Select files to upload
or use drag and drop
Select files to upload
or use drag and drop
Select files to upload
or use drag and drop
Select files to upload
or use drag and drop
Select files to upload
or use drag and drop
E - Climate Modeling and Forecasting
E - Catastrophe Modeling
E - Climate Uncertainty
E - Expert Elicitation
E - Integrated Assessment Modeling
E - Model Reliability
2011/1 Global Surface Temperature Anomalies
1990-2300 (1996) Global temperature change associated with SLR estimates
1995 Projected geographic distribution of global temperature change based on 2x CO2
1995 Projected temperature change to 2070
2009 Climate change modeling has gotten a lot better
2010 Annual variation in national precipitation estimates based on 53 model runs using 24 models
2010 Modeled sensitivity per 1000 GTs emissions
2011 The increasing resolution of climate models
2011 The many steps associated with estimating extreme event damages
2012 There's huge uncertainty about really long-term outcomes
2014 Related concentrations to temperature based on these runs
2016 IAMs are at the core of climate change economic analysis, but have a very hard incorporating tipping points
2017 The ice core data is key because it tracks the development of humans
2021 Current and proposed connections between climate research and business
Applying Bayes' Theorem to Climate Change Trends
Breakdown of these conclusions by resources and data
Climate models have evolved significantly
CMIP6 Global Climate Model Projections
Computer models of the atmosphere
Dealing with the water cycle
Estimated warming in 2100 based on revisions in Transient Climate Response estimates
Issue of measurement site bias appears a red herring
1983 Key components of the analytical methodology
Modeling the climate system
Models Have to Grapple With Several Sources of Uncertainty
Most scenarios lead to a high probability of exceeding 2 degrees of change
Muller's Review of the Temperature Record
No evidence found in review
Research need to focus on model verification
Scenarios make a big difference 2050 to 2100, making some scenarios much riskier than others
Temperature probabilities vary widely across the scenarios
Testing the IPCC Hypothesis Over the Short Term
The evolution of climate models
The family tree of GCMs
The IPCC's Estimates Were Too High
The models have a lot to contend with
The Noise Can Easily Obscure the Signal
The reason for model downscaling
There has been a lot of evolution in models since 1970s
Uncertainties in climate change projections come from several sources, varying over time
Warming and Colling Influences Since 1750 - NAS Public
We know that models have uncertainties
1983 Yearly Modeling Sequence
Abstract
Be very careful about misreading model results
GCMs are not valid tools for examining how climate will change at the scale of physical assets
The desire of governments, regulators, standard-setters, and business to assess climate risk requires urgent understanding of the uses and limitations of climate model information
The IPCC has used very different scenario approaches over time
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 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?
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 Modeled sensitivity per 1000 GTs emissions
2010 NRC Climate Stabilization Targets
Climate Sensitivity to GHGs
Under-Estimating Climate Risk
Visualizing GHG Emissions
E - Climate Modeling and Forecasting
E - Catastrophe Modeling
E - Climate Uncertainty
E - Expert Elicitation
E - Integrated Assessment Modeling
E - Model Reliability
2011/1 Global Surface Temperature Anomalies
1990-2300 (1996) Global temperature change associated with SLR estimates
1995 Projected geographic distribution of global temperature change based on 2x CO2
1995 Projected temperature change to 2070
2009 Climate change modeling has gotten a lot better
2010 Annual variation in national precipitation estimates based on 53 model runs using 24 models
2010 Modeled sensitivity per 1000 GTs emissions
2011 The increasing resolution of climate models
2011 The many steps associated with estimating extreme event damages
2012 There's huge uncertainty about really long-term outcomes
2014 Related concentrations to temperature based on these runs
2016 IAMs are at the core of climate change economic analysis, but have a very hard incorporating tipping points
2017 The ice core data is key because it tracks the development of humans
2021 Current and proposed connections between climate research and business
Applying Bayes' Theorem to Climate Change Trends
Breakdown of these conclusions by resources and data
Climate models have evolved significantly
CMIP6 Global Climate Model Projections
Computer models of the atmosphere
Dealing with the water cycle
Estimated warming in 2100 based on revisions in Transient Climate Response estimates
Issue of measurement site bias appears a red herring
1983 Key components of the analytical methodology
Modeling the climate system
Models Have to Grapple With Several Sources of Uncertainty
Most scenarios lead to a high probability of exceeding 2 degrees of change
Muller's Review of the Temperature Record
No evidence found in review
Research need to focus on model verification
Scenarios make a big difference 2050 to 2100, making some scenarios much riskier than others
Temperature probabilities vary widely across the scenarios
Testing the IPCC Hypothesis Over the Short Term
The evolution of climate models
The family tree of GCMs
The IPCC's Estimates Were Too High
The models have a lot to contend with
The Noise Can Easily Obscure the Signal
The reason for model downscaling
There has been a lot of evolution in models since 1970s
Uncertainties in climate change projections come from several sources, varying over time
Warming and Colling Influences Since 1750 - NAS Public
We know that models have uncertainties
1983 Yearly Modeling Sequence
Abstract
Be very careful about misreading model results
GCMs are not valid tools for examining how climate will change at the scale of physical assets
The desire of governments, regulators, standard-setters, and business to assess climate risk requires urgent understanding of the uses and limitations of climate model information
The IPCC has used very different scenario approaches over time
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 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?
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