Global Warming Global Warming Prediction Prediction L. David Roper L. David Roper Professor Emeritus of Physics Professor Emeritus of Physics Virginia Polytechnic Inst. & St. Univ. Virginia Polytechnic Inst. & St. Univ. [email protected][email protected]http://arts.bev.net/RoperLDavid http://arts.bev.net/RoperLDavid http://www.roperld.com/science/ http://www.roperld.com/science/ GlobalWarmingPrediction.htm GlobalWarmingPrediction.htm Global Warming and Peak Oil may be the greatest challenges that humans have encountered in the last 10,000 years.
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Global WarmingGlobal WarmingPredictionPrediction
L. David RoperL. David RoperProfessor Emeritus of PhysicsProfessor Emeritus of Physics
Virginia Polytechnic Inst. & St. Univ.Virginia Polytechnic Inst. & St. Univ.
Global Warming and Peak Oil may be the greatest challenges that humans have encountered in the last
10,000 years.
Global Warming PredictionGlobal Warming Prediction It is very important to account for fossil-fuels It is very important to account for fossil-fuels
depletion when calculating Global Warming depletion when calculating Global Warming predictions.predictions.
Otherwise, it might be assumed that more Otherwise, it might be assumed that more carbon can be put into the atmosphere from carbon can be put into the atmosphere from burning fossil fuels than physically possible.burning fossil fuels than physically possible.
Calculating fossil-fuels depletion is not exact, Calculating fossil-fuels depletion is not exact, but can be estimated reasonably well.but can be estimated reasonably well.
Fossil Fuels Global WarmingFossil Fuels Global Warming Fit depletion curves to extraction data for coal, Fit depletion curves to extraction data for coal,
crude oil and natural gas using discoveries data crude oil and natural gas using discoveries data and reserves estimates.and reserves estimates.
Calculate the carbon emitted due to burning fossil Calculate the carbon emitted due to burning fossil fuels and the COfuels and the CO22 concentration in the concentration in the
atmosphere, accounting for residence time.atmosphere, accounting for residence time. Calculate the Earth temperature due to the COCalculate the Earth temperature due to the CO22 in in
the atmosphere, including time lag.the atmosphere, including time lag. Consider triggering of other effects that raise Consider triggering of other effects that raise
temperature, including temperature feedbacks temperature, including temperature feedbacks that increase COthat increase CO22 concentration. concentration.
12
1
12
2 1 exp
1 2 1 exp
nn
n
n
t t
QP t
n t t
Verhulst Function for resources depletion.
Verhulst Function: An asymmetric peaked curve.
Q = amount already extracted + amount left to be extracted =
total amount to be extracted
n ≠ 1 allows asymmetry.
Peak OilOil discoveries will not allow higher average
extraction.
Skewed toward later times.
You can’t extract it if you have You can’t extract it if you have not discovered it!not discovered it!
The areas under the two curves are the same: ~2x1012 barrels.
Areas under both curves are the same.That is, the amount discovered equals the amount extracted.
discoveries
extraction
Gas discoveries will not allow higher average
extraction.
Peak Gas
Skewed toward later times.
You can’t extract it if you have You can’t extract it if you have not discovered it!not discovered it!
The areas under the two curves are the same: ~8x1015 cu. ft.
Areas under both curves are the same.That is, the amount discovered equals the amount extracted.discoveries
Double known coal. Unlikely!
Known existent coal (EIA)
Peaks between 2060 & 2100
Factors and AssumptionsFactors and Assumptions Coal = 50% carbon, short ton = 0.907 tonnesCoal = 50% carbon, short ton = 0.907 tonnes Crude oil = 84% carbon, bbl = 0.136 tonnesCrude oil = 84% carbon, bbl = 0.136 tonnes Natural gas = 76% carbon, tcf = 0.0189 tonnesNatural gas = 76% carbon, tcf = 0.0189 tonnes COCO22 concentration in ppmv = concentration in ppmv = 0.470.47 x gigatonnes x gigatonnes
carbon emitted (may increase with high carbon emitted (may increase with high concentration; i.e., may be nonlinear; see later)concentration; i.e., may be nonlinear; see later)
Climate sensitivity = Climate sensitivity = 3°C3°C for doubling CO for doubling CO22
25% of fossil fuels are used to make useful 25% of fossil fuels are used to make useful materials or are lost instead of being burned.materials or are lost instead of being burned.
Background year 1700 COBackground year 1700 CO22 concentration = concentration = 280 280
ppmvppmv
20% left after 250 years
10% left after 2000 years
6% left after 10,000 years
Equation for CO2 left in nth year for emissions in all previous years.
1
0.0875exp 0.165exp 0.733exp35600 682 50.8
where factor (0.47x0.84 for crude oil) and amount burned at time in gigatonnes.
nn i n i n i
n ii
i i
t t t t t tC t g E t
g E t t
Coal CO2 emissions and CO2 concentration contribution.
Shift in ppmv is due to CO2 residence time.
Crude-oil CO2 emissions and CO2 concentration contribution.
Shift in ppmv is due to CO2 residence time.
Natural-Gas CO2 emissions and CO2 concentration contribution.
Shift in ppmv is due to CO2 residence time.
Fossil-Fuels CO2 emissions and CO2 concentration contribution.
CO2 concentration due to Fossil-Fuels burning
Peaks at about 2110.
CO2 concentration due to Fossil-Fuels burning + background
Fit of COFit of CO2 2 Concentration Data to Concentration Data to
Fossil-Fuels EmissionsFossil-Fuels Emissions
Pre-fossil-fuels industrialization
NFF=14% of FF
CO2 concentration due to Fossil-Fuels burning + Non-fossil-fuels sources;latter assumed proportional to fossil-fuels concentration.
CO2 concentration due to Fossil-Fuels burning + Non-fossil-fuels + background
465 ppmv
Carbon-dioxide concentration due to burning fossil fuels with non-fossil fuels emissions,
assuming that no Earth states are triggered.
It peaks at about 2100 instead of rising into the next century as many assume.
Climate Sensitivity (s)Climate Sensitivity (s)Earth average atmospheric temperature rise Earth average atmospheric temperature rise
due to doubling the carbon-dioxide due to doubling the carbon-dioxide concentration in the atmosphere. Accounts concentration in the atmosphere. Accounts for fast feedbacks, such as ice melting.for fast feedbacks, such as ice melting.
The average is The average is about 3 degrees Celsiusabout 3 degrees Celsius..
It must be applied each year using the carbon-It must be applied each year using the carbon-dioxide concentration for that year.dioxide concentration for that year.
CC00=concentration for =concentration for reference year (1700)reference year (1700)..
0
3ln
ln 2n
n
C tdT t
C
Climate-Response FunctionClimate-Response FunctionThere is a time lag for the atmospheric There is a time lag for the atmospheric
temperature after carbon emissions.temperature after carbon emissions.
Data errors are large.
Fit of two hyperbolic tangents to the data.
Due to energy absorbed and released later in mostly the oceans, but also in ice.
Climate-Response FunctionClimate-Response Function
The climate-sensitivity function is multiplied by a series of two hyperbolic tangents:
Temperature lag is due to energy absorbed and released later in mostly the oceans, but also in ice.
1 1
2773 0.6320.368 tanh 1 tanh ln
ln 2 10.5 2 524
nin i n i
ni i
C tt t t tdT t
C t
1.3 degrees C
Close to the current measured value.
Although the temperature is not extremely high, it hangs around for a long time.
Does not account for fluctuations due to global dimming.
Temperature & CO2 are mutually reinforcing (positive feedback).
8°C
Disaster region!Peak in this
calculation.
Ice age to current interglacial is about 8 degrees C in Antarctica and about half that in the temperate
regions.
Why such a high projection?!
Assume carbon sequestration or a coal-burning moratorium.
Probably optimistic!
1 20501 tanh
2 25
tf
Assume carbon sequestration or a coal-burning moratorium.
Coal
CO2 is somewhat reduced by carbon sequestration
or a coal-burning moratorium.
430 ppmv; reduced from 465
Temperature is somewhat reduced by carbon sequestration
or a coal-burning moratorium.
1.1 degrees C; reduced from 1.3
Will we have waited too late?!
Double the coal extracted.
Coal
CO2 concentration due to doubled coal extraction
490 ppmv
Temperature is increased due to doubled coal extraction.
1.65 degrees CInstead of 1.3
Temperatures for some of the cases considered
Coal Moratorium or Carbon Sequestration
Double Coal
Assumes that there is no triggering of Earth states.
changes with increasing concentration from changes with increasing concentration from 0.47 to 0.94 (land and ocean become 0.47 to 0.94 (land and ocean become saturated with COsaturated with CO22).).
Suppose permafrosted tundra release of Suppose permafrosted tundra release of carbon during the next century (example of carbon during the next century (example of temperature feedback).temperature feedback).
Suppose climate sensitivity changes from 3 Suppose climate sensitivity changes from 3 to 4 over the next two centuries. (It is known to 4 over the next two centuries. (It is known that it changes to 6 over millennia because that it changes to 6 over millennia because of slow feedbacks.)of slow feedbacks.)
Suppose concentration/emissions factor changes Suppose concentration/emissions factor changes with concentration from 0.47 to 0.94 (doubled).with concentration from 0.47 to 0.94 (doubled).
Due to land and oceans being saturated with carbon dioxide.
820 ppmvAssumes hyperbolic-tangent change with 450 ppmv break
point and 50 ppmv width.Disaster Region!
Suppose emissions/concentration Factor changes Suppose emissions/concentration Factor changes with concentration from 0.47 to 0.94 (doubled).with concentration from 0.47 to 0.94 (doubled).
Dangerously high temperatures
2.7 degrees C
Assume permafrosted tundra release of carbon.
Total 400 gigatonnes
Example of temperature feedback; there are other temperature feedbacks.
CO2 concentration due to permafrosted tundra release of carbon
Total CO2 concentration including permafrosted tundra release of carbon
Disaster Region!
555 ppmv
Temperature including permafrosted tundra release of carbon.
Disaster Region!1.8 degrees C
Worst case CO2 concentration
Most likely fossil-fuels depletion, CO2 feedback & carbon release
in Arctic
1110 ppmv !Calamitous!
Worst case temperatureWill cause terrible catastrophes for human life. (See Six Degrees: Our Future on a Hotter Planet by Mark Lynas.)
4.5 degrees Cfor climate sensitivity
change to 4
3.5 degrees C for climate
sensitivity = 3
Approximately the same temperature change between the last glacial maximum and now!
concentration from going extremely high, concentration from going extremely high, unless it triggers other effectsunless it triggers other effects..
Since temperature rise of about 0.8°C from Since temperature rise of about 0.8°C from 1818thth century is already causing disastrous century is already causing disastrous events, the continuing increase of another events, the continuing increase of another 1°C or more will cause even more disasters 1°C or more will cause even more disasters and may other Earth changes that will cause and may other Earth changes that will cause a higher temperature.a higher temperature.
The peaking of fossil fuels may be as large The peaking of fossil fuels may be as large immediate disaster as is global warming.immediate disaster as is global warming.
World Population ProjectionsWorld Population Projections
Fit of population to available fossil-fuels energy 1950-2006.Fit of population to available fossil-fuels energy 1950-2006.
Population without renewable energy
Population with renewable energy
Next Major Ice Age with Global Warming EffectNext Major Ice Age with Global Warming Effect
Accounting for claim that Earth average temperature changes are about half Antarctica average temperature changes.
This lecture is on the Internet, along with other This lecture is on the Internet, along with other related lectures:related lectures:
http://www.roperld.com/science/http://www.roperld.com/science/energyGWNMIA.ppt (Energy, Global energyGWNMIA.ppt (Energy, Global Warming and the Next Major Ice Age)Warming and the Next Major Ice Age)