The anomalous ionosphere between solar cycles 23 and 24
The solar minimum period during 2008–2009 was characterized by lower thermospheric density than the previous solar minimum and lower than any previously measured. Recent work used the NCAR Thermosphere‐Ionosphere‐Electrodynamics General Circulation Model to show that the primary cause of density cha...
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Veröffentlicht in: | Journal of geophysical research. Space physics 2013-10, Vol.118 (10), p.6524-6535 |
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description | The solar minimum period during 2008–2009 was characterized by lower thermospheric density than the previous solar minimum and lower than any previously measured. Recent work used the NCAR Thermosphere‐Ionosphere‐Electrodynamics General Circulation Model to show that the primary cause of density changes from 1996 to 2008 was a small reduction in solar extreme ultraviolet (EUV) irradiance, causing a decrease in thermospheric temperature and hence a contracted thermosphere. There are similar effects in the ionosphere, with most measurements showing an F region ionosphere that is unusually low in density, and in peak altitude. This paper addresses the question of whether model simulations previously conducted, and their solar, geomagnetic, and anthropogenic inputs, produce ionospheric changes commensurate with observations. We conducted a 15 year model run and obtained good agreement with observations of the global mean thermospheric density at 400 km throughout the solar cycle, with a reduction of ~30% from the 1996 solar minimum to 2008–2009. We then compared ionosonde measurements of the midday peak density of the ionospheric F region (NmF2) to the model simulations at various locations. Reasonable agreement was obtained between measurements and the model, supporting the validity of the neutral density comparisons. The global average NmF2 was estimated to have declined between the two solar minima by ~15%. In these simulations, a 10% reduction of solar EUV plays the largest role in causing the ionospheric change, with a minor contribution from lower geomagnetic activity and a very small additional effect from anthropogenic increase in CO2.
Key Points
The ionosphere and thermosphere were anomalously low in density during 2008‐2009
Model simulations comparing 2008‐2009 to 1996 generally agree with observations
The primary cause was lower solar EUV irradiance than the previous solar minimum |
doi_str_mv | 10.1002/jgra.50561 |
format | Article |
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Key Points
The ionosphere and thermosphere were anomalously low in density during 2008‐2009
Model simulations comparing 2008‐2009 to 1996 generally agree with observations
The primary cause was lower solar EUV irradiance than the previous solar minimum</description><identifier>ISSN: 2169-9380</identifier><identifier>EISSN: 2169-9402</identifier><identifier>DOI: 10.1002/jgra.50561</identifier><language>eng</language><publisher>Hoboken, NJ: Blackwell Publishing Ltd</publisher><subject>Anthropogenic factors ; Astronomy ; Carbon dioxide ; climate ; Climate change ; Clouds ; Computer simulation ; Density ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; F region ; Interplanetary space ; Ionosphere ; Ionospherics ; Irradiance ; Physics of the ionosphere ; Physics of the magnetosphere ; Reduction ; solar ; Solar cycle ; Solar cycles ; Solar system ; thermosphere ; ultraviolet</subject><ispartof>Journal of geophysical research. Space physics, 2013-10, Vol.118 (10), p.6524-6535</ispartof><rights>2013. American Geophysical Union. All Rights Reserved.</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4711-22ab9aceb075d027c7c1cda40cd51959de662d4d6062b115b4abe8f4386ce3fe3</citedby><cites>FETCH-LOGICAL-c4711-22ab9aceb075d027c7c1cda40cd51959de662d4d6062b115b4abe8f4386ce3fe3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjgra.50561$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjgra.50561$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,27924,27925,45574,45575,46409,46833</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27977783$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Solomon, Stanley C.</creatorcontrib><creatorcontrib>Qian, Liying</creatorcontrib><creatorcontrib>Burns, Alan G.</creatorcontrib><title>The anomalous ionosphere between solar cycles 23 and 24</title><title>Journal of geophysical research. Space physics</title><addtitle>J. Geophys. Res. Space Physics</addtitle><description>The solar minimum period during 2008–2009 was characterized by lower thermospheric density than the previous solar minimum and lower than any previously measured. Recent work used the NCAR Thermosphere‐Ionosphere‐Electrodynamics General Circulation Model to show that the primary cause of density changes from 1996 to 2008 was a small reduction in solar extreme ultraviolet (EUV) irradiance, causing a decrease in thermospheric temperature and hence a contracted thermosphere. There are similar effects in the ionosphere, with most measurements showing an F region ionosphere that is unusually low in density, and in peak altitude. This paper addresses the question of whether model simulations previously conducted, and their solar, geomagnetic, and anthropogenic inputs, produce ionospheric changes commensurate with observations. We conducted a 15 year model run and obtained good agreement with observations of the global mean thermospheric density at 400 km throughout the solar cycle, with a reduction of ~30% from the 1996 solar minimum to 2008–2009. We then compared ionosonde measurements of the midday peak density of the ionospheric F region (NmF2) to the model simulations at various locations. Reasonable agreement was obtained between measurements and the model, supporting the validity of the neutral density comparisons. The global average NmF2 was estimated to have declined between the two solar minima by ~15%. In these simulations, a 10% reduction of solar EUV plays the largest role in causing the ionospheric change, with a minor contribution from lower geomagnetic activity and a very small additional effect from anthropogenic increase in CO2.
Key Points
The ionosphere and thermosphere were anomalously low in density during 2008‐2009
Model simulations comparing 2008‐2009 to 1996 generally agree with observations
The primary cause was lower solar EUV irradiance than the previous solar minimum</description><subject>Anthropogenic factors</subject><subject>Astronomy</subject><subject>Carbon dioxide</subject><subject>climate</subject><subject>Climate change</subject><subject>Clouds</subject><subject>Computer simulation</subject><subject>Density</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>F region</subject><subject>Interplanetary space</subject><subject>Ionosphere</subject><subject>Ionospherics</subject><subject>Irradiance</subject><subject>Physics of the ionosphere</subject><subject>Physics of the magnetosphere</subject><subject>Reduction</subject><subject>solar</subject><subject>Solar cycle</subject><subject>Solar cycles</subject><subject>Solar system</subject><subject>thermosphere</subject><subject>ultraviolet</subject><issn>2169-9380</issn><issn>2169-9402</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqNkNFKwzAUhosoKNMbn6AgggjVnKRJ2ss5depkiihehjQ9dZ1dO5ONubc3s3MXXoi5SQjf_3HOHwSHQM6AEHo-frP6jBMuYCvYoyDSKI0J3f55s4TsBgfOjYk_if8CvhfI5xGGum4mumrmLiybunHTEVoMM5wtEOvQNZW2oVmaCl1ImYfzkMb7wU6hK4cH67sTvFxfPfduovuH_m2vex-ZWAJElOos1QYzInlOqDTSgMl1TEzOIeVpjkLQPM4FETQD4FmsM0yKmCXCICuQdYKT1ju1zccc3UxNSmewqnSNfmAFQoIAmgr-DxRA0CQW0qNHv9BxM7e1X8RTLKGSMroSnraUsY1zFgs1teVE26UColaNq1Xj6rtxDx-vldoZXRVW16Z0mwSVqZQyYZ6DlluUFS7_MKq7_lP3xx21mdLN8HOT0fZd-WUkV6_Dvhokr4On4cWlemRfhx2cLg</recordid><startdate>201310</startdate><enddate>201310</enddate><creator>Solomon, Stanley C.</creator><creator>Qian, Liying</creator><creator>Burns, Alan G.</creator><general>Blackwell Publishing Ltd</general><general>Wiley</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>H8D</scope><scope>KL.</scope><scope>L7M</scope></search><sort><creationdate>201310</creationdate><title>The anomalous ionosphere between solar cycles 23 and 24</title><author>Solomon, Stanley C. ; Qian, Liying ; Burns, Alan G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4711-22ab9aceb075d027c7c1cda40cd51959de662d4d6062b115b4abe8f4386ce3fe3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Anthropogenic factors</topic><topic>Astronomy</topic><topic>Carbon dioxide</topic><topic>climate</topic><topic>Climate change</topic><topic>Clouds</topic><topic>Computer simulation</topic><topic>Density</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>F region</topic><topic>Interplanetary space</topic><topic>Ionosphere</topic><topic>Ionospherics</topic><topic>Irradiance</topic><topic>Physics of the ionosphere</topic><topic>Physics of the magnetosphere</topic><topic>Reduction</topic><topic>solar</topic><topic>Solar cycle</topic><topic>Solar cycles</topic><topic>Solar system</topic><topic>thermosphere</topic><topic>ultraviolet</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Solomon, Stanley C.</creatorcontrib><creatorcontrib>Qian, Liying</creatorcontrib><creatorcontrib>Burns, Alan G.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Journal of geophysical research. Space physics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Solomon, Stanley C.</au><au>Qian, Liying</au><au>Burns, Alan G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The anomalous ionosphere between solar cycles 23 and 24</atitle><jtitle>Journal of geophysical research. Space physics</jtitle><addtitle>J. Geophys. Res. Space Physics</addtitle><date>2013-10</date><risdate>2013</risdate><volume>118</volume><issue>10</issue><spage>6524</spage><epage>6535</epage><pages>6524-6535</pages><issn>2169-9380</issn><eissn>2169-9402</eissn><abstract>The solar minimum period during 2008–2009 was characterized by lower thermospheric density than the previous solar minimum and lower than any previously measured. Recent work used the NCAR Thermosphere‐Ionosphere‐Electrodynamics General Circulation Model to show that the primary cause of density changes from 1996 to 2008 was a small reduction in solar extreme ultraviolet (EUV) irradiance, causing a decrease in thermospheric temperature and hence a contracted thermosphere. There are similar effects in the ionosphere, with most measurements showing an F region ionosphere that is unusually low in density, and in peak altitude. This paper addresses the question of whether model simulations previously conducted, and their solar, geomagnetic, and anthropogenic inputs, produce ionospheric changes commensurate with observations. We conducted a 15 year model run and obtained good agreement with observations of the global mean thermospheric density at 400 km throughout the solar cycle, with a reduction of ~30% from the 1996 solar minimum to 2008–2009. We then compared ionosonde measurements of the midday peak density of the ionospheric F region (NmF2) to the model simulations at various locations. Reasonable agreement was obtained between measurements and the model, supporting the validity of the neutral density comparisons. The global average NmF2 was estimated to have declined between the two solar minima by ~15%. In these simulations, a 10% reduction of solar EUV plays the largest role in causing the ionospheric change, with a minor contribution from lower geomagnetic activity and a very small additional effect from anthropogenic increase in CO2.
Key Points
The ionosphere and thermosphere were anomalously low in density during 2008‐2009
Model simulations comparing 2008‐2009 to 1996 generally agree with observations
The primary cause was lower solar EUV irradiance than the previous solar minimum</abstract><cop>Hoboken, NJ</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/jgra.50561</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Anthropogenic factors Astronomy Carbon dioxide climate Climate change Clouds Computer simulation Density Earth, ocean, space Exact sciences and technology External geophysics F region Interplanetary space Ionosphere Ionospherics Irradiance Physics of the ionosphere Physics of the magnetosphere Reduction solar Solar cycle Solar cycles Solar system thermosphere ultraviolet |
title | The anomalous ionosphere between solar cycles 23 and 24 |
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