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ERMUSR MISC MEMO 02-12-2008
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ERMUSR MISC MEMO 02-12-2008
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Environmental Effects of Increased Atmospheric Carbon Dioxide <br />ARTHUR B. ROBINSON, NOAH E. ROBINSON, AND WILLIE SOON <br />Oregon Institute of Science and Medicine, 2251 Dick George Road, Cave Junction, Oregon 97523 [arty@oism.org] <br />ABSTRACT A review of the research literature concerning the <br />environmental consequences of increased levels of atmospheric <br />carbon dioxide leads to the conclusion that increases during the <br />20th and early 21st centuries have produced no deleterious ef- <br />fects upon Earth's weather and climate. Increased carbon diox- <br />ide has, however, markedly increased plant growth. Predictions <br />of harmful climatic effects due to future increases in hydrocar- <br />bon use and minor greenhouse gases like C02 do not conform to <br />current experimental knowledge. The environmental effects of <br />rapid expansion of the nuclear and hydrocarbon energy indus- <br />tries are discussed. <br />SUMMARY <br />Political leaders gathered in Kyoto, Japan, in December 1997 to <br />consider a world treaty restricting human production of "greenhouse <br />gases," chiefly carbon dioxide (COZ). They feared that COZ would <br />result in "human-caused global warming" -hypothetical severe in- <br />creases in Earth's temperatures, with disastrous environmental con- <br />sequences. During the past 10 years, many political efforts have been <br />made to force worldwide agreement to the Kyoto treaty. <br />When we reviewed this subject in 1998 (1,2), existing satellite re- <br />cords were short and were centered on a period of changing interme- <br />diate temperature trends. Additional experimental data have now <br />been obtained, so better answers to the questions raised by the hy- <br />pothesis of "human-caused global warming" are now available. <br />;~ 25 <br />0 <br />y <br />-0°. <br />E <br />F <br />U <br />t <br />0 <br />Little Ice Age <br />24 <br />23 <br />22 <br />3,000-Year Average <br />21 <br />-1000 -500 0 300 1000 1500 2000 <br />Year <br />Figure 1: Surface temperatures in the Sargasso Sea, a 2 million square mile <br />region of the Atlantic Ocean, with time resolution of 50 to 100 years and <br />ending in 1975, as determined by isotope ratios of marine organism remains <br />in sediment at the bottom of the sea (3). The horizontal line is the average <br />temperature for this 3,000-yeaz period. The Little Ice Age and Medieval Cli- <br />mate Optimum were naturally occurring, extended intervals of climate de- <br />partures from the mean. A value of 0.25 °C, which is the change in Sazgasso <br />Sea temperature between 1975 and 2006, has been added to the 1975 data in <br />order to provide a 2006 temperature value. <br />The average temperature of the Earth has varied within a range of <br />about 3°C during the past 3,000 years. It is currently increasing as the <br />Earth recovers from a period that is known as the Little Ice Age, as <br />shown in Figure 1. George Washington and his army were at Valley <br />Forge during the coldest era in 1,500 years, but even then the temper- <br />ature was only about 1 ° Centigrade below the 3,000-year average. <br />The most recent part of this warnvng period is reflected by short- <br />Medieval Climate Optimum <br />2006 <br />0 <br />aR <br />E <br />ao <br />0 <br />a <br />V <br />'~ <br />a <br />E <br />L <br />z <br />_2e Betore Hydrocarbon ~ Daring <br /> Use Increase Increase <br /> <br />-16 E- ~ --~ <br />Glacier Shortening ; ~ <br />a <br /> <br />-l2 Occurs Before ~ tio <br />~ <br />o <br />o <br /> ~~ <br />and Is Unaffected by ~ Go <br /> Hydrocarbon Use , <br />~40 oa ~.~' <br />~ , <br />o~~~oa ~ ~~eq`c~o <br />~ <br /> r <br />' g <br /> <br />-a <br />`~~y~qc ~ <br />Gas <br />i <br />6 <br /> 4 <br />G~ ~~ ~ Oil <br />4 <br />0 <br /> Coal 2 <br />4 <br />1 rw 1 ~7e IaW 1a39 IYW 19311 2UOB <br />Year <br />a <br />cn <br />0 <br />a <br />U <br />0 <br />F <br />Figure 2: Average length of 169 glaciers from 1700 to 2000 (4). The princi- <br />pal source of melt energy is solaz radiation. Variations in glacier mass and <br />length are primarily due to temperature and precipitation (5,6). This melting <br />trend lags the temperature increase by about 20 years, so it predates the <br />6-fold increase in hydrocarbon use (7) even more than shown in the figure. <br />Hydrocazbon use could not have caused this shortening trend. <br />ening of world glaciers, as shown in Figure 2. Glaciers regularly <br />lengthen and shorten in delayed correlation with cooling and warm- <br />ing trends. Shortening lags temperature by about 20 years, so the cur- <br />rent warming trend began in about 1800. <br />Atmospheric temperature is regulated by the sun, which fluctuates <br />in activity as shown in Figure 3; by the greenhouse effect, largely <br />caused by atmospheric water vapor (H20); and by other phenomena <br />that are more poorly understood. While major greenhouse gas HZO <br />substantially warms the Earth, minor greenhouse gases such as COZ <br />U 2 <br />C <br />~° <br />a i <br />.~ <br />O <br />'o <br />d <br />a <br />E <br />F -t <br />Q <br />-2 <br />d <br />I <br />Solar Activity <br />1 <br />1 <br />~ Arctic Air 1 <br />Temperature <br />Temperature Correlates with 8 <br />Sun, Not Hydrocarbon Use Gas <br />6 <br />Oil q <br />World Hydrocarbon Use <br />\~ Coal 2 <br />---- --- 0 <br />1at•Y IYYO 1Y[e IYgU 1YOU IYaU 2011® <br />Year <br />374 <br />E <br />3 <br />372 ~ <br />u <br />c <br />w <br />'v <br />370 <br />as <br />368 <br />c <br />o <br />e~ <br />F '~ <br />~~ <br />~~ <br />w <br />U <br />Figure 3: Arctic surface air temperature compared with total solaz irradiance <br />as measured by sunspot cycle amplitude, sunspot cycle length, solar equato- <br />rial rotation rate, fiaction of penumbral spots, and decay rate of the 11-yeaz <br />sunspot cycle (8,9). Solaz irradiance correlates well with Arctic temperature, <br />while hydrocazbon use (7) does not correlate. <br />.journal ofAmerican Physicians and Surgeons (2007) 12, 79-90. <br />
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