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CO2 Forcing: Fact or Fiction

Explore the correlation between CO2, CH4, and temperature through ice core data, atmospheric absorption analysis, and satellite observations, revealing the periodic influences and identifying cause and effect relationships. Is the CO2 forcing hypothesis factual or a fiction?

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CO2 Forcing: Fact or Fiction

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  1. Science provides the unambiguous answer George White October 2008 Revised July 2009 co2@palisad.com CO2 Forcing: Fact or Fiction

  2. The Ice Cores • > 400K year history from Vostok • > 800K year history from Dome C • The climate is far from constant • CO2, CH4 and Temperature are all correlated • The data tells us far more than this • What kind of changes are expected? • Which came first, the gas or the heat? • What are the periodic influences?

  3. Many sources of information • Ice Core Data • Atmospheric Absorption Data • Satellite Observations • Ground Based Observations • Biology • Physics

  4. Vostok Ice Core Temperatures

  5. Ice Core Temp + CO2

  6. Temp + CO2 + CH4

  7. Last 15K years Temp + CO2

  8. Dome C Ice Temp + CO2

  9. Data Smoothing • Data samples are intrinsically biased • Recent samples represent short term averages • Ancient samples represent long term averages • Different variables have different sample periods • Integrate samples over N years • Matches short term data to long term data • Matches temperature to CO2 and CH4 • Isolate long and short term periodicity • Isolate long and short term dependency

  10. Temp + CO2 1500 year smoothing

  11. Dome C Temp + CO2 with smoothing

  12. Last 15K years with smoothing

  13. Last 15K years Dome C

  14. Compare Vostok and Dome C

  15. Dome C 15K years + smoothing

  16. Correlation Analysis • Simple correlation metric for time Δt from t • Plus 1 when t+Δt changes in the same direction as t • Minus 1 when t+Δt changes in the opposite direction • Cross correlation identifies cause and effect • Auto correlation identifies periodic components • Use smoothing to select long or short term • Variable window to match Δt to sample period

  17. Cross Correlation Analysis • Can identify which of 2 variables changes first • Temperature and CO2 • Temperature and CH4 • CO2 and CH4 • Smoothing is required to normalize variability • Smoothing does not mask cause and effect • Smoothing makes short term dependence apparent

  18. Cross Correlate Temp and CO2

  19. Cross Correlate Temp and CH4

  20. Cross Correlate Temp, CO2 and CH4

  21. Dome C Cross Correlation • Dome C has finer resolution CO2 measurements • Shows apparent correlation of CO2 to future Temp • Frequently misinterpreted as a causal dependency • Also shows earlier correlation to opposite change • This is an aliasing effect which really indicates • CO2 increase -> Temp Decrease -> Temp Increase • Indicates correlation across a period of unrelated change • Indicates interference from a periodic effect • When smoothing is applied • Same results as Vostok data

  22. Dome C Correlate Temp and Co2

  23. Dome C Correlate with smoothing

  24. Dome C Temp, CO2 and CH4

  25. Auto Correlation Analysis • Auto correlate temperature • Apparent short term periodic behavior • 180 year Dome C, 120 Year (25yr bucket), 270 year Vostok • Seems to be aliasing of seasonal variability • Apply smoothing • Unambiguous 22K, 41K period (Vostok and Dome C) • Modulated peaks are evidence for other periodicity • Related to variability in Earth's orbit and axis • Related to sums and harmonics of this variability • Common to temperature, CO2 and CH4

  26. Short Term Auto Correlation

  27. Medium Term Auto Correlation

  28. Long Term Auto Correlation

  29. Longer Term Auto Correlation

  30. An Even Longer Term Effect

  31. Combined Effects • The change between 96K and 41K ice ages • Considered by some to be a mystery • When the 41K, 96K and 500K forcing are combined • One can cancel or enhance the other • 96K is weaker, 500K is weakest, 41K is dominant • The pattern is clearly an interference pattern • We are entering a new age of 41K ice ages • Evidenced by current weaker, but longer interglacial • Currently approaching 500K peak • 41K and 96K peaks are separated by about 30K years • Stretching out the current interglacial

  32. Is This Enough Forcing? • Some say that these effects are not strong enough • The periodicity clearly aligns • Magnitudes seem unexpected • 96K is weak, but appears dominant recently • Several 41K peaks have aligned with 96K minimums • This mitigates the magnitude of the 41K effects • There is a feedback effect at work • Hemispheric asymmetry and ice amplification

  33. Atmospheric Absorption • An objective review of atmospheric absorption is all that's required to disprove CO2 forcing • The atmospheric absorption spectrum is known • It has been measured and correlated to theory • Water vapor contributes about 2/3, CO2 is 1/3 • Relatively transparent window from 8μ to 14μ • Weak ozone absorption in the middle • 7.5μ CH4 line on one side, 15μ CO2 line on the other, water vapor continuum absorption throughout

  34. Atmospheric Absorption Spectrum

  35. CO2 Absorption • 15μ CO2 line absorption • Highly saturated • Energy limited, not concentration limited • Double CO2 • Insignificant increase in width • Primarily decreases mean distance before absorption • Other bands are between 2μ and 4.3μ • Narrower lines • Significant H2O overlap • Far less energy available to be absorbed

  36. GHG Forcing • The Energy Cycle • CO2 captures 15μ surface energy • Collisions transfer energy to other gas molecules • Some energy gets back to the surface • The cycle repeats • Delays the release of surface energy • GHG flux is a circulating flux • Solar flux is an incident flux

  37. Satellite Observations • 25 year history of detailed weather measurements • 10 km surface resolution • 3 hour time resolution • 100% surface coverage • Measurements include • Surface temperature • Cloud temperature • Cloud coverage • Reflectivities

  38. Anomaly Analysis

  39. Anomaly Fix

  40. Anomaly Partial Fix

  41. Observed Variability • Global mean temperature varies significantly • +/- 2.1˚C seasonal variability • +2.1˚C in June, -2.1˚C in December • Sun is closest in early January, farthest in July • Global mean temperature changes oppositely • Indicates dramatic hemispheric asymmetry • Unambiguously supports Milankovitch forcing • Data calibration error around 2001-2002 • This has been misinterpreted as 'evidence' of warming

  42. Global Average Temperature

  43. Hemispheric Differences • Southern Hemisphere • 8˚C peak to peak variability • 276˚K absolute mean temperature (=3˚C) • Northern Hemisphere • 24˚C peak to peak variability • 280˚K absolute mean temperature (=7˚C) • Equatorial • Small 6 month periodic variability • Clearly illustrates 2001/2002 calibration error

  44. Hemispheric Differences

  45. Surface Reflectivity • Northern Hemisphere • Higher mean • More land, less water • More variability • Greater range in albedo – whiteness of snow and ice • More time spent during higher reflectivity • More persistent snow and ice coverage • Consequences • Sun closer in Northern summer -> cooler climate • Sun closer in Southern summer -> warmer climate

  46. Reflectivity Asymmetries

  47. Temperature and Reflectivity

  48. Where is the Sun Now? • Sun is closest in early January • 3.4% more incident energy than average • Sun is farthest away in early July • 3.4% less incident solar energy than average • Nearly 7% total solar variability over a year • Corresponds to a 4˚C difference in temperature • Peak aphelion/perihelion differences are > 20%

  49. Temperature and Energy

  50. Implications of Sun-Earth distance? • When Sun is closest during North winter (now)‏ • Warmer seasons, ice shrinks • Ice shrinks, -> less reflected energy -> even warmer • Positive feedback stops once minimum ice is reached • When Sun is farther away during Northern winter • Colder seasons, ice grows • Ice grows -> more reflected energy -> even colder • Southern hemisphere climate is more stable • Equatorial climate is even more stable

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