{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,18]],"date-time":"2025-10-18T13:10:51Z","timestamp":1760793051327,"version":"build-2065373602"},"reference-count":21,"publisher":"IOP Publishing","issue":"35","license":[{"start":{"date-parts":[[2022,6,16]],"date-time":"2022-06-16T00:00:00Z","timestamp":1655337600000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/publishingsupport.iopscience.iop.org\/iop-standard\/v1"},{"start":{"date-parts":[[2022,6,16]],"date-time":"2022-06-16T00:00:00Z","timestamp":1655337600000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/iopscience.iop.org\/info\/page\/text-and-data-mining"}],"content-domain":{"domain":["iopscience.iop.org"],"crossmark-restriction":false},"short-container-title":["J. Phys. D: Appl. Phys."],"published-print":{"date-parts":[[2022,9,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n               <jats:p>The paper titled \u2018Collision and radiative processes in emission of atmospheric carbon dioxide\u2019 (Smirnov 2018 <jats:italic>J. Phys. D: Appl. Phys.<\/jats:italic>\n                  <jats:bold>51<\/jats:bold> 214004) dismisses the role of increasing concentrations of anthropogenic CO<jats:sub>2<\/jats:sub> on global warming of planet Earth. We show that these conclusions are the consequence of two flaws in the paper theoretical model which neglect the effects of the increased concentrations of CO<jats:sub>2<\/jats:sub> on the absorption of Earth\u2019s blackbody radiation in the 12\u201315\u2009<jats:italic>\u00b5<\/jats:italic>m region. The influence of doubling the concentration of CO<jats:sub>2<\/jats:sub> in the atmosphere on the surface temperature is not <jats:inline-formula>\n                     <jats:tex-math\/>\n                     <mml:math xmlns:mml=\"http:\/\/www.w3.org\/1998\/Math\/MathML\" overflow=\"scroll\">\n                        <mml:mi mathvariant=\"normal\">\u0394<\/mml:mi>\n                        <mml:mi>T<\/mml:mi>\n                        <mml:mo>=<\/mml:mo>\n                        <mml:mn>0.02<\/mml:mn>\n                     <\/mml:math>\n                  \n                  <\/jats:inline-formula>\u2009K, or even <jats:inline-formula>\n                     <jats:tex-math\/>\n                     <mml:math xmlns:mml=\"http:\/\/www.w3.org\/1998\/Math\/MathML\" overflow=\"scroll\">\n                        <mml:mi mathvariant=\"normal\">\u0394<\/mml:mi>\n                        <mml:mi>T<\/mml:mi>\n                        <mml:mo>=<\/mml:mo>\n                        <mml:mn>0.4<\/mml:mn>\n                     <\/mml:math>\n                  \n                  <\/jats:inline-formula>\u2009K if only one of the two mistakes in the paper\u2019s analysis is corrected. The correct value lies within <jats:inline-formula>\n                     <jats:tex-math\/>\n                     <mml:math xmlns:mml=\"http:\/\/www.w3.org\/1998\/Math\/MathML\" overflow=\"scroll\">\n                        <mml:mi mathvariant=\"normal\">\u0394<\/mml:mi>\n                        <mml:mi>T<\/mml:mi>\n                        <mml:mo>=<\/mml:mo>\n                        <mml:mn>1.1<\/mml:mn>\n                        <mml:mo>\u2212<\/mml:mo>\n                        <mml:mn>1.3<\/mml:mn>\n                     <\/mml:math>\n                  \n                  <\/jats:inline-formula>\u2009K as outlined by Wilson and Gea-Banacloche (2012 <jats:italic>Am. J. Phys.<\/jats:italic>\n                  <jats:bold>80<\/jats:bold> 306\u201315) using simplified, yet more theoretically consistent models. In addition, if feedback effects are factored in, a higher value of <jats:inline-formula>\n                     <jats:tex-math\/>\n                     <mml:math xmlns:mml=\"http:\/\/www.w3.org\/1998\/Math\/MathML\" overflow=\"scroll\">\n                        <mml:mi mathvariant=\"normal\">\u0394<\/mml:mi>\n                        <mml:mi>T<\/mml:mi>\n                        <mml:mo>=<\/mml:mo>\n                        <mml:mn>3<\/mml:mn>\n                     <\/mml:math>\n                  \n                  <\/jats:inline-formula>\u2009K is predicted, as assessed in the latest Intergovernmental Panel on Climate Change working group report of 2021.<\/jats:p>","DOI":"10.1088\/1361-6463\/ac7758","type":"journal-article","created":{"date-parts":[[2022,6,16]],"date-time":"2022-06-16T04:36:21Z","timestamp":1655354181000},"page":"358001","update-policy":"https:\/\/doi.org\/10.1088\/crossmark-policy","source":"Crossref","is-referenced-by-count":0,"title":["Comment on \u2018Collision and radiative processes in emission of atmospheric carbon dioxide\u2019"],"prefix":"10.1088","volume":"55","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-1993-1548","authenticated-orcid":true,"given":"M","family":"Lino da Silva","sequence":"first","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-5909-1512","authenticated-orcid":false,"given":"J","family":"Vargas","sequence":"additional","affiliation":[]}],"member":"266","published-online":{"date-parts":[[2022,6,16]]},"reference":[{"key":"dac7758bib1","doi-asserted-by":"publisher","DOI":"10.1088\/1361-6463\/aabac6","type":"journal-article","article-title":"Collision and radiative processes in emission of atmospheric carbon dioxide","volume":"51","author":"Smirnov","year":"2018","journal-title":"J. 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