Variations in the Arctic upper atmosphere since the early 20th century: Relation to Arctic surface warming and cooling

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Analysis of Tromsø ionosonde data from 1932 reveals increasing foF2 trends during Arctic surface cooling (1940s-1960s) and decreasing trends since 2001, correlating with Arctic warming.

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The paper analyzes long-term ionospheric changes using Tromsø ionosonde observations from 1932 onward, building a database to examine daily variations over roughly 90 years. It reports that during the 1940s to 1960s—when Arctic surface temperatures were cooling—there was a gradually increasing trend in the F2-layer critical frequency (foF2) at 0.022 ± 0.011 MHz/year, attributed to changes consistent with Earth’s global atmospheric energy balance, and that since 2001 foF2 shows a clear decrease at -0.046 ± 0.007 MHz/year. The authors state that these trends are qualitatively consistent with upper-atmosphere changes inferred from Arctic surface warming and cooling, but they note that verification of the proposed scenario will require further study with global models. The paper does not explicitly discuss endometriosis or adenomyosis; it was included in the corpus via a keyword match in the upstream search index.

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Abstract

Abstract We have studied long-term ionospheric variations using data from the Tromsø ionosonde since 1932. To investigate Arctic ionospheric variations in relation to the Arctic warming and cooling before the 1970s, we have developed a Tromsø ionosonde database that makes it possible to study the daily variations over about 90 years. During the 1940s to 1960s, when the Arctic surface was cooling, a gradually increasing trend in the critical frequency of the F2 layer, foF2, was observed in the Tromsø ionosonde data with a rate of 0.022 ± 0.011 MHz/year. This can be explained by the Earth's atmosphere global energy balance. As for the trend of foF2 since 2001, there is a clear decrease with a rate of -0.046 ± 0.007 MHz/year. These trends are qualitatively consistent with the changes in the upper atmosphere that can be inferred from the cooling and warming of the Arctic surface. Studying these changes is important for understanding the coupling of the whole atmosphere. Further studies will require verification of the plausible scenario using global models.
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Variations in the Arctic upper atmosphere since the early 20th century: Relation to Arctic surface warming and cooling | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Research Article Variations in the Arctic upper atmosphere since the early 20th century: Relation to Arctic surface warming and cooling Yasunobu Ogawa, Magnar G. Johnsen, Njål Gulbrandsen, Andrea D. Løkke, and 2 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-5945142/v1 This work is licensed under a CC BY 4.0 License Status: Posted Version 1 posted You are reading this latest preprint version Abstract We have studied long-term ionospheric variations using data from the Tromsø ionosonde since 1932. To investigate Arctic ionospheric variations in relation to the Arctic warming and cooling before the 1970s, we have developed a Tromsø ionosonde database that makes it possible to study the daily variations over about 90 years. During the 1940s to 1960s, when the Arctic surface was cooling, a gradually increasing trend in the critical frequency of the F2 layer, foF2, was observed in the Tromsø ionosonde data with a rate of 0.022 ± 0.011 MHz/year. This can be explained by the Earth's atmosphere global energy balance. As for the trend of foF2 since 2001, there is a clear decrease with a rate of -0.046 ± 0.007 MHz/year. These trends are qualitatively consistent with the changes in the upper atmosphere that can be inferred from the cooling and warming of the Arctic surface. Studying these changes is important for understanding the coupling of the whole atmosphere. Further studies will require verification of the plausible scenario using global models. Full Text Supplementary Files EPStromsoionosondegraphicalabstractv15s3.png Cite Share Download PDF Status: Posted Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. 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