<?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">
    acs
   </journal-id>
   <journal-title-group>
    <journal-title>
     Atmospheric and Climate Sciences
    </journal-title>
   </journal-title-group>
   <issn pub-type="epub">
    2160-0414
   </issn>
   <issn publication-format="print">
    2160-0422
   </issn>
   <publisher>
    <publisher-name>
     Scientific Research Publishing
    </publisher-name>
   </publisher>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="doi">
    10.4236/acs.2025.153033
   </article-id>
   <article-id pub-id-type="publisher-id">
    acs-144123
   </article-id>
   <article-categories>
    <subj-group subj-group-type="heading">
     <subject>
      Articles
     </subject>
    </subj-group>
    <subj-group subj-group-type="Discipline-v2">
     <subject>
      Earth 
     </subject>
     <subject>
       Environmental Sciences
     </subject>
    </subj-group>
   </article-categories>
   <title-group>
    Time Lag in Changes in Global Temperature and CO
    <sub>2</sub> Concentration Following Changes in the Oceanic Niño Index
   </title-group>
   <contrib-group>
    <contrib contrib-type="author" xlink:type="simple">
     <name name-style="western">
      <surname>
       Masaharu
      </surname>
      <given-names>
       Nishioka
      </given-names>
     </name>
    </contrib>
   </contrib-group> 
   <aff id="affnull">
    <addr-line>
     aRetired, Chicago, IL, USA
    </addr-line> 
   </aff> 
   <pub-date pub-type="epub">
    <day>
     23
    </day> 
    <month>
     05
    </month>
    <year>
     2025
    </year>
   </pub-date> 
   <volume>
    15
   </volume> 
   <issue>
    03
   </issue>
   <fpage>
    668
   </fpage>
   <lpage>
    680
   </lpage>
   <history>
    <date date-type="received">
     <day>
      16,
     </day>
     <month>
      June
     </month>
     <year>
      2025
     </year>
    </date>
    <date date-type="published">
     <day>
      18,
     </day>
     <month>
      June
     </month>
     <year>
      2025
     </year> 
    </date> 
    <date date-type="accepted">
     <day>
      18,
     </day>
     <month>
      July
     </month>
     <year>
      2025
     </year> 
    </date>
   </history>
   <permissions>
    <copyright-statement>
     © 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>
    Satellite measurements of global temperature began in 1979. According to the results of these measurements, the correlation between the global temperature and ocean temperature is very good, with a correlation coefficient of 0.99. The global temperature is controlled by the ocean temperature. The ocean temperature is not always constant but changes periodically, with high and low temperatures occurring repeatedly. This phenomenon is known as the El Niño or La Niña phenomenon. El Niño and La Niña phenomena are monitored by temperature changes in a specific area of the equator in the Pacific Ocean and are called the Oceanic Niño Index (ONI). When the ONI fluctuates significantly, El Niño and La Niña phenomena occur. A comparison of the ONI data from the National Oceanic and Atmospheric Administration (NOAA) and the global temperature data reveals that the temperature change throughout the entire Earth occurred approximately five months after the ONI change. At the western end of the Pacific Ocean, the direction of the warm current changes, and a warm current flows northward via the coast of the Japanese Islands. Even in such a unique location, the temperature change during the El Niño phenomenon changed five months later than did the change in the ONI value. Measurements of atmospheric CO
    <sub>2</sub> concentrations at the Mauna Loa Observatory in Hawaii began in 1958. We compared these CO
    <sub>2</sub> concentration changes with the above global temperature changes via NOAA data. As a result, we found that changes in global CO
    <sub>2</sub> concentrations appeared approximately four months after global temperature changes. The CO
    <sub>2</sub> concentration increases with increasing temperature. El Niño and La Niña phenomena are observed as small fluctuations in atmospheric CO
    <sub>2</sub> concentrations. This is mainly due to increased plant respiration and accelerated decomposition of organic matter in soils due to rising temperatures. CO
    <sub>2</sub> emissions from the ocean are also thought to have a significant impact, but quantitative investigations are a future task. On the other hand, compared with the global CO
    <sub>2</sub> balance, CO
    <sub>2</sub> emissions from anthropogenic activities are low. Our recent research results revealed that temperature and CO
    <sub>2</sub> changes are correlated, but CO
    <sub>2</sub> changes are the result of temperature changes, and we have not found that CO
    <sub>2</sub> changes cause temperature changes.
   </abstract>
   <kwd-group> 
    <kwd>
     Global Warming
    </kwd> 
    <kwd>
      Anthropogenic CO
     <sub>2</sub>
    </kwd> 
    <kwd>
      Thermally Induced CO
     <sub>2</sub>
    </kwd> 
    <kwd>
      Soil Respiration
    </kwd> 
    <kwd>
      Cross-Correlation
    </kwd> 
    <kwd>
      Time Lag
    </kwd> 
    <kwd>
      El Niño
    </kwd> 
    <kwd>
      Oceanic Niño Index
    </kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <sec id="s1">
   <title>1. Introduction</title>
   <p>Analyses of Antarctic ice cores revealed that temperature changes preceded changes in CO<sub>2</sub> concentrations by hundreds to thousands of years in past glacial and interglacial cycles <xref ref-type="bibr" rid="scirp.144123-1">
     [1]
    </xref>. However, the Intergovernmental Panel on Climate Change (IPCC) states that modern warming differs from past natural climate changes in that it is the result of a rapid increase in atmospheric CO<sub>2</sub> concentrations caused by human activity, which has intensified the greenhouse effect and caused the Earth’s temperature to rise <xref ref-type="bibr" rid="scirp.144123-2">
     [2]
    </xref>. This means that the increase in CO<sub>2</sub> may precede the increase in Earth’s temperature, and the Earth’s temperature may continue to rise.</p>
   <p>Humlum et al. <xref ref-type="bibr" rid="scirp.144123-3">
     [3]
    </xref> examined the relationship between changes in CO<sub>2</sub> concentration and land-sea surface temperature over the period from January 1980 to December 2011 and reported that changes in CO<sub>2</sub> always lag changes in temperature by 10 - 12 months. Wang et al. <xref ref-type="bibr" rid="scirp.144123-4">
     [4]
    </xref> analyzed the relationships between the Mauna Loa atmospheric CO<sub>2</sub> growth rate and tropical land climatic elements. They reported that the Mauna Loa CO<sub>2</sub> growth rate lags precipitation by 4 months, leads temperature by 1 month, and correlates with soil moisture with a zero.</p>
   <p>On the basis of our recent analysis <xref ref-type="bibr" rid="scirp.144123-5">
     [5]
    </xref>, the temperature change and rate of CO<sub>2</sub> change are correlated with a temperature-leading time lag. The correlation was investigated by calculating a correlation coefficient r of these changes for selected ENSO events in the study. Annual periodical increases and decreases in the CO<sub>2</sub> concentration were considered, with a regular pattern of minimum values in August and maximum values in May each year. An increased deviation in CO<sub>2</sub> and temperature was found in response to the occurrence of El Niño, but the increase in CO<sub>2</sub> lagged behind the change in temperature by 5 months. This pattern was not observed for La Niña events. An increase in global CO<sub>2</sub> emissions and a subsequent increase in global temperature proposed by the IPCC were not observed, but an increase in global temperature, an increase in soil respiration, and a subsequent increase in global CO<sub>2</sub> emissions were noticed. This natural process can be clearly detected during periods of increasing temperature, specifically during El Niño events. The results cast strong doubts that anthropogenic CO<sub>2</sub> is the cause of global warming.</p>
   <p>When El Niño events occur, an increase in the global temperature is usually observed several months later <xref ref-type="bibr" rid="scirp.144123-6">
     [6]
    </xref> <xref ref-type="bibr" rid="scirp.144123-7">
     [7]
    </xref>. El Niño is a climate phenomenon characterized by the warming of sea surface temperatures in the central and eastern Pacific Oceans. While the exact causes of El Niño events are complex, several key factors that contribute to El Niño occurrence may be summarized as follows <xref ref-type="bibr" rid="scirp.144123-8">
     [8]
    </xref>-<xref ref-type="bibr" rid="scirp.144123-10">
     [10]
    </xref>. El Niño events are driven primarily by a weakening of Pacific trade winds, which disrupts normal ocean-atmosphere interactions. This weakening allows warmer water from the western Pacific to spread eastward, leading to positive sea surface temperature anomalies in the central and eastern equatorial Pacific. These warmer surface waters then deepen the thermocline, further reinforcing warming and atmospheric changes. While influenced by natural climate cycles, the critical factors are the initial weakening of trade winds, the subsequent ocean-atmosphere feedback, and the resulting changes in sea surface temperatures and thermocline depth.</p>
   <p>The Oceanic Niño Index (ONI) is an index that reflects fluctuations in sea surface temperatures in the equatorial Pacific Ocean. The National Oceanic and Atmospheric Administration (NOAA) considers El Niño conditions to be present in the ocean when the ONI in that area, known as the Niño-3.4 region (see <xref ref-type="fig" rid="fig1">
     Figure 1
    </xref>) <xref ref-type="bibr" rid="scirp.144123-11">
     [11]
    </xref>, is +0.5 or higher, meaning that surface waters in the east-central tropical Pacific are 0.5˚C warmer than average. Oceanic La Niña conditions exist when the ONI is −0.5 or lower, indicating that the region is 0.5˚C or greater, which is cooler than average. The Niño-3.4 region is the east-central equatorial Pacific between 5N-5S, 170W-120W, which is approximately 6.179 × 10<sup>6</sup> km<sup>2</sup> and 1.2% of the Earth’s surface area, approximately 510.1 × 10<sup>6</sup> km<sup>2</sup>.</p>
   <fig id="fig1" position="float">
    <label>Figure 1</label>
    <caption>
     <title>Figure 1. Locations of the parts (the Niño 3.4 region) of the tropical Pacific used for monitoring sea surface temperature to determine NOAA’s official Oceanic Niño Index <xref ref-type="bibr" rid="scirp.144123-11">
       [11]
      </xref>.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId15.jpeg?20250721015048" />
   </fig>
   <p>Our recent research <xref ref-type="bibr" rid="scirp.144123-5">
     [5]
    </xref> <xref ref-type="bibr" rid="scirp.144123-12">
     [12]
    </xref>-<xref ref-type="bibr" rid="scirp.144123-16">
     [16]
    </xref> has shown that global temperature changes precede changes in CO<sub>2</sub> concentrations by 5 months. Therefore, rising temperatures may induce increased CO<sub>2</sub> emissions. This phenomenon is due mainly to the promotion of soil respiration. Large amounts of “thermally induced CO<sub>2</sub>” are emitted, especially from midlatitude forests. “Thermally induced CO<sub>2</sub>” is more temperature dependent than the amount emitted from tropical rainforests. Moreover, its amount significantly exceeds anthropogenic emissions. This process can be organized as shown in <xref ref-type="fig" rid="fig2">
     Figure 2
    </xref> <xref ref-type="bibr" rid="scirp.144123-16">
     [16]
    </xref>. This differs from the view of the IPCC.</p>
   <p>The IPCC proposed that anthropogenic CO<sub>2</sub> is causing global warming through the greenhouse effect. The observed temperature-leading process suggests a natural phenomenon via soil respiration, casting doubt on the theory that anthropogenic CO<sub>2</sub> is the only cause. Considering the important role of temperature-dependent soil respiration, it is necessary to consider whether the current efforts to reduce anthropogenic CO<sub>2</sub> emissions are effective in lowering global CO<sub>2</sub> concentrations <xref ref-type="bibr" rid="scirp.144123-16">
     [16]
    </xref>. The purpose of this paper is to further clarify and confirm the process summarized in <xref ref-type="fig" rid="fig2">
     Figure 2
    </xref>. To do so, we focus on the ONI, which is an index of the ENSO process. We then consider the time-dependent changes in the ONI, global temperature, and CO<sub>2</sub> concentration and the processes by which they change.</p>
   <fig id="fig2" position="float">
    <label>Figure 2</label>
    <caption>
     <title>Figure 2. Processes of increases in atmospheric CO<sub>2</sub> during the modern warm period <xref ref-type="bibr" rid="scirp.144123-16">
       [16]
      </xref>.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId16.jpeg?20250721015048" />
   </fig>
  </sec><sec id="s2">
   <title>2. Global Data</title>
   <p>The ONI data are reported by the National Oceanic and Atmospheric Administration (NOAA), and all the original data were downloaded <xref ref-type="bibr" rid="scirp.144123-11">
     [11]
    </xref>. The three-month average ONI values were used.</p>
   <p>Since 1979, the University of Alabama in Huntsville (UAH) has updated global temperature datasets that represent the piecing together of temperature data from a total of fifteen instruments flying on different satellites. Further details are available <xref ref-type="bibr" rid="scirp.144123-17">
     [17]
    </xref>. Temperatures here were obtained from the datasets, and the 13-month average of lower troposphere anomaly values was used, where the temperatures were averaged over the 6 months before and after each specific month.</p>
   <p>In general, the correlation coefficient r between variables x and y can be defined as follows:</p>
   <p>
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   <p>For convenience, r can be easily calculated via built-in functions in Microsoft Excel®. This calculated r is used to show correlations between two variables throughout this paper.</p>
   <p>The annual mean growth rate of CO<sub>2</sub> in a given year is the difference in concentration between the end of December and the start of January of that year reported by NOAA. Further details are available on their website <xref ref-type="bibr" rid="scirp.144123-18">
     [18]
    </xref>. Because of the seasonal changes in CO<sub>2</sub> concentrations, the annual means and the monthly data are compared.</p>
   <p>Monthly average temperature data in Japan were obtained from 15 locations selected from meteorological observation stations that have been conducting observations since 1898 by the Japan Meteorological Agency, with little impact from urbanization and without bias toward specific regions. For each location, the deviation of the monthly average temperature (observed monthly average temperature minus the 30-year average from 1991to 2020) is calculated <xref ref-type="bibr" rid="scirp.144123-19">
     [19]
    </xref>.</p>
  </sec><sec id="s3">
   <title>3. Results and Discussion</title>
   <p>The 13-month average global and ocean temperatures based on satellite observations are available from the UAH database <xref ref-type="bibr" rid="scirp.144123-17">
     [17]
    </xref>. <xref ref-type="fig" rid="fig3">
     Figure 3
    </xref> compares these results between 1979 and 2023. Both results are well correlated, with a correlation coefficient of 0.993. This means that the global temperature is almost completely controlled by the ocean temperature.</p>
   <fig id="fig3" position="float">
    <label>Figure 3</label>
    <caption>
     <title>Figure 3. Correlation between the global temperature anomaly (red line, ˚C) and ocean temperature (blue line, ˚C) between 1979 and 2023.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId19.jpeg?20250721015050" />
   </fig>
   <p>
    <xref ref-type="fig" rid="fig4(a)">
     Figure 4(a)
    </xref> compares the changes in the ONI values obtained from NOAA and satellite-based global temperatures between 1979 and 2023. The correlation coefficient between the two is 0.143. The global temperatures lag behind the ONI. Therefore, the correlation coefficient between the ONI and global temperature was investigated by changing the lag time (in months). <xref ref-type="fig" rid="fig4(b)">
     Figure 4(b)
    </xref> shows the result. The value at which the correlation coefficient is maximized indicates that the global temperature changes with a lag of approximately five months compared with the ONI value.</p>
   <fig-group id="fig4" position="float">
    <fig id="fig4" position="float">
     <label>Figure 4</label>
     <caption>
      <title>Figure 4. (a) Correlations between global temperature anomalies (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis) and (b) Changes in correlation coefficients with time lag (in months).--Figure 4. (a) Correlations between global temperature anomalies (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis) and (b) Changes in correlation coefficients with time lag (in months).</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId20.jpeg?20250721015050" />
    </fig>
    <fig id="fig4" position="float">
     <label>Figure 4</label>
     <caption>
      <title>Figure 4. (a) Correlations between global temperature anomalies (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis) and (b) Changes in correlation coefficients with time lag (in months).--Figure 4. (a) Correlations between global temperature anomalies (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis) and (b) Changes in correlation coefficients with time lag (in months).</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId21.jpeg?20250721015051" />
    </fig>
   </fig-group>
   <p>Oceanic gyres are large systems of circular ocean currents <xref ref-type="bibr" rid="scirp.144123-20">
     [20]
    </xref> driven primarily by global wind patterns and the Coriolis effect, which deflect moving water. Oceanic gyres are broadly shown in <xref ref-type="fig" rid="fig5">
     Figure 5
    </xref> <xref ref-type="bibr" rid="scirp.144123-21">
     [21]
    </xref>. While gyres are generally stable, their formation and characteristics can be significantly influenced by phenomena such as the El Niño-Southern Oscillation (ENSO).</p>
   <fig id="fig5" position="float">
    <label>Figure 5</label>
    <caption>
     <title>Figure 5. This map broadly shows the formation of different gyres in the ocean <xref ref-type="bibr" rid="scirp.144123-21">
       [21]
      </xref>.</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId22.jpeg?20250721015051" />
   </fig>
   <p>The Niño 3.4 region shown in <xref ref-type="fig" rid="fig1">
     Figure 1
    </xref>, which is used to monitor the ONI, is located near the equator, and the ocean currents flowing through this region head westward. Then, at the western end of the Pacific Ocean, they turn northward in the Northern Hemisphere, whereas in the Southern Hemisphere, they turn southward. The warm current flowing east of the Japanese Islands is called the Kuroshio Current. During El Niño events, the Kuroshio Current may cause an increase in temperature near the Japanese Islands. Therefore, the relationship between the ONI and temperature changes in Japan was investigated during two El Niño events. <xref ref-type="fig" rid="fig6(a)">
     Figure 6(a)
    </xref> compares the changes in the ONI values obtained from NOAA and the temperature anomalies in Japan from the Japan Meteorological Agency between Jan. 2015 and Dec. 2016. The correlation coefficient between the two is 0.0194. The global temperatures lag behind the ONI, and the correlation coefficient between the two is 0.855 after moving temperatures by 5 months ahead. Similarly, <xref ref-type="fig" rid="fig6(b)">
     Figure 6(b)
    </xref> compares the changes in the ONI and temperature anomalies in Japan between September 2022 and August 2024. The correlation coefficient between the two is 0.809 and 0.843 after moving temperatures by 5 months ahead. The local temperature changes with a lag of five months compared with the ONI value during these El Niño events.</p>
   <p>We found here that temperature changes can be observed at a global scale and in selected places where warm currents flow. They are particularly noticeable when El Niño events occur. We next investigate ONI fluctuations, subsequent fluctuations in global temperature, and how CO<sub>2</sub> changes due to fluctuations in global temperature.</p>
   <fig-group id="fig6" position="float">
    <fig id="fig6" position="float">
     <label>Figure 6</label>
     <caption>
      <title>Figure 6. Correlation between temperature anomalies in Japan (by the Japan Meteorological Agency) (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis): (a) Durations of Jan. 2015 and Dec. 2016 and (b) Durations of Sept. 2022 and Aug. 2024.--Figure 6. Correlation between temperature anomalies in Japan (by the Japan Meteorological Agency) (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis): (a) Durations of Jan. 2015 and Dec. 2016 and (b) Durations of Sept. 2022 and Aug. 2024.</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId23.jpeg?20250721015051" />
    </fig>
    <fig id="fig6" position="float">
     <label>Figure 6</label>
     <caption>
      <title>Figure 6. Correlation between temperature anomalies in Japan (by the Japan Meteorological Agency) (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis): (a) Durations of Jan. 2015 and Dec. 2016 and (b) Durations of Sept. 2022 and Aug. 2024.--Figure 6. Correlation between temperature anomalies in Japan (by the Japan Meteorological Agency) (red line, scale: right axis, ˚C) and the ONI (blue line, scale: left axis): (a) Durations of Jan. 2015 and Dec. 2016 and (b) Durations of Sept. 2022 and Aug. 2024.</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId24.jpeg?20250721015051" />
    </fig>
   </fig-group>
   <p>Global temperature anomalies and CO<sub>2</sub> annual growth rates are correlated over 40 years, as reported in our recent paper <xref ref-type="bibr" rid="scirp.144123-5">
     [5]
    </xref>. The 12-month average CO<sub>2</sub> annual growth rates are reported by NOAA <xref ref-type="bibr" rid="scirp.144123-18">
     [18]
    </xref>. The latest correlation between July 1979 and December 2023 is shown in <xref ref-type="fig" rid="fig7">
     Figure 7
    </xref>. Its correlation coefficient r is 0.744, and the correlation is relatively good.</p>
   <p>Since the 13-month average of temperature change and the annual average of the rate of CO<sub>2</sub> increase are used in <xref ref-type="fig" rid="fig7">
     Figure 7
    </xref>, a time lag within 12 months between two variables cannot be effectively analyzed. <xref ref-type="fig" rid="fig8(a)">
     Figure 8(a)
    </xref> compares global temperature anomalies and CO<sub>2</sub> monthly growth rates instead of CO<sub>2</sub> annual growth rates between 1980 and 2023. The correlation coefficient between the two is 0.664. The CO<sub>2</sub> growth rates lag behind the global temperatures. Therefore, the correlation coefficient between the CO<sub>2</sub> growth rates and global temperatures was investigated by changing the lag time (in months). <xref ref-type="fig" rid="fig8(b)">
     Figure 8(b)
    </xref> shows the result. The value at which the correlation coefficient is maximized indicates that the CO<sub>2</sub> growth rate changes with a lag of approximately four months compared with the global temperature.</p>
   <fig id="fig7" position="float">
    <label>Figure 7</label>
    <caption>
     <title>Figure 7. Correlation between the global temperature anomaly (red line, scale: left axis, ˚C) and 12-month average annual CO<sub>2</sub> growth rates (blue bar, scale: right axis, ppm/year).</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId25.jpeg?20250721015051" />
   </fig>
   <fig-group id="fig8" position="float">
    <fig id="fig8" position="float">
     <label>Figure 8</label>
     <caption>
      <title>Figure 8. (a) Correlations between global temperature anomalies (red line, scale: left axis, ˚C) and monthly CO2 annual growth rates (ΔCO2, blue line, scale: right axis, ppm/year) and (b) changes in correlation coefficients with time lag (in months).--Figure 8. (a) Correlations between global temperature anomalies (red line, scale: left axis, ˚C) and monthly CO2 annual growth rates (ΔCO2, blue line, scale: right axis, ppm/year) and (b) changes in correlation coefficients with time lag (in months).</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId26.jpeg?20250721015051" />
    </fig>
    <fig id="fig8" position="float">
     <label>Figure 8</label>
     <caption>
      <title>Figure 8. (a) Correlations between global temperature anomalies (red line, scale: left axis, ˚C) and monthly CO2 annual growth rates (ΔCO2, blue line, scale: right axis, ppm/year) and (b) changes in correlation coefficients with time lag (in months).--Figure 8. (a) Correlations between global temperature anomalies (red line, scale: left axis, ˚C) and monthly CO2 annual growth rates (ΔCO2, blue line, scale: right axis, ppm/year) and (b) changes in correlation coefficients with time lag (in months).</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId27.jpeg?20250721015050" />
    </fig>
   </fig-group>
   <p>
    <xref ref-type="fig" rid="fig9">
     Figure 9
    </xref> shows the correlation between global temperature anomalies and monthly CO<sub>2</sub> growth rates during two El Niño events between (a) Jan. 2015 and Dec. 2016 and (b) Sep. 2022 and Aug. 2024. The correlation coefficients between the two variables increased (a) 0.901 from 0.705 and (b) 0.973 from 0.822 when time lags of (a) five months and (b) four months were considered. The temperature change and rate of CO<sub>2</sub> change are correlated with a time lag, as reported in a previous paper <xref ref-type="bibr" rid="scirp.144123-5">
     [5]
    </xref>. The time lag of CO<sub>2</sub> behind the change in temperature was five months. The time lags of four and five months in <xref ref-type="fig" rid="fig9">
     Figure 9
    </xref> are coincident with the results in the previous paper <xref ref-type="bibr" rid="scirp.144123-5">
     [5]
    </xref>.</p>
   <fig-group id="fig9" position="float">
    <fig id="fig9" position="float">
     <label>Figure 9</label>
     <caption>
      <title>Figure 9. Correlation between the global temperature anomaly and monthly CO2 growth rates during El Niño between (a) Jan. 2015 and Dec. 2016 and between (b) Sep. 2022 and Aug. 2024.--Figure 9. Correlation between the global temperature anomaly and monthly CO2 growth rates during El Niño between (a) Jan. 2015 and Dec. 2016 and between (b) Sep. 2022 and Aug. 2024.</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId28.jpeg?20250721015050" />
    </fig>
    <fig id="fig9" position="float">
     <label>Figure 9</label>
     <caption>
      <title>Figure 9. Correlation between the global temperature anomaly and monthly CO2 growth rates during El Niño between (a) Jan. 2015 and Dec. 2016 and between (b) Sep. 2022 and Aug. 2024.--Figure 9. Correlation between the global temperature anomaly and monthly CO2 growth rates during El Niño between (a) Jan. 2015 and Dec. 2016 and between (b) Sep. 2022 and Aug. 2024.</title>
     </caption>
     <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId29.jpeg?20250721015050" />
    </fig>
   </fig-group>
   <p>The results summarized here show that there is a correlation between ONI (or ENSO) variations, changes in global temperature, and changes in CO<sub>2</sub> concentration. There is a time lag between these correlations. The overall results are consistent with the results reported in previous papers and can be summarized, as shown in <xref ref-type="fig" rid="fig10">
     Figure 10
    </xref>, from the results in <xref ref-type="fig" rid="fig4(a)">
     Figure 4(a)
    </xref> and <xref ref-type="fig" rid="fig8(a)">
     Figure 8(a)
    </xref>. The results show that changes in CO<sub>2</sub> concentration do not cause changes in global temperature but rather that changes in global temperature cause changes in CO<sub>2</sub> concentration.</p>
   <fig id="fig10" position="float">
    <label>Figure 10</label>
    <caption>
     <title>Figure 10. Time lag in changes in global temperature and global CO<sub>2</sub> concentration following changes in the Oceanic Niño Index (ONI).</title>
    </caption>
    <graphic mimetype="image" position="float" xlink:type="simple" xlink:href="https://html.scirp.org/file/4701352-rId30.jpeg?20250721015050" />
   </fig>
   <p>Our recent research has shown that soil respiration and ocean CO<sub>2</sub> emissions significantly contribute to atmospheric CO<sub>2</sub> concentration changes as global temperatures rise, which is based on the global CO<sub>2</sub> balance <xref ref-type="bibr" rid="scirp.144123-13">
     [13]
    </xref> <xref ref-type="bibr" rid="scirp.144123-14">
     [14]
    </xref> <xref ref-type="bibr" rid="scirp.144123-16">
     [16]
    </xref>. The general process changes are shown in <xref ref-type="fig" rid="fig2">
     Figure 2
    </xref>. The quantitative investigation of ocean emissions is a future challenge. When ONI changes are large, ENSO appears. This event is characterized by small fluctuations in the atmospheric CO<sub>2</sub> concentration <xref ref-type="bibr" rid="scirp.144123-16">
     [16]
    </xref>. Compared with these CO<sub>2</sub> balance amounts, the amount of CO<sub>2</sub> emissions due to anthropogenic activities is small <xref ref-type="bibr" rid="scirp.144123-16">
     [16]
    </xref>.</p>
  </sec><sec id="s4">
   <title>4. Conclusions</title>
   <p>The ONI is an index that indicates the variation in sea surface temperature in the equatorial Pacific Ocean. When the ONI varies greatly, El Niño or La Niña phenomena occur. Changes in global temperature appear approximately 5 months after ONI variations (<xref ref-type="fig" rid="fig4">
     Figure 4
    </xref>). El Niño events cause the temperature to rise, whereas La Niña events cause the temperature to decrease. There are peculiar places where the direction of the warm current has changed, such as the western end of the Pacific Ocean, such as the Japanese Islands. In these peculiar places, during El Niño events, the temperature changes 5 months later than the ONI value changes (<xref ref-type="fig" rid="fig6">
     Figure 6
    </xref>).</p>
   <p>Additionally, changes in the global CO<sub>2</sub> concentration appeared approximately 4 months after the global temperature change (<xref ref-type="fig" rid="fig8">
     Figure 8
    </xref>). The CO<sub>2</sub> concentration tends to increase with increasing temperature. El Niño or La Niña phenomena are small perturbations in the atmospheric CO<sub>2</sub> concentration. This is mainly due to increased plant respiration and accelerated decomposition of organic matter in soil due to rising temperatures and is thought to be largely due to CO<sub>2</sub> emissions from the ocean. A quantitative investigation of emissions from the ocean is a future task. Compared with these CO<sub>2</sub> budgets, CO<sub>2</sub> emissions from anthropogenic activities are small.</p>
   <p>Our recent results, including those of this work, reveal that temperature and CO<sub>2</sub> changes are correlated, but CO<sub>2</sub> changes are the result of temperature changes, and we have not found that CO<sub>2</sub> changes cause temperature changes (<xref ref-type="fig" rid="fig2">
     Figure 2
    </xref>).</p>
  </sec><sec id="s5">
   <title>Abbreviations</title>
   <table class="MsoTableGrid custom-table" border="0" cellspacing="0" cellpadding="0"> 
    <tr> 
     <td class="aleft"><p style="text-align:left">ONI</p></td> 
     <td class="aleft"><p style="text-align:left">Oceanic Niño Index</p></td> 
    </tr> 
    <tr> 
     <td class="aleft"><p style="text-align:left">ENSO</p></td> 
     <td class="aleft"><p style="text-align:left">El Niño-Southern Oscillation</p></td> 
    </tr> 
    <tr> 
     <td class="aleft"><p style="text-align:left">IPCC</p></td> 
     <td class="aleft"><p style="text-align:left">Intergovernmental Panel on Climate Change (the United Nations body)</p></td> 
    </tr> 
    <tr> 
     <td class="aleft"><p style="text-align:left">NOAA</p></td> 
     <td class="aleft"><p style="text-align:left">National Oceanic and Atmospheric Administration</p></td> 
    </tr> 
    <tr> 
     <td class="aleft"><p style="text-align:left">UAH</p></td> 
     <td class="aleft"><p style="text-align:left">University of Alabama in Huntsville</p></td> 
    </tr> 
    <tr> 
     <td class="aleft"><p style="text-align:left">r</p></td> 
     <td class="aleft"><p style="text-align:left">Correlation Coefficient</p></td> 
    </tr> 
   </table>
  </sec>
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