - 1 Degree 350 ppm Scenario
E - 2 Degree 450 PPM Pathway
E - 3-4 Degree Scenario
200X Cumulative CO2 emissions and temperature change under AR5 scenarios
200X If unrestrained climate change, what would it really mean?
2009 At what temperature will we stabilize?
2009 Characterizing the IPCC scenarios
2009 Potential climate change feedback loops
2009 Risk of temperature directly related to concentrations, and varies widely over time
2009 Summary of IPCC stabilization scenarios
2009 Temperatures Will Rise - Australia as an Example
2010 Linking temperature to cumulative emissions
2010 Relating emissions trajectories to near-term and long-term warming
2011 Aggregated climate change index shows future change relative to current variability
2011 The 4 climate security scenarios to be planning for
2011 Very good chance we're already committed to >2 degrees C
2011 Why is the warming so slow to manifest itself?
2012 Probabilistic Forecasts to 2100 based on new Representative Concentration Pathways
2012 Showing North American Detail
2012 There's huge uncertainty about really long-term outcomes
2013 Emissions are currently on a 4-6 degree C trajectory
2013 There is a lot of uncertainty re future scenarios
2014/8 Future Temperature and Precipitation Change in Colorado
2014 Average summer temperatures across the U.S.
2014 Average winter temperatures
2014 Global temperature projections different and timelines
2014 Number of extreme cold days
2014 U.S. average temperature projections
2015/5 Longer dry spells in store for U.S. Great Plains
2015 BAU vs. INDCs vs. 2 degrees
2016 1.5 to 4.5 degrees C by 2100 with high degree of confidence
2016 Box plots for temperature change and CO2 concentrations
2016 Current emissions scenarios and temperatures
2016 Potential temperature increase associated with consuming proven fossil fuels
2016 Temperature trend associated with scenarios
2017 Cumulative emissions and warming to 2100 - multiple GHGs
2017 Forecasting Oregon's hottest days to 2069
2017 Probability density function for warming in 2050 and 2100
2017 Projected global mean temperature change and incremental temperature change
2017 The IPCC scenarios for temperature change
2017 Warming probabilities based on feedback uncertainties
2018 Comparing Shell's scenarios in terms of global temperature
2018 Temperature impacts of forestry interventions under the Sky Scenario
2018 The scenario probability distribution
2019 Visualizing average global temperature change 2040-2060
2021 Predictions for near surface temperature anomalies 2021 - 2025
2021 Projected changes in average annual temperatures across the US associated with warming of 2oC and 4oC
2021 Referent - Surface Temperature w/UQ
2021 Two future temperature scenarios which companies might consider
2030-2050 (2020) Regional increase in average annual temperature
2050-2100 (2012) Projected increase 20-year return values of annual maximum daily temperatures
2100 (2012) Expected change in regional extreme temperatures (degrees and SDs)
2100 (2012) Expected regional temperature change (degrees and SDs)
2100 (2012) Percentage of expected to exceed 3, 4, and 5 SDs from current temperatures
2100 100 Degree days in U.S. Under 2 Emissions Scenarios
A 2100 snapshot of climate change for Maryland
AR4 Emissions scenarios and temperature change
Assessment Box SPM.1 Figure 1
Average warming under IPCC Scenarios - NAS Public
Changing U.S. frequency of 1 in 20 year events by 2099
CO2 Levels: Current & Historic Atmospheric Carbon Dioxide
Comparing different scenario types SRES and RCP
Comparing mitigation, non-mitigation, and full stop scenarios to 2100
Comparing SRES and RCP scenarios - carbon emissions
Comparing the temperature projections of different scenarios to 2100
Cumulative global emissions vs. temperature change
Days Above 95 degrees by 2100
Days over 110 degrees in Phoenix by 2100
Decreases in number of frost days per year
Emissions and Temperature Linkage - NAS Public
Emissions vs. temperature for IPCC scenarios to 2100
Emissions vs. temperature to 2100 for IPCC RCP 2.6
Estimated positive feedbacks not routinely incorporated into climate estimates
Figure SPM.4b
Figure SPM.4c
Forecast atmospheric vs. ocean temperature change to 2100
Forecast global temperatures to 2200 by time period
Forecast temperature change by scenario and timeframe to 2100
Forecasted US temp changes
Global average temperature change under differing scenarios
Global mean temperature rise across the three scenarios
Global temperature forecasting
Historical and projected temperature distribution for the U.S.
How different models forecast temperature change to 2100
Key IPCC scenario variables to 2300
Linking global emissions to temperatures - various models
Long term implications of current emissions scenarios
Long-term temperature imlications of IPCC scenarios
Longer Great Plains dry spells by 2100
Maps
New simulations for projected temperature in the U.S.
Patterns of warming in Summer and Winter - NAS Public
Potential global temperature rise by 2026
Probabilities
Projected global temperature change
Projected temperature change of hottest and coldest days
Projected U.S. temperature change
Projecting the ratio of temperature records to 2100
Putting current temperatures in context
Range of possible temperature responses globally to 2100
Regional temperature and precipitation probabilities based on RCP3 and RCP8.5
Regional temperature forecast range
Relating emissions pathway to temperature probabilities
Temperature forecasts comparing IPCC SRES and RCP scenarios
Temperature increases of 10-12 degrees C by 2300
Temperature ranges for IPCC scenarios by 2099
The geographic ratio of local to global temperature change
The implications of climate sensitivity
The IPCC scenarios used in the TAR and FAR
The scenarios used in the NCA:vs. the new IPCC Scenarios
Three paths for responding to climate change
Variability across model runs
Various temperature shifts to 2100 under the IPCC 8.5 scenario
Why black swans are likely
2010-2100 Regional Warming under 3 scenarios
Probability of temperature exceedance curves in 2100 for current IPCC scenarios - there is a lot of uncertainty
2010 NRC_Climate Stabilization Targets
0oC - 3.5oC heating degree days impacts in the U.S.
0oC - 4oC crop yield impacts
1900-2100 (2010) Changes in permafrost coverage to 2100
2010 % of summers warmer than today's 95th percentile, based on 3oC from pre-industrial
2010 1 Meter of Sea Level Rise on the Gulf Coast
2010 Ability of ocean organizations to calcify, related to stabilized CO2 concentrations
2010 An alternative view of temperature vs. cumulative emissions
2010 CO2 and HFC emissions to 2050
2010 Cumulative and projected carbon emissions to 2050
2010 Direct climate impacts, and associated human/ecological impacts
2010 Economics of climate change in Chicago by 2070-2099
2010 Linking temperature to cumulative emissions
2010 Modeled sensitivity per 1000 GTs emissions
2010 Potential distances species will have to cover to stay at the same temperature
2010 Relating emissions trajectories to near-term and long-term warming
2010 Relating sea level rise to storm return time for NYC
2010 The Greenland ice sheet under alternative long-term scenarios
2010 Timescale for removing CO2 from the atmosphere
Centigrade vs. Fahrenheit
Per degree changes in precipitation globally
Per degree impacts on hurricane and typhoon intensity
Per degree relative change in runoff globally
I:ConcentrationTemperatureCorrelation