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<front>
<journal-meta>
<journal-id journal-id-type="publisher">EGUsphere</journal-id>
<journal-title-group>
<journal-title>EGUsphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">EGUsphere</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">EGUsphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub"></issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/egusphere-2026-5141</article-id>
<title-group>
<article-title>Emergence of a non-linear global surface air temperature response to rapidly increasing effective radiative forcing</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Smith</surname>
<given-names>Craig R.</given-names>
<ext-link>https://orcid.org/0009-0003-1500-8902</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>independent scientist: Naples, Florida, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>31</day>
<month>08</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>35</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Craig R. Smith</copyright-statement>
<copyright-year>2026</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5141/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5141/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5141/egusphere-2026-5141.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5141/egusphere-2026-5141.pdf</self-uri>
<abstract>
<p>A time series of global surface air temperature anomalies (GSAT) and effective radiative forcing (ERF) obtained from IPCC Sixth Assessment Report (AR6) for 1977 to 2025 provides evidence that GSAT is a non-linear, power-law function of ERF when ERF is rapidly increasing. With ERF &amp;gt; 0 W m&lt;sup&gt;&lt;span&gt;&amp;minus;&lt;/span&gt;&lt;/sup&gt;&lt;sup&gt;2&lt;/sup&gt; (n = 48), the GSAT-ERF relationship is described by a power-law, GSAT = 0.41 + 0.11 &amp;times; ERF&lt;sup&gt;1.90&lt;/sup&gt; (R&amp;sup2; = 0.896; likely range = ERF&lt;sup&gt;1.74&lt;/sup&gt;&lt;sup&gt;-&lt;/sup&gt;&lt;sup&gt;2.24&lt;/sup&gt;). A linear relationship was rejected (F(1,45) = 15.41, p &amp;lt; 0.0003). GSAT, ERF&lt;sup&gt;1.90&lt;/sup&gt;, and the Ni&amp;ntilde;o 3.4 sea surface temperature anomaly index (ONI) were used in an autoregressive distributed lag model [ARDL(1,0,0)] yielding GSAT&lt;sub&gt;t&lt;/sub&gt; = 0.32 + 0.23 GSAT&lt;sub&gt;t-1&lt;/sub&gt; + 0.08 ERF&lt;sup&gt;1.90 &lt;/sup&gt;+ 0.11 ONI. This model is equivalent to a two-layer energy-balance model with the deep-ocean temperature held constant. The ARDL model explains 96 % of GSAT variability from 1977 to 2025 (R&lt;sup&gt;2 &lt;/sup&gt;= 0.959). Residual diagnostics indicate no evidence of residual autocorrelation or heteroskedasticity and bounds testing (&lt;em&gt;F&lt;/em&gt; = 40.51) supports cointegration. The model was validated by expanding-window recursive out-of-sample prediction from 1994 to 2025 (Theil&amp;rsquo;s U = 0.53). Earth&amp;rsquo;s climate system has entered a new regime in which the radiative response to the energy imbalance at the top of the atmosphere is progressively decreasing. ARDL projections for GSAT in 2041&lt;span&gt;&amp;ndash;&lt;/span&gt;2060 with ONI = 0 exceed the AR6 best estimate by 0.6 &amp;deg;C. If ERF continues to rise 0.7 W m&lt;sup&gt;&lt;span&gt;&amp;minus;&lt;/span&gt;&lt;/sup&gt;&lt;sup&gt;2&lt;/sup&gt; decade&lt;sup&gt;&lt;span&gt;&amp;minus;&lt;/span&gt;&lt;/sup&gt;&lt;sup&gt;1&lt;/sup&gt;, GSAT by mid-century will likely be 2.8 &amp;plusmn; 0.3 &amp;deg;C.</p>
</abstract>
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