Hot Times Or Hot Air: The Sun in the Science of Global Warming

Hot Times Or Hot Air: The Sun in the Science of Global Warming

August 07, 1998

PREFACE

The global warming scare assumes that human emissions of carbon dioxide and other greenhouse gases are the dominant driving force in recent and probable future climate changes. Yet as Dr. Sallie Baliunas points out in the lecture published below, surface temperature records indicate that the world has warmed only about 0.5 degrees centigrade during the last 100 years – roughly half the amount "predicted" by the computer models on which warming scenarios are based. Moreover, at least half the warming observed during the 20th century occurred before 1940, while most of the increase in greenhouse gas concentrations occurred after 1940. That suggests that of the observed warming, mankind is responsible for only one or two tenths of a degree. It further suggests that any future temperature increases due to industrial activity during the next century are likely to be modest.

But if mankind is responsible for no more than half the warming of the past century, what accounts for the remainder? One distinct possibility is the sun. As Dr. Baliunas explains, there is a close correlation between changes in solar magnetism, changes in solar brightness, and changes in global temperature. In periods when solar magnetism is at maximum strength, the world tends to experience global warming, as in the Medieval Warming of the 10th and 11th centuries. In periods when solar magnetism falls to minimum levels, the world tends to experience global cooling, as in the Little Ice Age of the 17th and 18th centuries.

Changes in solar brightness may not be the only means by which the sun affects global climate. As Dr. Baliunas notes, British scientists have suggested that shifts in the sun’s ultraviolet light affect the earth’s ozone layer and, in turn, the dynamics of climate. In addition, Danish astronomers have proposed that increases in solar magnetism may contribute to global warming by diminishing cloud cover. According to this theory, a stronger solar magnetic wind blocks cosmic rays that would otherwise penetrate earth’s atmosphere and provide nuclei for cloud formation.

But what if, despite the best evidence from temperature records and other scientific research, a major global warming is about to occur? Dr. Baliunas argues that a true "no regrets" policy would be a period of intense research combined with a moratorium on mandatory emission reductions. The "penalty" for waiting up to thirty years before mandating controls on greenhouse gas emissions would be an extra few tenths of a degree warming by the year 2100. Spread over a century, that small temperature increase would be negligible against the background of natural fluctuations. The benefits of delay would be considerable. Science would

gain a better understanding of climate change – its mechanisms, impacts, and risks. Nations would gain greater wealth and technological prowess, allowing them to mitigate and/or adapt to climate change more affordably than would be possible today.

 

Marlo Lewis, Jr. Vice President for Policy & Coalitions

 

 

HOT TIMES OR HOT AIR: THE SUN IN THE SCIENCE OF GLOBAL WARMING

SALLIE BALIUNAS, PH.D. As presented at the Cooler Heads Global Warming Lecture

Rayburn House Office Building August 7, 1998

 

 

The extent of human effects on global climate change remains a highly complex scientific matter, as the United Nations Intergovernmental Panel on Climate Change (IPCC) made clear in its last report:

Our ability to quantify the human influence on global climate is limited because the expected signal is still emerging from the noise of natural variability [NB: The signal has not yet been detected], and because there are uncertainties in key factors [NB: like natural factors]. (IPCC 1995, p. 5)

Given the complexities of climate, how can forecasts of climate change from increased greenhouse gases 100 years into the future be checked? One starts by noting that the increase in the different greenhouse gases in the atmosphere due to human activities over the last 100 years is effectively equal to roughly a 50 percent increase in the atmospheric concentration of carbon dioxide alone. That 50 percent effective increase in carbon dioxide concentration gives a way to test the accuracy of the computer forecasts of climate change simply by measuring the response of the climate to the increase in greenhouse gases that has already occurred.

1. Tests of climate projection scenarios against measurements

For example, all the IPCC 1995 scenarios make specific forecasts for warming that should have already occurred, including:

(i) Global warming of as much as 1 degree C;

(ii) Extremely large and rapid warming in the North Polar Region.

Both forecasts will be discussed.

(i) Global temperature records -- According to thermometer records collected near the surface, over land and sea, in the last 100 years as well as temperature estimates from proxy records, the temperature averaged from different parts of the world rose about 0.5 C since the late 19th century. Although global warming has occurred, its cause is an issue of scientific study.

Figure 1 -- Land and sea surface temperatures sampled world wide, compiled and analyzed by the United Kingdom Meteorological Office (for details of analysis, see D. E. Parker et al., 1995, Climatic Change, 31, 559, for marine records and P. D. Jones, 1994, Journal of Climate, 7, 1794. Updates kindly provided by UKMO.

As noted above, the 100-year instrument record is important because it covers the period in which there has been an effective 50% increase in carbon dioxide. The computer scenarios say that there should already be a warming as much as 1° C in the globally averaged temperature as a result of increased greenhouse gases in the atmosphere. At first glance it seems that the observed warming occurred due to the increases in the minor greenhouse gases in the last 100 years and is good evidence for the validity of projections of global warming from human activities.

That conclusion is insupportable for several reasons. First, at least half of the warming seen in the surface temperature record occurred before about 1940, while most of the greenhouse gas increase in the atmosphere occurred after 1940. That means that most of the temperature rise of the last 100 years occurred before the substantial increases in greenhouse gases in the atmosphere from human activities. Of the 0.5 C rise observed, at most only one or two tenths of a degree can be attributed to increased greenhouse gases.

A second problem is the uncertainty of the urban-heat-island effect in the temperature records: temperature measurements made in growing, modern cities can read excess warmth due to the effects of machinery, pavement, tree-cutting, etc. A correction, as best as possible, can been made, but the process can introduce a systematic error to the average record.

Another uncertainty comes from uneven coverage in the surface records. Good records with near-continual coverage for the last 100 years apply to only 18% of the surface. Better coverage exists today of the surface; still, the Polar Regions as well as vast areas of the southern and tropical oceans are not adequately sampled.

Beginning in 1978 NASA satellites were launched and their measurements have yielded a record of nearly globally averaged temperature. Measurements are made of the lower troposphere and were discussed in a series of lectures by Dr. John Christy. The forecasts claim the increase in atmospheric greenhouse gases is now so large that the global temperature should be rising about 0.2 C per decade. But the satellite readings (validated by independent balloon experiments) show that the temperature has not changed at all in the last 19 years in response to the increased greenhouse gases.

Figure 2 -- Annually averaged global temperatures of the lower troposphere measured by satellite (Christy and Spencer; see Note 5).

An uncertainty of all instrumental records is their shortness, which limits our ability to compare the warming of the early 20th century to natural fluctuations of the climate during other periods. No worldwide instrumental records go back further than the mid-19th century, but there are records or reconstructions of several regions going back further. For example, the natural variability of temperature in the mid-latitude Atlantic Ocean over the last 3000 years has been reconstructed from ocean-bottom sediments.

Figure 3 -- Reconstructed temperatures of the Sargasso Sea (Keigwin 1996). The horizontal line marks the level of the current, instrumental temperature.

The longer perspective, hidden by the bias of the shortness of the instrumental records, shows substantial natural variability of temperature. Evident are periods like the Little Ice Age, reaching its coldest during the 17th and 18th centuries, and the Medieval Climate Optimum, a warming in the 10th - 11th centuries. That record does not stretch as far back as the Holocene Optimum, 6500 years ago, the warmest interval of the last 10,000 years after the end of the last major ice age. The record of natural variability indicates that the warming of the early 20th century is not unusual, either in amplitude or speed.

Neither the surface records nor the lower tropospheric temperature records show the substantial increasing warming trends expected from increased greenhouse gases, in contradiction to the projections from the computer scenarios.

(ii)Temperature Records of the Arctic -- According to the computer forecasts, the polar areas are very sensitive to global warming. The forecasts say that the Arctic region should have warmed by as much as 2 - 4 degrees C in the last 50 years in response to increased greenhouse gases in the atmosphere. Instrumental measurements contradict the intense warming trend for that region projected by the computer scenarios. On the average over the last 40 years, the temperature record does not show and increasing warming trend. A longer-term view of the lower Arctic comes from proxy records like tree-ring growth. In that record there is rapid warming in the early 20th century, but it began before 1920, and again, must be largely unrelated to increased greenhouse gases. Since 1950, that record suggests that the Arctic has cooled despite the increases in greenhouse gases.

Figure 4 -- Reconstructed temperatures (highly weighted by summer temperature) of the near-Arctic region (Overpeck et al. 1997).

In the test of the Arctic temperature record, the computer forecasts exaggerate the expected warming, this time, by more than ten-fold.

Looking at the temperature information, one concludes two things: (1) the climate scenarios exaggerate the warming that should have already occurred (and likely also the future warming) as a result of increased greenhouse gases; and (2) most of the warming this century cannot have been caused by increased greenhouse gases, because the warming predates the greatest increases in such gases.

2. What’s wrong with the computer forecasts?

The calculation of the response of the climate system to the energy input from increases in greenhouse gases is difficult because the climate system is a complex nonlinear system that is not well understood.

Incomplete physics, insufficient computing power -- The most sophisticated of the computer simulations track five million parameters. Understanding of the physics of some of the processes (e.g., upper tropospheric water vapor) is incomplete; the measured values of some parameters are poor. The computer scenarios presently do not but need to span 16 orders of magnitude in spatial scale and to include ten million trillion degrees of freedom.

Margins of error larger than the effects to be measured -- The computer programs calculate the effect of adding a small amount of energy, 4 W m-2, to a simulated climate. That amount roughly corresponds to a doubling of the atmospheric concentration of carbon dioxide. But the uncertainty in calculating, e.g., the effects of humidity, clouds and the flow of energy from the equatorial to the polar regions may be each at least five times larger. Such errors can give rise to area-by-area "flux adjustments" of up to 25 times larger in some regions of several coupled ocean-atmosphere simulations. When the unknowns in the climate simulations are more than an order of magnitude larger, it seems difficult to accept the calculated response of the climate to the small, added energy expected from doubling carbon dioxide.

Water vapor -- Compared to the temperature records, the computer projections exaggerate the warming that should have appeared. Why? The scenarios assume that the small warming from increases in the minor greenhouse gases like carbon dioxide is amplified by water vapor in the upper atmosphere. That is, water vapor is assumed to provide a strong, positive feedback for any minor warming. This assumption has been challenged by both developments in convection theory and new measurements. When the gain in temperature due to water vapor feedback is removed, doubling carbon dioxide yields roughly only 1° degree C warming or less, which is more consistent with the observed trends in the surface temperature records.

  1. Natural factors of climate change: the sun

Another reason for exaggerated forecasts may rest in incomplete knowledge of natural variations, as the IPCC suggests. One such natural factor may be changes in the brightness of the sun over decades and centuries. The magnetism on the sun’s surface varies roughly every 11 years.

 

Figure 5 -- Record of Sunspot Number.

According to recent findings based on measurements from NASA satellites, the sun brightens and fades in its total energy output, in step with the 11-year cycle of magnetism. Not only the sun’s brightness, but also its flux of high-energy particles that bombard the earth, changes with the surface magnetism of the sun. The observed association of brightness change with magnetic change over nearly two decades is the basis for thinking that changes in the sun’s brightness occur over many decades, along with recorded changes in magnetism. If significant, brightness changes over decades could drive non-trivial global temperature change.

The climate record indicates a solar influence of this kind. An example is the record of the sun’s magnetism and reconstructed land temperatures of the Northern Hemisphere over 240 years. The two curves are highly correlated over several centuries. Those changes in the sun’s magnetism may track changes in the sun’s brightness, for which direct measurements are lacking.

Figure 6 -- Changes in the Sun’s magnetism (the length of the 22-year, or Hale magnetic polarity cycle, dotted line) and changes in Northern Hemisphere land temperatures (solid line). Shorter magnetic cycles are more intense which suggests a brighter sun (Baliunas and Soon 1995).

Assuming that the timing of the sun’s magnetic changes is a proxy for the sun’s changing brightness, computer simulations of the earth’s climate suggest that changes of 0.4 percent in the sun’s brightness could have produced global average temperature changes of about 0.5 degrees C over the last 100 years.

Additional evidence points to the sun’s signature in the climate record over many millennia. Every few centuries the sun’s magnetism weakens to low levels sustained for several decades. An example is the magnetic low circa 1640 - 1720, when sunspots were rare and the sun’s magnetic field weak. That period coincided with a climate cooling called the Little Ice Age, when the global temperature is estimated to have been roughly 1° degree C colder than today.

Quantitative records of the sun’s magnetism over millennia come from measurements of the isotopes radiocarbon (14C, in tree rings) and Beryllium (10Be, in ice cores). The reason that the isotope records yield information on the sun’s magnetism is as follows. Cosmic rays, energetic particles from the debris of nearby supernova explosions tens of millions of years ago, interact with the magnetic fields of the sun and earth and the earth's atmosphere and ultimately can form 14C and 10Be. The amounts of 14C and 10Be formed in the earth's atmosphere by this process are modulated by changes in the sun’s magnetism. Once formed, 14C in a carbon dioxide molecule may be incorporated in a tree ring through photosynthesis; 10Be may precipitate into an ice layer accumulating in the ice sheets at high latitudes.

The isotope records confirm the occurrence of the sun’s low magnetism in the 17th century, seen in the early telescopic records of sunspots, and reveal similar periods of low magnetism every few centuries, plus occasional, sustained magnetic maxima (circa 10th-11th centuries). During the periods of weak magnetism, the sun should be dimmer compared to the average; periods of high magnetism should mean a brighter sun. Those estimated brightness changes may seem relatively small -- a few tenths per cent for the large swings in magnetism -- but they are large enough, according to some climate scenarios, to explain changes in global temperatures of as much as ~1-2 degrees C.

The influence of the sun on the climate can be inferred from tree ring records 5000 years long. They show that 6 out of 7 long-term lows in the sun’s magnetism correspond to cold spells. Records from Scandinavia covering 10,000 years show that 17 out of 19 coolings line up with lows in the sun’s magnetism.

Similar results are obtained from observations of solar surface magnetism and brightness changes in sun-like stars: changes in the sun’s brightness over decades may be as large as several tenths per cent.

The idea that the total energy output of the sun changes is one of the simplest mechanisms for the sun’s possible effect on climate change. But the fact is that the sun’s output comes in many wavelengths; it also emits energetic particles, and both are variable in time, space and frequency. British scientists have suggested that the sun’s changing ultraviolet light affects the ozone layer in the earth’s stratosphere, and in turn the dynamics of the climate. Danish astronomers have additionally proposed that the galaxy’s cosmic rays, modulated by the sun’s changing magnetism, alter the cloud cover and, hence, climate of the earth. The different components of the earth’s atmosphere and surface respond to different aspects of the sun’s diverse energy outflows, in ways that are yet unknown. Understanding of the possible effects of the changing sun on climate change is still evolving. Further research should improve computer scenario modeling of natural variations in climate, which form the background against which human effects must be quantitatively assessed.

Comments

The best scientific evidence says that global warming as a result of increasing greenhouse gases in the atmosphere would be slow and insignificant compared to the natural changes of the climate, which are subjects of intense research. But what if that conclusion is wrong? Despite the best interpretation of the temperature records, what if a major global warming is occurring or about to occur, but its signal cannot be detected?

From the best science and economics emerges an opportunity for a "no regrets" policy of intense research while deep emission cuts are delayed. Consider first that the penalty paid in the increase of projected temperature in the next century by delaying severe reductions of greenhouse gas emissions is small. For example, assume the IPCC’s current estimate: that global warming will cause a temperature rise of roughly 2 degrees C by the year 2100. In that case, the extra temperature rise from delaying action up to thirty years on policies to limit greenhouse gas emissions is a few tenths of a degree C. The penalty of an extra few tenths of a degree, spread over a century, will be entirely negligible against the backdrop of natural fluctuations.

Consider further that the projected warming -- judged by the temperature records -- is likely exaggerated. Should severe emission cuts be delayed, two major benefits may result: first, with further research a better understanding of climate change should emerge and lead to an improved estimate of the timing and magnitude of any problems. Second, mitigation and adaptation should become more affordable as technology advances. Together those considerations suggest a slow emergence of any global human effect and an opportunity to take the time to insure the best response to the possibility of human-caused climate change.

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* The opinions expressed are solely those of the author and do not necessarily represent views of any of the institutions with which the author is affiliated. 1Climate Change 1995: The Science of Climate Change, Contribution of Working Group to the Second Assessment Report of the Intergovernmental Panel on Climate Change, 1996, eds. J. T. Houghton et al., Cambridge University Press, 572pp. 2See R. C. Balling, Jr., 1994, The Heated Debate, (San Francisco: Pacific Research Institute) 195pp. See also comments by D. Hoyt at http://www.erols.com/dhoyt1. 3S. M. Robeson, 1995, Climatic Change, 29, 213. 4P.J. Michaels, R. C. Balling, Jr., R. S. Vose and P. C. Knappenberger, 1998, Climate Research 10, 27. 5J. R. Christy, 1995, Climatic Change, 31, 455; data available from http://wwwghrc.nsfc.nasa.gov/ims-cgi-bin/mkdata?mwu2rm190+/pub/data/msu/.... See also http://science.nasa.gov/newhome/headlines/notebook/essd99aug98_1.htm for a discussion of recent corrections to the satellite temperature record, which, when properly made, results in no statistically significant increasing warming trend. 6L. Keigwin 1996, Science, 274, 1504. See also D. Dahl-Jensen et al., 1998 Science, 282, 268, for reconstructed temperatures for Greenland over the last 1,000 years. 7J. Overpeck et al. 1997, Science, 278, 1251. 8J. L. Lions et al., 1997, Journal of Atmospheric Science, 43, 1137. 9"...[W]ithout knowing the dynamical heat fluxes, it is clear...that one cannot even calculate the mean temperature of the earth." (R. S. Lindzen 1997, Proceedings. National Academy of Science, USA, 94, 8335); K.Y. Kondratyev, 1997, Bulletin of the American Meterological Society, 78, 689. 10"...[We] conclude that ... the GCM considered cannot be used for any physical experiment devoted to studying real climate change, such as greenhouse warming..." (I. Polyak and G. North, 1997, Journal. Geophysical Research, 102, 1921). "...[I]t [is] clear that using the GCM for investigation of the real climate variability...has no scientific justification." (I. Polyak and G. North, 1997, Journal. Geophysical Research, 102, 6799). "...[I]t is hard to say...that an anthropogenic climate signal has or has not been detected," (T. P. Barnett, B. D. Santer, P. D. Jones, R. S. Bradley and K. R. Briffa, 1996, Holocene, 6, 255). 11D.-Z. Sun and R. S. Lindzen, 1993, Journal of Atmospheric Sciences, 50, 1643; R. W. Spencer and W. D. Braswell, 1997, Bulletin of the American Meteorological Society, 78, 1097. 12R. S. Lindzen, 1993, Annual Reviews of Fluid Mechanics, 26, 353; R.S. Lindzen, 1996, Climate Sensitivity to Radiative Perturbations: Physical Mechanisms and Their Variation, ed. H. le Trent NATO ASI Series, Vol. I 34, Berlin: (Springer-Verlag) 51. 13Over the 11-year cycle, the full range of brightness change is at most 0.14%. Such changes seem insufficient in amplitude and time scale to cause a temperature response of the climate system that is larger than 0.1 C over the period of observations. 14Northern Hemisphere land temperatures (from B. S. Groveman and H. E. Landsberg 1979, Geophysical Research Letters, 6, 767; P. D. Jones et al. 1986, Journal of Climate and Applied Meteorology, 25, 161) are shown because the global surface records do not reach back so far (S. Baliunas and W. H. Soon, 1995, Astrophysical Journal, 450, 896); first discovered by E. Friis-Christensen and K. Lassen 1991, Science, 254, 698; K. Lassen and E. Friis-Christensen, 1995, Journal of Atmospheric and Terrestrial Physics, 57, 835). 15In other words, assuming that one knows the mechanism of solar change (i.e., total brightness), and the response of the climate to such change. Neither is known! Some wavelengths of sunlight may be more important than others in affecting the climate. For example, the solar ultraviolet irradiance may make changes in the chemistry in the stratosphere and troposphere (J. D. Haigh, 1996, Science, 272, 981); visible-wavelength irradiance changes may affect the lower atmosphere and sea surface (W. B. White, J. Lean, D. R. Cayan and M. D. Dettinger, 1997, Journal of Geophysical Research, 102, 3255). Both portions of the solar irradiance spectrum may combine to influence the dynamics of planetary-scale waves and Hadley circulation. In addition, brightness changes have been considered here independent of wavelength. Then, too, the sun’s surface magnetism and wind modulate the amount of galactic cosmic rays striking the earth's atmosphere and magnetosphere, and so the electrical (B. A. Tinsley, 1997, Eos, 78, No. 33, 341) and chemical (J. W. Chamberlain, 1977, Journal of Atmospheric Science, 34, 737) properties of the upper atmosphere. In turn, cloud microphysics and cloud coverage may change (H. Svensmark & E. Friis-Christensen 1997, Journal of Atmospheric & Terrestrial Physics, 59, 1225). 16Further details can be found in W. H. Soon et al. 1996, Astrophysical Journal,472, 891 and references therein. 17A recent analysis (R. Willson, 1997, Science, 277, 1963) finds a baseline change of irradiance between the solar minima in 1986 and 1996. Over a century, that base change would be about 0.4 percent. 18T. M. L. Wigley and P. M. Kelly, 1990, Phil. Trans. Roy. Soc. London, A, 330, 547; W. Karlen and J. Kuylenstierna, 1996, Holocene, 6, 359. 19S. L. Baliunas and W. H. Soon, note 15; Q. Zhang et al. 1994, Astrophysical Journal (Letters), 427, L111. 20J. Haigh et al, note 15. 21H. Stevens mark and E. Friis-Christensen, note 15. 22See also T. M. L. Wigley et al. 1996, Nature, 379, 240; T.M.L. Wigley, 1997, Nature, 390, 267-270; M. Parry et al. 1998, Nature, 395, 74.