<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">AJCC</journal-id><journal-title-group><journal-title>American Journal of Climate Change</journal-title></journal-title-group><issn pub-type="epub">2167-9495</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ajcc.2015.43014</article-id><article-id pub-id-type="publisher-id">AJCC-56384</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Earth&amp;Environmental Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  On the Relationship between Atmospheric Carbon Dioxide and Global Temperature
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>lexander</surname><given-names>Ruzmaikin</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Alexey</surname><given-names>Byalko</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Landau Institute of Theoretical Physics, Chernogolovka, Russia</addr-line></aff><aff id="aff1"><addr-line>Jet Propulsion Laboratory, California Institute of Technology, Pasadena, USA</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>Alexander.Ruzmaikin@jpl.nasa.gov(LR)</email>;<email>alex@byalko.ru(AB)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>18</day><month>05</month><year>2015</year></pub-date><volume>04</volume><issue>03</issue><fpage>181</fpage><lpage>186</lpage><history><date date-type="received"><day>10</day>	<month>January</month>	<year>2015</year></date><date date-type="rev-recd"><day>accepted</day>	<month>15</month>	<year>May</year>	</date><date date-type="accepted"><day>18</day>	<month>May</month>	<year>2015</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  The study of dynamic relationships between the atmospheric carbon dioxide and the Earth’s global temperature in the current changing climate supported the notion that the trend in the global temperature followed the trend in the atmospheric CO2 before the climate hiatus that started in the beginning of the 21st century. During the hiatus period, the heat trapped by the atmospheric CO2 is going mostly to the ocean. This conclusion is supported by comparison of the CO2 trend with the trend in the ocean heat content. The phase relationships between the CO2 and temperature are more complicated after the removal of the trends. The phase relationships are chaotic on time scales shorter than the annual time scale. During 1986-2008, the atmospheric CO2 changed in an-ti-phase with the global temperature. The phase relationship reversed in 1979 and after 2010. The atmospheric CO2 was in-phase with the global temperature on the El Nino time scale (2.3 - 7 years) except during very strong El Nino years in 1991-1999 when CO2 led the global temperature.
 
</p></abstract><kwd-group><kwd>Atmospheric Carbon Dioxide</kwd><kwd> Earth’s Global Temperature</kwd><kwd> Phase Relationships</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Carbon dioxide (CO<sub>2</sub>) is the major greenhouse gas that absorbs and re-emits the outgoing long wave radiation causing an increase of the Earth’s heat content. The change in the Earth’s surface global temperature T is commonly considered to be driven by the increase of CO<sub>2</sub>. However, the situation is more complicated because the atmospheric concentration of CO<sub>2</sub> does not follow the rate of its industrial emissions [<xref ref-type="bibr" rid="scirp.56384-ref1">1</xref>] , see <xref ref-type="fig" rid="fig1">Figure 1</xref>. The re-evaluation of the current global temperature trend [<xref ref-type="bibr" rid="scirp.56384-ref2">2</xref>] , indicates that in spite of the steadily growing trend in CO<sub>2</sub> there has been no trend in the global temperature during the last 17 years [<xref ref-type="bibr" rid="scirp.56384-ref3">3</xref>] .</p><fig id="fig1"  position="float"><label><xref ref-type="fig" rid="fig1">Figure 1</xref></label><caption><title> The atmospheric concentration (solid curve) and total emissions of CO<sub>2</sub> (dashed curve), which includes emissions from fossil-fuel combustion, cement production, and change of land-use emissions [<xref ref-type="bibr" rid="scirp.56384-ref2">2</xref>] . The trend in the growth rate of the atmospheric CO<sub>2</sub> (ppm/yr/yr) ends with the onset of the 21st century while the trend in the total CO<sub>2</sub> emission rate increases</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-2360241x5.png"/></fig><p>Considering the critical role of CO<sub>2</sub> and the Earth’s temperature for climate change, it is imperative to investigate the relationship between them in more detail.</p><p>Paper [<xref ref-type="bibr" rid="scirp.56384-ref4">4</xref>] noting the inverse phase relationship between the trends of these two variables suggested that the temperature variations were not induced by changes in atmospheric CO<sub>2</sub>. However, it has been pointed out [<xref ref-type="bibr" rid="scirp.56384-ref5">5</xref>] that a differential method used in [<xref ref-type="bibr" rid="scirp.56384-ref4">4</xref>] removes the long-term trend in the CO<sub>2</sub>. The corrected analysis showed that the temperature trend followed the CO<sub>2</sub> trend. A more general approach to the problem of phase relationship between the global temperature and all climate forcings was taken in [<xref ref-type="bibr" rid="scirp.56384-ref6">6</xref>] to test whether the global temperature follows the CO<sub>2</sub> trends.</p><p>Less controversial were the analyses of the de-trended time series. References [<xref ref-type="bibr" rid="scirp.56384-ref4">4</xref>] and [<xref ref-type="bibr" rid="scirp.56384-ref7">7</xref>] analyzed the spectra of the CO<sub>2</sub> measured at Mauna Loa Observatory (MLO) and the cross-correlations between the CO<sub>2</sub> and global temperature and found that their Fourier spectra were similar to each other in the period range 2 - 10 years, and that the global temperature oscillations were leading the CO<sub>2</sub> by about 7 - 11 months. Three spectral lines (2.4 - 2.5, 3.6 - 3.8, and 8 - 9 years) were found to be close to spectral lines observed in the global atmospheric momentum oscillations and the length of day variability associated with it [<xref ref-type="bibr" rid="scirp.56384-ref8">8</xref>] - [<xref ref-type="bibr" rid="scirp.56384-ref10">10</xref>] . These spectral analyses indicated a physical connection between the global temperature (T), CO<sub>2</sub> and El Ni&#241;o-like variability.</p><p>Here we investigate the dynamical relationship between T and CO<sub>2</sub> using the global atmospheric CO<sub>2</sub> and methods of spectral analyses that allow us to separate the long-term trend from natural oscillations and quantify their phase differences.</p></sec><sec id="s2"><title>2. The Global Atmospheric CO<sub>2</sub> and Temperature Data</title><p>To characterize the atmospheric CO<sub>2</sub> over the Earth’s globe we use the 2D distribution of zonally averaged atmospheric carbon dioxide mixing ratios from the NOAA ESRL Carbon Cycle Cooperative Global Air Sampling Network for 1979 to 2013 [<xref ref-type="bibr" rid="scirp.56384-ref11">11</xref>] . We use the monthly Earth’s surface temperature from the global CRUTEM4 data set for the same time period developed by the Climatic Research Unit at University of East Anglia in conjunction with the Hadley Centre at the UK Met Office (http://www.cru.uea.ac.uk/cru/data/temperature/).</p><p><xref ref-type="fig" rid="fig2">Figure 2</xref> shows the latitude-time distribution of the CO<sub>2</sub>. We see that as time progresses the atmospheric carbon dioxide tends to be more abundant in the Northern Hemisphere spreading around the globe within about a year. This diagram demonstrates not only an obvious fact that CO<sub>2</sub> is mostly released in the Northern Hemisphere but also a less trivial process of the CO<sub>2</sub> transport to the Southern Hemisphere and its timing. A similar distribution of the atmospheric carbon dioxide is found in the upper troposphere using satellite data [<xref ref-type="bibr" rid="scirp.56384-ref12">12</xref>] . The time series of the globally averaged atmospheric CO<sub>2</sub> and the global temperature anomaly are shown in <xref ref-type="fig" rid="fig3">Figure 3</xref> presenting the original data (panel a) and de-trended data (panel b). It is clear that the temperature trend in the 21st century does not follow the rise of CO<sub>2</sub> although it had been close to the CO<sub>2</sub> trend during the previous 30 years. However the Ocean Heat Content for the global ocean follows the globally smoothed (trend) in CO<sub>2</sub> (panel c). The de-trended and annually smoothed data (panel b) indicate a more complicated behavior of the CO<sub>2</sub> and global temperature.</p></sec><sec id="s3"><title>3. Phase Synchronization of Global Temperature and CO<sub>2</sub></title><p>It is not easy to extract clear and qualitative information about the phase relationship between CO<sub>2</sub> and global temperature T directly from their time series shown in <xref ref-type="fig" rid="fig3">Figure 3</xref>.</p><p>Modern dynamical system theories offer recurrence techniques allowing tracing the return of a variable to any of its values and comparing co-occurrences of such returns for two variables [<xref ref-type="bibr" rid="scirp.56384-ref13">13</xref>] . To investigate the relationship between the phases of our two variables (C = CO<sub>2</sub> and T) we apply the Recurrence-based Measure of</p><fig id="fig2"  position="float"><label><xref ref-type="fig" rid="fig2">Figure 2</xref></label><caption><title> The latitude-time distribution of the CO<sub>2</sub> at the Earth’s surface. The color bar units are ppm</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-2360241x6.png"/></fig><fig id="fig3"  position="float"><label><xref ref-type="fig" rid="fig3">Figure 3</xref></label><caption><title> Monthly CO<sub>2</sub> (solid) and global temperature anomaly (dash): (a) Original data; (b) De- trended data smoothed by 12 month filter for a better display; (c) Similarly smoothed the atmospheric CO<sub>2</sub> concentration (solid) and the annually averaged ocean heat content in the top 2000 meters of the ocean (dash)</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-2360241x7.png"/></fig><p>Dependence (RMD) suggested and used in [<xref ref-type="bibr" rid="scirp.56384-ref6">6</xref>]</p><disp-formula id="scirp.56384-formula86"><graphic  xlink:href="http://html.scirp.org/file/1-2360241x8.png"  xlink:type="simple"/></disp-formula><p>where <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/1-2360241x9.png" xlink:type="simple"/></inline-formula> is the time shift between C and T, n is the length of the time series, P(C<sub>i</sub>) and P(T<sub>i</sub>) are probabilities that the values of C and T return to the point C<sub>i</sub> and T<sub>i</sub> correspondingly. The joint probability P(C<sub>i</sub>, T<sub>i</sub>(<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/1-2360241x10.png" xlink:type="simple"/></inline-formula>)) captures co-occurring of the returns to C<sub>i</sub> and T<sub>i</sub> at the same time instant t = i.</p><p><xref ref-type="fig" rid="fig4">Figure 4</xref> shows the Recurrence-based Measure of Dependence (RMD) for the original and de-trended data. We see that the global temperature follows and is strongly dependent on CO<sub>2</sub> for all time lags in the original data (upper curve) but the two variables are almost independent when the trends are taken out (lower curve).</p><p>Now we investigate in detail the actual phase relationships between the de-trended CO<sub>2</sub> and T on all time scales by applying the wavelet coherence technique [<xref ref-type="bibr" rid="scirp.56384-ref14">14</xref>] allowing us to trace the phases of the two variables in time. <xref ref-type="fig" rid="fig5">Figure 5</xref> shows that phase relationships on shorter time scales than annual time scale are chaotic, but there are statistically significant correlations on the annual time scale in 1986-2008. The directions of arrows indicate that CO<sub>2</sub> is in anti-phase with the temperature changes in this period. But the directions of the arrows reversed in the beginning (in 1979) and the end (after 2010) of the data sets when CO<sub>2</sub> and T were varying in phase. On longer time scale there was a significant correlation with CO<sub>2</sub> leading T in 1994-1998, which we believe is</p><fig id="fig4"  position="float"><label><xref ref-type="fig" rid="fig4">Figure 4</xref></label><caption><title> Recurrence-based measure of dependence for the original time series of CO<sub>2</sub> and T (upper curve) and for the de-trended time series (lower curve). The curves are calculated with the Matlab software that can be found at www.agnld.uni-potsdam.de/\%7Emarwan/toolbox.php</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-2360241x11.png"/></fig><fig id="fig5"  position="float"><label><xref ref-type="fig" rid="fig5">Figure 5</xref></label><caption><title> Wavelet coherence of the globally-averaged CO<sub>2</sub> and global temperature. The thick black contours designate the 95% significance level against red noise. The cone of influence where edge effects might distort the picture is shown by side lines. The phase relationships are indicated by arrows pointing right for the in-phase CO<sub>2</sub>-T relationship, left for the anti-phase relationship, and straight up when CO<sub>2</sub> is leading the temperature anomaly</title></caption><graphic mimetype="image"   position="float"  xlink:type="simple"  xlink:href="http://html.scirp.org/file/1-2360241x12.png"/></fig><p>related to the multiple relatively strong El Ni&#241;o episodes occurred in that time period (http://www.esrl.noaa.gov/). The arrows at the time scale about 6 years clear indicate that the temperature was in phase with CO<sub>2</sub> changes in the time period preceding and following the period of the strong El Ni&#241;o episodes in 90s.</p></sec><sec id="s4"><title>4. Conclusions</title><p>We confirm the previous findings [<xref ref-type="bibr" rid="scirp.56384-ref5">5</xref>] [<xref ref-type="bibr" rid="scirp.56384-ref6">6</xref>] that trend in the global Earth’s temperature follows the trend in the atmospheric CO<sub>2</sub> before the period of the climate hiatus. However, we show that the trends are not in phase during the hiatus when the heat trapped by the atmospheric CO<sub>2</sub> goes mostly into the ocean. This is supported by comparison of the CO<sub>2</sub> trend with the trend in the ocean heat content.</p><p>We find that after the removal of the trend there are more complex phase relationships between these variables. The phase relationships are chaotic on shorter time scales than the annual time scale. On the annual time scale, the atmospheric CO<sub>2</sub> changed in anti-phase with the global temperature anomaly changes in the time period from 1986 to 2008 except for the end of it. This relationship was reversed in 1979 and after 2010 when CO<sub>2</sub> and T were changing in-phase. On the El Ni&#241;o time scale (2.3 - 7 years), the atmospheric CO<sub>2</sub> was in-phase with the global temperature changes except for the 1991-1999 time period, which included a very strong El Ni&#241;o episodes, when the time scale was suddenly changed and CO<sub>2</sub> led the global temperature.</p></sec><sec id="s5"><title>Acknowledgements</title><p>The research described in this paper was carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration.</p></sec></body><back><ref-list><title>References</title><ref id="scirp.56384-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Keeling, C.D., Whorf, T.P., Walen, M. and van der Plicht, J. (1995) Interannual Extremes in the Rate of Rise of Atmospheric Carbon Dioxide since 1980. Nature, 375, 666-670. http://dx.doi.org/10.1038/375666a0</mixed-citation></ref><ref id="scirp.56384-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Le Quere, L., et al. (2014) Global Carbon Budget 2013. Earth System Science Data, 6, 235-263.http://dx.doi.org/10.5194/essd-6-235-2014</mixed-citation></ref><ref id="scirp.56384-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">(2014) Hiatus in Context. Nature Geoscience, 7, 154. www.natute.com/naturegeoscience</mixed-citation></ref><ref id="scirp.56384-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Humlum, O., Solheim, J.-E. and Stordahl, K. (2013) The Phase Relation between Atmospheric Carbon Dioxide and Global Temperature. Global and Planetary Change, 100, 51-69. http://dx.doi.org/10.1016/j.gloplacha.2012.08.008</mixed-citation></ref><ref id="scirp.56384-ref5"><label>5</label><mixed-citation publication-type="other" xlink:type="simple">Richardson, K. (2013) Comment on “The Phase Relation between Atmospheric Carbon Dioxide and Global Temperature” by Humlum, Stordahl and Solheim. Global and Planetary Change, 107, 226-228.http://dx.doi.org/10.1016/j.gloplacha.2013.03.011</mixed-citation></ref><ref id="scirp.56384-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Goswami, B., Marwan, N., Feulner, G. and Kurths, J. (2013) How Do Global Temperature Drivers Influence Each Other? European Physical Journal Special Topics, 222, 861-873. http://dx.doi.org/10.1140/epjst/e2013-01889-8</mixed-citation></ref><ref id="scirp.56384-ref7"><label>7</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Byalko</surname><given-names> A.V. </given-names></name>,<etal>et al</etal>. (<year>2013</year>)<article-title>Spectra of Climate Perturbations</article-title><source> Priroda</source><volume> 9</volume>,<fpage> 17</fpage>-<lpage>26</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.56384-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">Dickey, J.O., Marcus, S.L. and de Viron, O. (2003) Coherent Interannual and Decadal Variations in the Atmosphere-Ocean System. Geophysical Research Letters, 30, 1573. http://dx.doi.org/10.1029/2002GL016763</mixed-citation></ref><ref id="scirp.56384-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Sidorenkov, N.S. (2009) The Interaction between Earth’s Rotation and Geophysical Processes. Wiley-VCH Verlag GmbH &amp; Co. KGaA, Weinheim. http://dx.doi.org/10.1002/9783527627721</mixed-citation></ref><ref id="scirp.56384-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">Abarca-del-Rio, R., Gambis, D. and Salstein, D. (2012) Intrdecadial Oscillations in Atmospheric Angular Momentum Variations. Journal of Geodetic Science, 2, 42-52. http://dx.doi.org/10.2478/v10156-011-0025-8</mixed-citation></ref><ref id="scirp.56384-ref11"><label>11</label><mixed-citation publication-type="other" xlink:type="simple">Dlugokency, E.J., Masarie, K.A., Lang, P.M. and Tans, P.P. (2013) NOAA Greenhouse Gas Reference from Atmospheric Carbon Dioxide.</mixed-citation></ref><ref id="scirp.56384-ref12"><label>12</label><mixed-citation publication-type="other" xlink:type="simple">Ruzmaikin, A., Aumann, H.H. and Pagano, T.S. (2012) Patterns of CO2 Variability from Global Satellite Data. Journal of Climate, 25, 6383-6393. http://dx.doi.org/10.1175/JCLI-D-11-00223.1</mixed-citation></ref><ref id="scirp.56384-ref13"><label>13</label><mixed-citation publication-type="other" xlink:type="simple">Marwan, N., Romano, M.C., Thiel, M. and Kurths, J. (2007) Recurrence Plots for the Analysis of Complex Systems. Physics Reports, 438, 237-329. http://dx.doi.org/10.1016/j.physrep.2006.11.001</mixed-citation></ref><ref id="scirp.56384-ref14"><label>14</label><mixed-citation publication-type="other" xlink:type="simple">Grinsted, A., Moore, J.C. and Jevrejeva, S. (2004) Application of the Cross Wavelet Transform and Wavelet Coherence to Geophysical Time Series. Nonlinear Processes in Geophysics, 11, 561-566.http://dx.doi.org/10.5194/npg-11-561-2004</mixed-citation></ref></ref-list></back></article>