SlideShare ist ein Scribd-Unternehmen logo
1 von 11
Downloaden Sie, um offline zu lesen
Summary and Conclusion
Carl Denef, January 2014
Despite the threat of the climate crisis, global emissions of CO2
are set to rise again in 2013, reaching a record high of
36 gigatonnes.
Gigatonnes C02
Overview of past, present and future climate
change
Era Global average temperature
anomaly
Atm. CO2
(ppm)
Sea level vs
preindustrial
In 2100 (RCP8.5 scenario) 2.8–5.5 ºC vs preindustrial 1200 0.5–1 m
Present 1.5 ºC vs preindustrial 395 0.3 m
8.2 ka event 2–3 ºC in 2 decades 275
Younger Dryas 7-8 ºC in 1 decade in Greenland
and N-Atlantic, followed by abrupt
250
D-O events 4–6 ºC in decades from ~200 to 220
Last Glacial Maximum 3–8 ºC vs preindustrial 190 120 m
Last Interglacial 1–2 ºC vs preindustrial 280 5.5–9 m
Less Greenland ice sheet
MIS-11 Interglacial 1.5–2.0 ºC vs preindustrial 280 6–20 m
No Greenland ice sheet
Older interglacials 2 ºC vs preindustrial 250-280 = preindustrial
Mid-pliocene 3–10 ºC vs preindustrial 365-415  7–20 m
No Greenland ice sheet
PETM 4-7 ºC vs preindustrial
Sea surface temp.Tropics = 35 ºC
Polar temp. = 10-20 ºC
1125 100–200 m
No polar ice sheets
Summary and Conclusion
 The present slide show depicts a critical geopolitical issue that humanity had never to face at
a planetary scale.The issue is climate change and its impact on human civilization. Is it true
that climate is changing today and what will climate bring to future generations? What are the
causes and mechanisms? Can the change become dangerous or catastrophic and when? Can
dangerous climate change be prevented or reversed?
 Science is convincing, climate is changing across our Planet and the change is largely due to
human activities. The change is detectable in all components of the climate system: warming of
land and sea surface,increase in ocean heat content, retreat of land and sea ice, sea level rise,ocean
acidification,and weather extremes. Certain regions become wetter,while others dryer. Global
warming means a rise in the yearly average surface temperature over the globe (1.5 °C since the
end of the 18th century) and an increase in the number of very hot days. In a warmerWorld,certain
regions can temporarily be colder than normal for that location, but at any given time areas with
higher temperatures exceed by far the areas with a temperature lower than normal. There is
no place on Earth where average yearly temperature is decreasing with statistical significance.
 Although natural processes often changed climate during Earth’s history,they cannot explain the
present changes, nor can changes in solar radiation be invoked.The present change is caused
primarily by an ever-increasing fossil fuel consumption and deforestation during the Industrial
Era,which enhanced the concentration of greenhouse gases in the atmosphere and of black
carbon dust at a rate much faster than the Earth can recycle.According to the laws of physics, the
consequence is increased longwave radiation, resulting in warming. Global warming,in turn,
causes melting of ice, sea level rise and extreme weather events. CO2 is the primary anthropogenic
warming factor,followed by methane, black carbon dust and ozone. The actual level of CO2 in the
atmosphere is ~400 ppm, which is 43 % above the preindustrial level of 280 ppm. Empirical data from
today and the past, and simulations in climate models have shown that doubling atmospheric CO2
results in a 2.6–4.1°C global warming.This is ~3 times more than expected from CO2 alone,because
radiative forcing of the latter is enhanced by water vapor,clouds, and ice sheet feedbacks.
 Climate change is modulated by natural variability.El Niño augments the warming rate,while La Niña
attenuates the trend.The last decade may have experienced less warming due to more La Niña, a small
decrease in solar radiation (sun spots),increased vulcanic aerosols and a recent cooling in the
eastern equatorial Pacific.
 Climate change is characterized by the phenomenon of inertia, commitment and irreversibility. It
takes several decades before warming of a given amount of CO2 is realized but the change is
committed to appear and to remain for at least 1000 years once established.
 Although negative impacts of climate change are already being seen today, they do not frighten people
yet in large parts of theWorld, but people will inevitably become frightened by the end of this
century. Large ensembles of climate models predict that, in the worst case scenario of continuously
increasing fossil fuel use (RCP8.5 scenario),average global temperature would be ~4 °C higher in 2100
relative to 1990. Average land surface temperature would be 6°C higher in theTropics and Subtropics.
That means that in those regions average temperature over land would be 26-36 °C instead of 20-
30°C today.Temperature extremes will be up to 11 °C higher than now and will occur more
frequently all over theWorld.Cities will experience even more warming as they heat more than the
v
surrounding land. By 2300 average global temperature would be 8 °C higher, with an upper
bound of 10 °C. Since the limit of sustained wet bulb temperature*,above which the human body can
no longer adequately cool, is 35 °C, and since a 10 °C rise in average surface temperature may
result in a wet-bulb temperature of 35 °C in many tropical and subtropical regions,where more than
40% of Earth`s population lives, a worst case scenario warming (RCP8.5) will have strong and
widespread devastating impacts on human society by 2300. Moreover,much of this warming will
persist for more than 1000 years,even if emissions are set to zero at that time. On top of this, sea
level rise, storms, droughts,wildfires,floods, climate refugee problems and food shortage will
exacerbate the situation.
 Will climate change become catastrophic?
In assessing the severity of future climate change several observations appear to argue against a
catastrophic development. 1) Sudden warming or cooling events of a similar magnitude as that
projected now under an RCP8.5 scenario, occurred often during the last Ice Age and during the
transition to the Holocene.Temperature change occurred sometimes even at a faster rate than today.
Nevertheless,Homo Sapiens evolved and spread over the globe during these harsh climate changes,
suggesting that rapid warming or cooling is not incompatible with human development.
Moreover,modern humans have scientific and technical capabilities for adaptation that our ancestors
did not have. 2) Under a 4 °C warming scenario, sea level rise will force people to be displaced and
migrate,but his process will be gradual over 2000 years and is limited to 10 m, allowing time to
adapt. 3) Reconstructions of palaeoclimates have shown that, millions of years ago, surface ocean pH
* Wet bulb temperature is the temperature indicated by a moistened thermometer bulb exposed to the air flow. If relative humidity is 100%,
wet bulb temperature equals air temperature. The lower the humidity, the higher the difference between both.
was 7.4 and then increased to the present value of 8.2.This suggests that ocean ecosystems might
adapt to a more acid ocean than that today.
The above assumptions,however, are misleading for several reasons. 1) Models predict that the upper
limit of viable temperature for humans (wet-bulb temperature of 35 °C) will be reached in regions of
theTropics and Subtropics if there is a 10 °C rise of the average global temperature (air
temperature).This temperature rise is not impossible under the RCP8.5 worst case scenario,
although it will probably not be reached before 2300. 2) Although there have been palaeoclimates,
such as the PETM and the EECO,with similar high temperatures,fossil data indicate that mammals
at those epochs were small (average 1 kg),making their surface to body mass ratio larger,hereby
improving their body cooling and hence enabling them to tolerate higher temperatures. Moreover,
anthropogenic warming today and in the future is at a much faster pace than during the PETM epoch,
making adaptation through biological evolution very unlikely. 3) A 10 °C warming will likely also
melt the Antarctic ice sheet, which would raise sea level by at least 50 m. 4) As to ocean pH,it
remains uncertain over which time scales biotic adaptation is feasible.Moreover, acidification acts
in synergy with the decline of oxygen and nutrient in the oceans, creating non-linear adverse
effects on ecosystems. 5) Last but not least, future climate change impacts may act in
synergy with other anthropogenic impacts. Human consumption of the Earth’s resources has
now reached levels exceeding the capacity of the Earth to regenerate several of these resources.[Ref]
These human impacts not only risk to cause shortages in food and materials supply but also to
deteriorate wildlife habitat and ecosystems. Since wildlife and ecosystems services are vital to human
life,their loss, in combination with climate change,could become disruptive to human existence.
Moreover,due to the global connectedness of ecosystems and economies, impacts in one place
can rapidly spread and cause instability in many other regions around theWorld. Finally,the
distribution of climate risks is very uneven, being greatest in the poorest countries which also are
the least responsible for greenhouse gas emissions. Inequity threatens political and social
stability, which may become flashpoints for ecological and human disaster. Thus,if temperature rise
remains unabated,climate change has the potential to become catastrophic by the end of this
century and even make large parts of the Planet inhabitable for humans by 2300.
 What should be done? Since the main cause of global warming is radiative forcing from the ~500
gigatons CO2 that humans releasedin the atmosphere,the direct solution is removing CO2 and
lowering global temperature by solar radiation management.Theoretical and small scale
methods exist but the efficacy, permanency and safety of these methods at a planetary scale remain
unsufficiently known.Until climate change can be fixed we ought to adapt to the change by building
resilience against climate impacts and reduce CO2 emissions to mitigate the aggressiveness of
climate in the future.The dominant current approach is stabilizing CO2 in the atmosphere at the
presumptive safe level below 450 ppm.This is believed (but not proven) to limit global average
temperature rise to 2ºC above preindustrial level and to keep it at that level. However,in
order to attain this target,a ~70 % reduction of greenhouse gas emissions is needed
worldwide by 2050 and low carbon renewable energy facilities should largely replace fossil fuel
energy.Emission cuts are also necessary to fix the serious health issue caused by pollution from
fossil fuel burning.
 Not to forget, cutting emissions will not reverse committed climate change and in case we fail to
meet the 70 % emission cuts rapidly,temperature will continue to rise.The longer it takes to
stabilize climate,the higher the chance that unforeseen climate feedbacks may develop,creating new
problems with potentially more dangerous consequences.Therefore,much more research attention
should be devoted to CO2 removal technology, solar radiation management and
strategies of adaptation to a warmerWorld, particularly since it is not for granted that stabilizing
atmospheric CO2 at 450 ppm is a safe bound. Indeed,during the Pliocene epoch CO2 levels were
similar to present levels, yet, average global temperature rose 3-4 °C, not 2 °C as anticipated now.
Another effective measure for cooling the atmosphere could be the drastic reduction of non-
CO2 greenhouse gas and black carbon emissions as the residence time of these substances in
the atmosphere is relatively short,resulting in more rapid cooling once they lower.
 What is the prognosis of success? Various measures to reduce greenhouse gas levels have been
implemented worldwide. However,global initiatives, such as the Kyoto protocol and UNFCCC
agreements,are still far removed from what is needed to meet the 2 °C target.Reticence and
inertia of governments and the general public impede progress. As the climate problem is
unprecedented, there is no experience to rely on.The average citizen does not feel responsible or is
locked in the existing consumer and individualistic society. Government decisions are often
dominated by particracy. Although the free market easily got global,the nationalistic reflex of self-
preservation still prevails over a global cooperative approach to the climate problem. Climate
mitigation efforts,such as the carbon credit system, are often misused. There is malicious
misleading by big companies that fund the undermining of climate science for the sake of short-
term viewed core business profits.[Ref1][Ref2] Climate change denials and biased or wrong
information about climate by Fox News in the U.S. ,[Ref][Ref][Ref] is seriously misleading public
opinion.Countries like the U.S. put strong emphasis on controversial shale gas exploitation but keep
eyes closed for the adverse effect that it brakes the incentive for renewable carbon-poor energy
development and that it has negative impacts on the environment.
A positive outlook, however, is that fusion and hydrogen energy may take over the World primary
energy production during the next century. Replacing nuclear reactors by fast breeder reactors is an
additional option to avoid further CO2 accumulation, an approach advocated even by some climate
activists.[Ref]
 The final message.
In search of explaining their physical environment, modern humans discovered carbon-rich energy, that
allowed them to produce and consume goods at intensities far above what is needed to fulfill basic
needs for existence and prosperity.This is an astonishing paradox as all cultures originally developed
intuitive understanding of limitation, the frailty of existence and the sacredness of natural environments.
In search of prosperity modern civilization has forgotten what intuition had learned.The tools designed
to acquire prosperity have now turned against the designer. However, human beings have a special gift, a
gift that distinguishes them from all other living systems, and that is our special relationship to the laws
of physics, our special ability to create explanations on the basis of these laws and using only energy and
matter.That special gift allows us to discover problems that we caused ourselves and to find the
evidence to explain and resolve those problems. In a World of ever increasing knowledge problems are
inevitable but problems are solvable.[Ref] Our vulnerability is not the failure of getting a solution, but the
failure of getting it in time. If we don’t nurture our gift, we deny our nature and we will disappear.
Therefore, it is crucial to create more knowledge, to make people understand what is known
and to foster a renaissance of human existence.
 I end with a few quotes, as I think they are relevant to the origin of the climate crisis and to
encouraging to urgently work at a solution.
Every problem that is interesting is
also soluble.
Inherently insoluble problems are
inherently boring.
David Deutsch
[Ref]
I cannot command winds and weather
Horatio Nelson

Weitere ähnliche Inhalte

Was ist angesagt?

Climate change
Climate changeClimate change
Climate changeAnkit Pal
 
Global warning and climate change
Global warning and climate change Global warning and climate change
Global warning and climate change Dipak Kumar
 
Introduction to Environmental Science
Introduction to Environmental ScienceIntroduction to Environmental Science
Introduction to Environmental Sciencewtidwell
 
Land and sea breeze
Land and sea breezeLand and sea breeze
Land and sea breezechampa1
 
Climate change
Climate changeClimate change
Climate changeAlex Walsh
 
Climate change A Presentation By Mr Allah Dad Khan Former Director General A...
Climate change  A Presentation By Mr Allah Dad Khan Former Director General A...Climate change  A Presentation By Mr Allah Dad Khan Former Director General A...
Climate change A Presentation By Mr Allah Dad Khan Former Director General A...Mr.Allah Dad Khan
 
Volcano ppt
Volcano pptVolcano ppt
Volcano pptgowri159
 
Basic of Climate Change
Basic of Climate ChangeBasic of Climate Change
Basic of Climate ChangeAli Abassi
 
Factors affecting climate
Factors affecting climateFactors affecting climate
Factors affecting climateSteven Heath
 
The greenhouse effect
The greenhouse effectThe greenhouse effect
The greenhouse effectRachel Espino
 
Climate change & global warming consequenses
Climate change & global warming consequensesClimate change & global warming consequenses
Climate change & global warming consequensesVreshgouda Vru
 
Climate and Ocean Currents
Climate and Ocean CurrentsClimate and Ocean Currents
Climate and Ocean Currentsdwinter1
 

Was ist angesagt? (20)

Climate change
Climate changeClimate change
Climate change
 
Global warning and climate change
Global warning and climate change Global warning and climate change
Global warning and climate change
 
Causes of climate change
Causes of climate changeCauses of climate change
Causes of climate change
 
Climate Change
Climate ChangeClimate Change
Climate Change
 
Climate change
Climate changeClimate change
Climate change
 
Introduction to Environmental Science
Introduction to Environmental ScienceIntroduction to Environmental Science
Introduction to Environmental Science
 
Land and sea breeze
Land and sea breezeLand and sea breeze
Land and sea breeze
 
Climate change
Climate changeClimate change
Climate change
 
Climate change A Presentation By Mr Allah Dad Khan Former Director General A...
Climate change  A Presentation By Mr Allah Dad Khan Former Director General A...Climate change  A Presentation By Mr Allah Dad Khan Former Director General A...
Climate change A Presentation By Mr Allah Dad Khan Former Director General A...
 
Volcano ppt
Volcano pptVolcano ppt
Volcano ppt
 
Basic of Climate Change
Basic of Climate ChangeBasic of Climate Change
Basic of Climate Change
 
Factors affecting climate
Factors affecting climateFactors affecting climate
Factors affecting climate
 
Climate
ClimateClimate
Climate
 
The greenhouse effect
The greenhouse effectThe greenhouse effect
The greenhouse effect
 
Climate change & global warming consequenses
Climate change & global warming consequensesClimate change & global warming consequenses
Climate change & global warming consequenses
 
Global Warming
Global WarmingGlobal Warming
Global Warming
 
Volcanic Eruption
Volcanic Eruption Volcanic Eruption
Volcanic Eruption
 
Climate and Ocean Currents
Climate and Ocean CurrentsClimate and Ocean Currents
Climate and Ocean Currents
 
Causes and effects of climate change
Causes and effects of climate changeCauses and effects of climate change
Causes and effects of climate change
 
Global warming
Global warmingGlobal warming
Global warming
 

Andere mochten auch

Conclusion
ConclusionConclusion
ConclusionGuadyssG
 
Global warming causes and effects
Global warming causes and effectsGlobal warming causes and effects
Global warming causes and effectshzrq
 
Jagan global warming
Jagan global warming Jagan global warming
Jagan global warming jaganshettar
 
Impact of human on climate conclusion
Impact of human on climate conclusionImpact of human on climate conclusion
Impact of human on climate conclusionhome
 
Climate change powerpoint
Climate change powerpointClimate change powerpoint
Climate change powerpointpacorz
 
A Presentation on Global Warming
A Presentation on Global WarmingA Presentation on Global Warming
A Presentation on Global WarmingJayant Gope
 
Fixing climate change
Fixing climate changeFixing climate change
Fixing climate changecdenef
 
16. global warming(anil chari)
16. global warming(anil chari)16. global warming(anil chari)
16. global warming(anil chari)Anil Mrperfect
 
Deforestation andré
Deforestation andréDeforestation andré
Deforestation andréepg
 
Impact of climate change on Moroccan agriculture
Impact of climate change on Moroccan agricultureImpact of climate change on Moroccan agriculture
Impact of climate change on Moroccan agricultureICARDA
 
Global Warming, Acid Rain, and Ozone Depletion
Global Warming, Acid Rain, and Ozone DepletionGlobal Warming, Acid Rain, and Ozone Depletion
Global Warming, Acid Rain, and Ozone Depletionddsheppard
 
Global Warming Presentation
Global Warming PresentationGlobal Warming Presentation
Global Warming Presentationj3228107
 

Andere mochten auch (20)

Conclusion
ConclusionConclusion
Conclusion
 
Global Warming Ppt
Global Warming PptGlobal Warming Ppt
Global Warming Ppt
 
Global warming causes and effects
Global warming causes and effectsGlobal warming causes and effects
Global warming causes and effects
 
Jagan global warming
Jagan global warming Jagan global warming
Jagan global warming
 
Global warming (EVS Project)
Global warming (EVS Project)Global warming (EVS Project)
Global warming (EVS Project)
 
Impact of human on climate conclusion
Impact of human on climate conclusionImpact of human on climate conclusion
Impact of human on climate conclusion
 
Climate change powerpoint
Climate change powerpointClimate change powerpoint
Climate change powerpoint
 
A Presentation on Global Warming
A Presentation on Global WarmingA Presentation on Global Warming
A Presentation on Global Warming
 
Fixing climate change
Fixing climate changeFixing climate change
Fixing climate change
 
Global Warming
Global WarmingGlobal Warming
Global Warming
 
16. global warming(anil chari)
16. global warming(anil chari)16. global warming(anil chari)
16. global warming(anil chari)
 
P2 GLOBAL WARMING PROJECT (F-TIER CLASS)
P2 GLOBAL WARMING PROJECT (F-TIER CLASS)P2 GLOBAL WARMING PROJECT (F-TIER CLASS)
P2 GLOBAL WARMING PROJECT (F-TIER CLASS)
 
Deforestation andré
Deforestation andréDeforestation andré
Deforestation andré
 
Glochamore Dieback1.0
Glochamore Dieback1.0Glochamore Dieback1.0
Glochamore Dieback1.0
 
Global climate change facts
Global climate change factsGlobal climate change facts
Global climate change facts
 
Global warming assignment
Global warming assignmentGlobal warming assignment
Global warming assignment
 
Impact of climate change on Moroccan agriculture
Impact of climate change on Moroccan agricultureImpact of climate change on Moroccan agriculture
Impact of climate change on Moroccan agriculture
 
Global Warming, Acid Rain, and Ozone Depletion
Global Warming, Acid Rain, and Ozone DepletionGlobal Warming, Acid Rain, and Ozone Depletion
Global Warming, Acid Rain, and Ozone Depletion
 
Global Warming Presentation
Global Warming PresentationGlobal Warming Presentation
Global Warming Presentation
 
Flooding Farming & Climate Change - Engagement of Gloucestershire Farmers
Flooding Farming & Climate Change - Engagement of Gloucestershire Farmers Flooding Farming & Climate Change - Engagement of Gloucestershire Farmers
Flooding Farming & Climate Change - Engagement of Gloucestershire Farmers
 

Ähnlich wie Climate change summary and conclusions

Global_warming_presentation.pptx
Global_warming_presentation.pptxGlobal_warming_presentation.pptx
Global_warming_presentation.pptxviveksingh20861
 
Global warming ppt tanya
Global warming ppt tanyaGlobal warming ppt tanya
Global warming ppt tanyashalinisharmaa
 
New Microsoft Office Word Document
New Microsoft Office Word DocumentNew Microsoft Office Word Document
New Microsoft Office Word DocumentSourav Ghosh
 
Poteplenie klimata O. Gunder_11-b
Poteplenie klimata O. Gunder_11-bPoteplenie klimata O. Gunder_11-b
Poteplenie klimata O. Gunder_11-bJulia Birhova
 
Global Warming And Renewable Energy
Global Warming And Renewable EnergyGlobal Warming And Renewable Energy
Global Warming And Renewable EnergyDaniel Rivera
 
Savulescu Ionut-Viorel
Savulescu Ionut-ViorelSavulescu Ionut-Viorel
Savulescu Ionut-Viorelmicutsu
 
Quick guide-Environment
Quick guide-EnvironmentQuick guide-Environment
Quick guide-Environmenthelenmazarron
 
Dr Ronald L Sass Lead Conf
Dr Ronald L Sass Lead ConfDr Ronald L Sass Lead Conf
Dr Ronald L Sass Lead ConfPaul Suckow
 
Changing Climatic Factors
Changing Climatic FactorsChanging Climatic Factors
Changing Climatic FactorsManisha Tanwar
 
Global warming
Global warmingGlobal warming
Global warmingreshmafmtc
 
Global warming
Global warmingGlobal warming
Global warmingreshmafmtc
 

Ähnlich wie Climate change summary and conclusions (20)

Global_warming_presentation.pptx
Global_warming_presentation.pptxGlobal_warming_presentation.pptx
Global_warming_presentation.pptx
 
Global warming
Global warmingGlobal warming
Global warming
 
Shashank
ShashankShashank
Shashank
 
Global warming ppt tanya
Global warming ppt tanyaGlobal warming ppt tanya
Global warming ppt tanya
 
New Microsoft Office Word Document
New Microsoft Office Word DocumentNew Microsoft Office Word Document
New Microsoft Office Word Document
 
Global warming effects
Global warming effectsGlobal warming effects
Global warming effects
 
Poteplenie klimata O. Gunder_11-b
Poteplenie klimata O. Gunder_11-bPoteplenie klimata O. Gunder_11-b
Poteplenie klimata O. Gunder_11-b
 
Global Warming And Renewable Energy
Global Warming And Renewable EnergyGlobal Warming And Renewable Energy
Global Warming And Renewable Energy
 
Savulescu Ionut-Viorel
Savulescu Ionut-ViorelSavulescu Ionut-Viorel
Savulescu Ionut-Viorel
 
Quick guide-Environment
Quick guide-EnvironmentQuick guide-Environment
Quick guide-Environment
 
Dr Ronald L Sass Lead Conf
Dr Ronald L Sass Lead ConfDr Ronald L Sass Lead Conf
Dr Ronald L Sass Lead Conf
 
Global Warming
Global WarmingGlobal Warming
Global Warming
 
Changing Climatic Factors
Changing Climatic FactorsChanging Climatic Factors
Changing Climatic Factors
 
energy security1
energy security1energy security1
energy security1
 
Global warming
Global warmingGlobal warming
Global warming
 
Climate change
Climate changeClimate change
Climate change
 
Global Warming 2
Global Warming 2Global Warming 2
Global Warming 2
 
Global warming
Global warmingGlobal warming
Global warming
 
Global warming
Global warmingGlobal warming
Global warming
 
Global warming
Global warmingGlobal warming
Global warming
 

Mehr von cdenef

Renewable energy
Renewable energyRenewable energy
Renewable energycdenef
 
climate change in the past: Palaeoclimate
climate change in the past: Palaeoclimateclimate change in the past: Palaeoclimate
climate change in the past: Palaeoclimatecdenef
 
Nuclear energy
Nuclear energyNuclear energy
Nuclear energycdenef
 
Fossil energy
Fossil energyFossil energy
Fossil energycdenef
 
Climate change: Extreme weather events
Climate change: Extreme weather eventsClimate change: Extreme weather events
Climate change: Extreme weather eventscdenef
 
Energy costs
Energy costsEnergy costs
Energy costscdenef
 
Climate change prediction
Climate change predictionClimate change prediction
Climate change predictioncdenef
 
Climate change: changes in the cryosphere
Climate change: changes in the cryosphereClimate change: changes in the cryosphere
Climate change: changes in the cryospherecdenef
 
Climate change: Changes in the hydrosphere
Climate change: Changes in the hydrosphereClimate change: Changes in the hydrosphere
Climate change: Changes in the hydrospherecdenef
 
Climate change: Changes in the biosphere
Climate change: Changes in the biosphereClimate change: Changes in the biosphere
Climate change: Changes in the biospherecdenef
 
Climate change: Changes in the atmosphere
Climate change: Changes in the atmosphereClimate change: Changes in the atmosphere
Climate change: Changes in the atmospherecdenef
 
Changes in the atmosphere
Changes in the atmosphereChanges in the atmosphere
Changes in the atmospherecdenef
 
Key concepts in Climate Science
Key concepts in Climate  ScienceKey concepts in Climate  Science
Key concepts in Climate Sciencecdenef
 
Energy production & consumption
Energy production & consumptionEnergy production & consumption
Energy production & consumptioncdenef
 
Energy in everyday life
Energy in everyday lifeEnergy in everyday life
Energy in everyday lifecdenef
 

Mehr von cdenef (15)

Renewable energy
Renewable energyRenewable energy
Renewable energy
 
climate change in the past: Palaeoclimate
climate change in the past: Palaeoclimateclimate change in the past: Palaeoclimate
climate change in the past: Palaeoclimate
 
Nuclear energy
Nuclear energyNuclear energy
Nuclear energy
 
Fossil energy
Fossil energyFossil energy
Fossil energy
 
Climate change: Extreme weather events
Climate change: Extreme weather eventsClimate change: Extreme weather events
Climate change: Extreme weather events
 
Energy costs
Energy costsEnergy costs
Energy costs
 
Climate change prediction
Climate change predictionClimate change prediction
Climate change prediction
 
Climate change: changes in the cryosphere
Climate change: changes in the cryosphereClimate change: changes in the cryosphere
Climate change: changes in the cryosphere
 
Climate change: Changes in the hydrosphere
Climate change: Changes in the hydrosphereClimate change: Changes in the hydrosphere
Climate change: Changes in the hydrosphere
 
Climate change: Changes in the biosphere
Climate change: Changes in the biosphereClimate change: Changes in the biosphere
Climate change: Changes in the biosphere
 
Climate change: Changes in the atmosphere
Climate change: Changes in the atmosphereClimate change: Changes in the atmosphere
Climate change: Changes in the atmosphere
 
Changes in the atmosphere
Changes in the atmosphereChanges in the atmosphere
Changes in the atmosphere
 
Key concepts in Climate Science
Key concepts in Climate  ScienceKey concepts in Climate  Science
Key concepts in Climate Science
 
Energy production & consumption
Energy production & consumptionEnergy production & consumption
Energy production & consumption
 
Energy in everyday life
Energy in everyday lifeEnergy in everyday life
Energy in everyday life
 

Kürzlich hochgeladen

Measures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDMeasures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDThiyagu K
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphThiyagu K
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhikauryashika82
 
Student login on Anyboli platform.helpin
Student login on Anyboli platform.helpinStudent login on Anyboli platform.helpin
Student login on Anyboli platform.helpinRaunakKeshri1
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeThiyagu K
 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13Steve Thomason
 
social pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajansocial pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajanpragatimahajan3
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Disha Kariya
 
Sanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdfSanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdfsanyamsingh5019
 
Interactive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communicationInteractive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communicationnomboosow
 
9548086042 for call girls in Indira Nagar with room service
9548086042  for call girls in Indira Nagar  with room service9548086042  for call girls in Indira Nagar  with room service
9548086042 for call girls in Indira Nagar with room servicediscovermytutordmt
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfciinovamais
 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Sapana Sha
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxiammrhaywood
 
APM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across SectorsAPM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across SectorsAssociation for Project Management
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingTeacherCyreneCayanan
 
microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introductionMaksud Ahmed
 

Kürzlich hochgeladen (20)

Measures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDMeasures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SD
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot Graph
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
 
Student login on Anyboli platform.helpin
Student login on Anyboli platform.helpinStudent login on Anyboli platform.helpin
Student login on Anyboli platform.helpin
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and Mode
 
The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13The Most Excellent Way | 1 Corinthians 13
The Most Excellent Way | 1 Corinthians 13
 
social pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajansocial pharmacy d-pharm 1st year by Pragati K. Mahajan
social pharmacy d-pharm 1st year by Pragati K. Mahajan
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..
 
Sanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdfSanyam Choudhary Chemistry practical.pdf
Sanyam Choudhary Chemistry practical.pdf
 
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptxINDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
INDIA QUIZ 2024 RLAC DELHI UNIVERSITY.pptx
 
Interactive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communicationInteractive Powerpoint_How to Master effective communication
Interactive Powerpoint_How to Master effective communication
 
9548086042 for call girls in Indira Nagar with room service
9548086042  for call girls in Indira Nagar  with room service9548086042  for call girls in Indira Nagar  with room service
9548086042 for call girls in Indira Nagar with room service
 
Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
 
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111Call Girls in Dwarka Mor Delhi Contact Us 9654467111
Call Girls in Dwarka Mor Delhi Contact Us 9654467111
 
Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1
 
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptxSOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
SOCIAL AND HISTORICAL CONTEXT - LFTVD.pptx
 
Advance Mobile Application Development class 07
Advance Mobile Application Development class 07Advance Mobile Application Development class 07
Advance Mobile Application Development class 07
 
APM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across SectorsAPM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across Sectors
 
fourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writingfourth grading exam for kindergarten in writing
fourth grading exam for kindergarten in writing
 
microwave assisted reaction. General introduction
microwave assisted reaction. General introductionmicrowave assisted reaction. General introduction
microwave assisted reaction. General introduction
 

Climate change summary and conclusions

  • 1. Summary and Conclusion Carl Denef, January 2014
  • 2. Despite the threat of the climate crisis, global emissions of CO2 are set to rise again in 2013, reaching a record high of 36 gigatonnes. Gigatonnes C02
  • 3. Overview of past, present and future climate change Era Global average temperature anomaly Atm. CO2 (ppm) Sea level vs preindustrial In 2100 (RCP8.5 scenario) 2.8–5.5 ºC vs preindustrial 1200 0.5–1 m Present 1.5 ºC vs preindustrial 395 0.3 m 8.2 ka event 2–3 ºC in 2 decades 275 Younger Dryas 7-8 ºC in 1 decade in Greenland and N-Atlantic, followed by abrupt 250 D-O events 4–6 ºC in decades from ~200 to 220 Last Glacial Maximum 3–8 ºC vs preindustrial 190 120 m Last Interglacial 1–2 ºC vs preindustrial 280 5.5–9 m Less Greenland ice sheet MIS-11 Interglacial 1.5–2.0 ºC vs preindustrial 280 6–20 m No Greenland ice sheet Older interglacials 2 ºC vs preindustrial 250-280 = preindustrial Mid-pliocene 3–10 ºC vs preindustrial 365-415  7–20 m No Greenland ice sheet PETM 4-7 ºC vs preindustrial Sea surface temp.Tropics = 35 ºC Polar temp. = 10-20 ºC 1125 100–200 m No polar ice sheets
  • 4. Summary and Conclusion  The present slide show depicts a critical geopolitical issue that humanity had never to face at a planetary scale.The issue is climate change and its impact on human civilization. Is it true that climate is changing today and what will climate bring to future generations? What are the causes and mechanisms? Can the change become dangerous or catastrophic and when? Can dangerous climate change be prevented or reversed?  Science is convincing, climate is changing across our Planet and the change is largely due to human activities. The change is detectable in all components of the climate system: warming of land and sea surface,increase in ocean heat content, retreat of land and sea ice, sea level rise,ocean acidification,and weather extremes. Certain regions become wetter,while others dryer. Global warming means a rise in the yearly average surface temperature over the globe (1.5 °C since the end of the 18th century) and an increase in the number of very hot days. In a warmerWorld,certain regions can temporarily be colder than normal for that location, but at any given time areas with higher temperatures exceed by far the areas with a temperature lower than normal. There is no place on Earth where average yearly temperature is decreasing with statistical significance.  Although natural processes often changed climate during Earth’s history,they cannot explain the present changes, nor can changes in solar radiation be invoked.The present change is caused primarily by an ever-increasing fossil fuel consumption and deforestation during the Industrial Era,which enhanced the concentration of greenhouse gases in the atmosphere and of black carbon dust at a rate much faster than the Earth can recycle.According to the laws of physics, the consequence is increased longwave radiation, resulting in warming. Global warming,in turn, causes melting of ice, sea level rise and extreme weather events. CO2 is the primary anthropogenic
  • 5. warming factor,followed by methane, black carbon dust and ozone. The actual level of CO2 in the atmosphere is ~400 ppm, which is 43 % above the preindustrial level of 280 ppm. Empirical data from today and the past, and simulations in climate models have shown that doubling atmospheric CO2 results in a 2.6–4.1°C global warming.This is ~3 times more than expected from CO2 alone,because radiative forcing of the latter is enhanced by water vapor,clouds, and ice sheet feedbacks.  Climate change is modulated by natural variability.El Niño augments the warming rate,while La Niña attenuates the trend.The last decade may have experienced less warming due to more La Niña, a small decrease in solar radiation (sun spots),increased vulcanic aerosols and a recent cooling in the eastern equatorial Pacific.  Climate change is characterized by the phenomenon of inertia, commitment and irreversibility. It takes several decades before warming of a given amount of CO2 is realized but the change is committed to appear and to remain for at least 1000 years once established.  Although negative impacts of climate change are already being seen today, they do not frighten people yet in large parts of theWorld, but people will inevitably become frightened by the end of this century. Large ensembles of climate models predict that, in the worst case scenario of continuously increasing fossil fuel use (RCP8.5 scenario),average global temperature would be ~4 °C higher in 2100 relative to 1990. Average land surface temperature would be 6°C higher in theTropics and Subtropics. That means that in those regions average temperature over land would be 26-36 °C instead of 20- 30°C today.Temperature extremes will be up to 11 °C higher than now and will occur more frequently all over theWorld.Cities will experience even more warming as they heat more than the v
  • 6. surrounding land. By 2300 average global temperature would be 8 °C higher, with an upper bound of 10 °C. Since the limit of sustained wet bulb temperature*,above which the human body can no longer adequately cool, is 35 °C, and since a 10 °C rise in average surface temperature may result in a wet-bulb temperature of 35 °C in many tropical and subtropical regions,where more than 40% of Earth`s population lives, a worst case scenario warming (RCP8.5) will have strong and widespread devastating impacts on human society by 2300. Moreover,much of this warming will persist for more than 1000 years,even if emissions are set to zero at that time. On top of this, sea level rise, storms, droughts,wildfires,floods, climate refugee problems and food shortage will exacerbate the situation.  Will climate change become catastrophic? In assessing the severity of future climate change several observations appear to argue against a catastrophic development. 1) Sudden warming or cooling events of a similar magnitude as that projected now under an RCP8.5 scenario, occurred often during the last Ice Age and during the transition to the Holocene.Temperature change occurred sometimes even at a faster rate than today. Nevertheless,Homo Sapiens evolved and spread over the globe during these harsh climate changes, suggesting that rapid warming or cooling is not incompatible with human development. Moreover,modern humans have scientific and technical capabilities for adaptation that our ancestors did not have. 2) Under a 4 °C warming scenario, sea level rise will force people to be displaced and migrate,but his process will be gradual over 2000 years and is limited to 10 m, allowing time to adapt. 3) Reconstructions of palaeoclimates have shown that, millions of years ago, surface ocean pH * Wet bulb temperature is the temperature indicated by a moistened thermometer bulb exposed to the air flow. If relative humidity is 100%, wet bulb temperature equals air temperature. The lower the humidity, the higher the difference between both.
  • 7. was 7.4 and then increased to the present value of 8.2.This suggests that ocean ecosystems might adapt to a more acid ocean than that today. The above assumptions,however, are misleading for several reasons. 1) Models predict that the upper limit of viable temperature for humans (wet-bulb temperature of 35 °C) will be reached in regions of theTropics and Subtropics if there is a 10 °C rise of the average global temperature (air temperature).This temperature rise is not impossible under the RCP8.5 worst case scenario, although it will probably not be reached before 2300. 2) Although there have been palaeoclimates, such as the PETM and the EECO,with similar high temperatures,fossil data indicate that mammals at those epochs were small (average 1 kg),making their surface to body mass ratio larger,hereby improving their body cooling and hence enabling them to tolerate higher temperatures. Moreover, anthropogenic warming today and in the future is at a much faster pace than during the PETM epoch, making adaptation through biological evolution very unlikely. 3) A 10 °C warming will likely also melt the Antarctic ice sheet, which would raise sea level by at least 50 m. 4) As to ocean pH,it remains uncertain over which time scales biotic adaptation is feasible.Moreover, acidification acts in synergy with the decline of oxygen and nutrient in the oceans, creating non-linear adverse effects on ecosystems. 5) Last but not least, future climate change impacts may act in synergy with other anthropogenic impacts. Human consumption of the Earth’s resources has now reached levels exceeding the capacity of the Earth to regenerate several of these resources.[Ref] These human impacts not only risk to cause shortages in food and materials supply but also to deteriorate wildlife habitat and ecosystems. Since wildlife and ecosystems services are vital to human life,their loss, in combination with climate change,could become disruptive to human existence. Moreover,due to the global connectedness of ecosystems and economies, impacts in one place
  • 8. can rapidly spread and cause instability in many other regions around theWorld. Finally,the distribution of climate risks is very uneven, being greatest in the poorest countries which also are the least responsible for greenhouse gas emissions. Inequity threatens political and social stability, which may become flashpoints for ecological and human disaster. Thus,if temperature rise remains unabated,climate change has the potential to become catastrophic by the end of this century and even make large parts of the Planet inhabitable for humans by 2300.  What should be done? Since the main cause of global warming is radiative forcing from the ~500 gigatons CO2 that humans releasedin the atmosphere,the direct solution is removing CO2 and lowering global temperature by solar radiation management.Theoretical and small scale methods exist but the efficacy, permanency and safety of these methods at a planetary scale remain unsufficiently known.Until climate change can be fixed we ought to adapt to the change by building resilience against climate impacts and reduce CO2 emissions to mitigate the aggressiveness of climate in the future.The dominant current approach is stabilizing CO2 in the atmosphere at the presumptive safe level below 450 ppm.This is believed (but not proven) to limit global average temperature rise to 2ºC above preindustrial level and to keep it at that level. However,in order to attain this target,a ~70 % reduction of greenhouse gas emissions is needed worldwide by 2050 and low carbon renewable energy facilities should largely replace fossil fuel energy.Emission cuts are also necessary to fix the serious health issue caused by pollution from fossil fuel burning.  Not to forget, cutting emissions will not reverse committed climate change and in case we fail to meet the 70 % emission cuts rapidly,temperature will continue to rise.The longer it takes to
  • 9. stabilize climate,the higher the chance that unforeseen climate feedbacks may develop,creating new problems with potentially more dangerous consequences.Therefore,much more research attention should be devoted to CO2 removal technology, solar radiation management and strategies of adaptation to a warmerWorld, particularly since it is not for granted that stabilizing atmospheric CO2 at 450 ppm is a safe bound. Indeed,during the Pliocene epoch CO2 levels were similar to present levels, yet, average global temperature rose 3-4 °C, not 2 °C as anticipated now. Another effective measure for cooling the atmosphere could be the drastic reduction of non- CO2 greenhouse gas and black carbon emissions as the residence time of these substances in the atmosphere is relatively short,resulting in more rapid cooling once they lower.  What is the prognosis of success? Various measures to reduce greenhouse gas levels have been implemented worldwide. However,global initiatives, such as the Kyoto protocol and UNFCCC agreements,are still far removed from what is needed to meet the 2 °C target.Reticence and inertia of governments and the general public impede progress. As the climate problem is unprecedented, there is no experience to rely on.The average citizen does not feel responsible or is locked in the existing consumer and individualistic society. Government decisions are often dominated by particracy. Although the free market easily got global,the nationalistic reflex of self- preservation still prevails over a global cooperative approach to the climate problem. Climate mitigation efforts,such as the carbon credit system, are often misused. There is malicious misleading by big companies that fund the undermining of climate science for the sake of short- term viewed core business profits.[Ref1][Ref2] Climate change denials and biased or wrong information about climate by Fox News in the U.S. ,[Ref][Ref][Ref] is seriously misleading public opinion.Countries like the U.S. put strong emphasis on controversial shale gas exploitation but keep
  • 10. eyes closed for the adverse effect that it brakes the incentive for renewable carbon-poor energy development and that it has negative impacts on the environment. A positive outlook, however, is that fusion and hydrogen energy may take over the World primary energy production during the next century. Replacing nuclear reactors by fast breeder reactors is an additional option to avoid further CO2 accumulation, an approach advocated even by some climate activists.[Ref]  The final message. In search of explaining their physical environment, modern humans discovered carbon-rich energy, that allowed them to produce and consume goods at intensities far above what is needed to fulfill basic needs for existence and prosperity.This is an astonishing paradox as all cultures originally developed intuitive understanding of limitation, the frailty of existence and the sacredness of natural environments. In search of prosperity modern civilization has forgotten what intuition had learned.The tools designed to acquire prosperity have now turned against the designer. However, human beings have a special gift, a gift that distinguishes them from all other living systems, and that is our special relationship to the laws of physics, our special ability to create explanations on the basis of these laws and using only energy and matter.That special gift allows us to discover problems that we caused ourselves and to find the evidence to explain and resolve those problems. In a World of ever increasing knowledge problems are inevitable but problems are solvable.[Ref] Our vulnerability is not the failure of getting a solution, but the failure of getting it in time. If we don’t nurture our gift, we deny our nature and we will disappear. Therefore, it is crucial to create more knowledge, to make people understand what is known and to foster a renaissance of human existence.
  • 11.  I end with a few quotes, as I think they are relevant to the origin of the climate crisis and to encouraging to urgently work at a solution. Every problem that is interesting is also soluble. Inherently insoluble problems are inherently boring. David Deutsch [Ref] I cannot command winds and weather Horatio Nelson