a clear indication of corresponding changes ingalactic cosmic rays (GCR), which are modulatedby variations in solar activity. The oxygen-18values are proxies for a climate parameter, liketemperature or precipitation, from a shift in <strong>the</strong>Intertropical Convergence Zone (ITCZ). Thecorrelation extends well over 3,000 years, withamazingly detailed correspondence. The bottomgraph shows <strong>the</strong> central 400 years expanded and isaccurate on almost a yearly basis, making acause-effect relationship very likely.The best explanation for <strong>the</strong>se observations, andsimilar ones elsewhere, is that – as has long beenrecognized [Singer 1958] – GCR intensity ismodulated by <strong>the</strong> strength of <strong>the</strong> solar wind and itsmagnetic field. More recently, a detailed mechanismwhereby cosmic rays can affect cloudiness and<strong>the</strong>refore climate has been suggested and verifiedexperimentally by Henrik Svensmark [2007a,b].More detailed work is to take place under <strong>the</strong>CLOUD project proposed by a group of scientists atCERN, <strong>the</strong> world’s largest particle accelerator.Solar <strong>Activity</strong> and <strong>Climate</strong> (as seen by proxies)12Figure 14: Values of carbon-14 (produced by cosmic rays – hence a proxy for solar activity)correlate extremely well with oxygen-18 (climate proxy); data are from a stalagmite in Oman [Neff2001]. The time interval covers more than 3,000 years, from about 9,600 to 6,200 years beforepresent (BP). The lower graph shows a particularly well-resolved time interval from 8,350 to 7,900years BP. It would be difficult to explain this detailed correlation except through <strong>the</strong> modulation ofgalactic cosmic rays by changes in <strong>the</strong> solar wind and solar magnetic activity [Singer 1958]. Themechanism whereby cosmic rays influence terrestrial climate is most likely a change in cloudiness,as suggested by Svensmark [2007a, 2007b].
Lockwood and Fröhlich [2007] have claimed adivergence between TSI and temperature in <strong>the</strong> past20 years; but this claim is disputed by both solar andclimate experts. For example, evidence for climateeffects of TSI in more recent times is presented byScafetta and West [2007], and of solar activity byUsoskin and Kovaltsov [2007]. Shaviv [2002, 2005]has demonstrated <strong>the</strong> climate effects of fluxvariations of Galactic Cosmic Rays on <strong>the</strong>hundred-million-year time scale. See also Shavivand Veizer [2003].There now is little doubt that solar-windvariability is a primary cause of climate change ona decadal time scale. Once <strong>the</strong> IPCC comes to termswith this finding, it will have to concede that solarvariability provides a better explanation for 20thCentury warming than GH effects. Indeed, solarvariability may explain <strong>the</strong> pre-1940 warming andsubsequent cooling period, <strong>the</strong> MWP and LIA – ando<strong>the</strong>r quasi-periodic climate oscillation with aperiod of roughly 1,500 years, going back a millionyears or more [Singer and Avery 2007].4. <strong>Climate</strong> Models Are <strong>Not</strong> ReliableIn its 2001 report <strong>the</strong> IPCC admitted, “In climateresearch and modelling, we should recognise thatwe are dealing with a coupled non-linear chaoticsystem, and <strong>the</strong>refore that <strong>the</strong> long-term predictionof future climate states is not possible” [IPCC-TAR2001, p. 774] Fur<strong>the</strong>r, as demonstrated in Section 3,<strong>the</strong> Earth’s climate system is subject to significant,changing influences beyond <strong>the</strong> Earth itself that arenot well understood and cannot be controlled.Computer models undoubtedly have <strong>the</strong>ir placeas a way of projecting possible consequences whenone or more variables are changed. However,models do not represent reality, yet <strong>the</strong> IPCCpersists in treating <strong>the</strong>m as if <strong>the</strong>y do. The IPCC andits predecessors have adopted climate sensitivities(for a doubling of CO 2 ) of 1.5º to 4.5º C. But actualmodel results exceed <strong>the</strong>se ‘canonical’ limits in bothminimum and maximum; some model results rangeup to 11º C.! Computer models do not consider solardimming and brightening.Current models do not consider <strong>the</strong> observedsolar ‘dimming’ and post-1985 ‘brightening’ [Wild2005b; Stanhill 2007]. Existing models do not takeaccount of <strong>the</strong> existence of water vapor (WV)‘dimers’ (double H 2 O molecules) [Paynter et al.2007] and <strong>the</strong>ir atmospheric absorption of incomingsolar radiation in <strong>the</strong> near-infrared, which may leadto a negative climate feedback as WV concentrationincreases in <strong>the</strong> lower troposphere.! Computer models do not accurately model<strong>the</strong> role of clouds.The differences among model results are largeand arise mostly from <strong>the</strong> treatment of clouds and<strong>the</strong> somewhat arbitrary choices of cloud-relatedparameters, notably, <strong>the</strong> droplet-size distribution[Senior and Mitchell 1993], which strongly affects<strong>the</strong> cloud albedo. Most of <strong>the</strong> effects of parametervariation are caused by a small subset of parameters;for example, <strong>the</strong> choice of entrainment coefficient inclouds is associated with 30 percent of <strong>the</strong> variationseen in climate sensitivity [Knight 2007].Special problems arise from <strong>the</strong> chaotic natureof climate. Small changes in initial conditions leadto vastly different outcomes. To overcome thiswell-recognized feature, modelers resort to multipleruns (‘simulations’), which are later averaged intoan ‘ensemble.’ The problem <strong>the</strong>n becomes one ofconvergence, especially when <strong>the</strong> outcomes differgreatly from each o<strong>the</strong>r [Lucarini et al. 2007]. Anadditional problem arises when trying to averageover different model ensembles, some based on asmany as 10 runs, some only on one run.As previously observed, current GH models donot match <strong>the</strong> observed latitude distribution oftemperature trends. In particular, one would expectthat <strong>the</strong> production of sulfate aerosols in <strong>the</strong>Nor<strong>the</strong>rn Hemisphere (NH) should create a reducedwarming trend <strong>the</strong>re – or even cooling. Theobservations show <strong>the</strong> opposite.In general, models do not consider realistically<strong>the</strong> lack of geographic homogeneity of forcing,especially for aerosols. Polar trends do not agreewith model expectations and can more easily beexplained with solar forcing [Soon 2005]. Modelsreviewed by <strong>the</strong> IPCC do not employ realisticgrowth figures for <strong>the</strong> GH gas methane[Dlugokencky 1998] and do not consider <strong>the</strong>resultant forcings caused by future changes in <strong>the</strong>stratosphere from increases in water vapor andozone depletion [Singer 1971; Shindell 2001].13
- Page 1 and 2: Nature, Not Human Activity,Rules th
- Page 3 and 4: ForewordIn his speech at the United
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- Page 39 and 40: About the ContributorsAnderson, War
- Page 41 and 42: ReferencesAnonymous 1994. IPCC’s
- Page 43 and 44: Keatinge W.R. et al, 2000. Heat rel
- Page 45 and 46: Rahmstorf, S., et al. 2007. Recent
- Page 47 and 48: AcronymsAGW Anthropogenic Global Wa
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