Seasonal dependence of MSTIDs obtained from 630.0 nm airglow imaging at Arecibo
All‐sky imaging data of 630.0 nm airglow emissions are used to study the seasonal and solar activity dependence of medium‐scale traveling ionospheric disturbances (MSTIDs) over Arecibo, Puerto Rico (18.3° N, 66.7° W, 28° N mag lat). MSTIDs are typical F‐region signatures at midlatitudes, yet limited...
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description | All‐sky imaging data of 630.0 nm airglow emissions are used to study the seasonal and solar activity dependence of medium‐scale traveling ionospheric disturbances (MSTIDs) over Arecibo, Puerto Rico (18.3° N, 66.7° W, 28° N mag lat). MSTIDs are typical F‐region signatures at midlatitudes, yet limited statistical results in the American sector hindered the progress in our understanding of these dynamical structures. This study compiles data from 2002 to 2007 and shows for the first time that optically‐determined MSTIDs at Arecibo present a semiannual pattern with peak occurrence at both solstices. In the Japanese longitude sector, a similar pattern has been found, but one with a main peak during local summer. This paper explains the high occurrence rate during local winter at Arecibo via E‐layer/F‐layer coupling and inter‐hemispheric coupling, thus accounting for a consistent morphology between the two longitude sectors. |
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MSTIDs are typical F‐region signatures at midlatitudes, yet limited statistical results in the American sector hindered the progress in our understanding of these dynamical structures. This study compiles data from 2002 to 2007 and shows for the first time that optically‐determined MSTIDs at Arecibo present a semiannual pattern with peak occurrence at both solstices. In the Japanese longitude sector, a similar pattern has been found, but one with a main peak during local summer. This paper explains the high occurrence rate during local winter at Arecibo via E‐layer/F‐layer coupling and inter‐hemispheric coupling, thus accounting for a consistent morphology between the two longitude sectors.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2010GL043569</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>6300 airglow ; Accounting ; Airglow ; all-sky imager ; Atmospheric sciences ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; F region ; Imaging ; Joining ; Longitude ; MSTIDs ; Solar activity ; Winter</subject><ispartof>Geophysical research letters, 2010-06, Vol.37 (11), p.n/a</ispartof><rights>Copyright 2010 by the American Geophysical Union.</rights><rights>2015 INIST-CNRS</rights><rights>Copyright 2010 by American Geophysical Union</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c5470-729253c197adbb932b15b13e916bf77187d26546b6e1b2cef087b3f2171ea403</citedby><cites>FETCH-LOGICAL-c5470-729253c197adbb932b15b13e916bf77187d26546b6e1b2cef087b3f2171ea403</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2010GL043569$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2010GL043569$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,11513,27923,27924,45573,45574,46408,46467,46832,46891</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=23032556$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Martinis, C.</creatorcontrib><creatorcontrib>Baumgardner, J.</creatorcontrib><creatorcontrib>Wroten, J.</creatorcontrib><creatorcontrib>Mendillo, M.</creatorcontrib><title>Seasonal dependence of MSTIDs obtained from 630.0 nm airglow imaging at Arecibo</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>All‐sky imaging data of 630.0 nm airglow emissions are used to study the seasonal and solar activity dependence of medium‐scale traveling ionospheric disturbances (MSTIDs) over Arecibo, Puerto Rico (18.3° N, 66.7° W, 28° N mag lat). MSTIDs are typical F‐region signatures at midlatitudes, yet limited statistical results in the American sector hindered the progress in our understanding of these dynamical structures. This study compiles data from 2002 to 2007 and shows for the first time that optically‐determined MSTIDs at Arecibo present a semiannual pattern with peak occurrence at both solstices. In the Japanese longitude sector, a similar pattern has been found, but one with a main peak during local summer. This paper explains the high occurrence rate during local winter at Arecibo via E‐layer/F‐layer coupling and inter‐hemispheric coupling, thus accounting for a consistent morphology between the two longitude sectors.</description><subject>6300 airglow</subject><subject>Accounting</subject><subject>Airglow</subject><subject>all-sky imager</subject><subject>Atmospheric sciences</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>F region</subject><subject>Imaging</subject><subject>Joining</subject><subject>Longitude</subject><subject>MSTIDs</subject><subject>Solar activity</subject><subject>Winter</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp9kU1vEzEURS0EEqGw4wdYSAgWnfL8MXa8rAJMC4FKNFKXlu15E7lMxsFOVPrv6ypVhVh05bc491o6l5C3DE4YcPOJA4NuCVK0yjwjM2akbOYA-jmZAZh6c61eklelXAOAAMFm5OISXUmTG2mPW5x6nALSNNAfl6vzz4Umv3Nxwp4OOW2oEnACdNpQF_N6TDc0btw6TmvqdvQ0Y4g-vSYvBjcWfPPwHpHV1y-rxVmzvOjOF6fLJrRSQ6O54a0IzGjXe28E96z1TKBhyg9as7nuuWql8gqZ5wEHmGsvBs40QydBHJEPh9ptTn_2WHZ2E0vAcXQTpn2xWtZfFOOmkh-fJJkW1RBnUlT03X_oddrn6qb2qQoYZeYVOj5AIadSMg52m6uGfGsZ2PsV7L8rVPz9Q6crwY1DdlOI5THD6wq8bVXl-IG7iSPePtlpu19Lrpm4t9AcQrHs8O9jyOXfVmmhW3v1s7Nw1nH5bXFlv4s7YI2f7A</recordid><startdate>201006</startdate><enddate>201006</enddate><creator>Martinis, C.</creator><creator>Baumgardner, J.</creator><creator>Wroten, J.</creator><creator>Mendillo, M.</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><general>John Wiley & Sons, Inc</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7SM</scope><scope>7SU</scope><scope>C1K</scope></search><sort><creationdate>201006</creationdate><title>Seasonal dependence of MSTIDs obtained from 630.0 nm airglow imaging at Arecibo</title><author>Martinis, C. ; 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Res. Lett</addtitle><date>2010-06</date><risdate>2010</risdate><volume>37</volume><issue>11</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>All‐sky imaging data of 630.0 nm airglow emissions are used to study the seasonal and solar activity dependence of medium‐scale traveling ionospheric disturbances (MSTIDs) over Arecibo, Puerto Rico (18.3° N, 66.7° W, 28° N mag lat). MSTIDs are typical F‐region signatures at midlatitudes, yet limited statistical results in the American sector hindered the progress in our understanding of these dynamical structures. This study compiles data from 2002 to 2007 and shows for the first time that optically‐determined MSTIDs at Arecibo present a semiannual pattern with peak occurrence at both solstices. In the Japanese longitude sector, a similar pattern has been found, but one with a main peak during local summer. This paper explains the high occurrence rate during local winter at Arecibo via E‐layer/F‐layer coupling and inter‐hemispheric coupling, thus accounting for a consistent morphology between the two longitude sectors.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2010GL043569</doi><tpages>5</tpages></addata></record> |
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subjects | 6300 airglow Accounting Airglow all-sky imager Atmospheric sciences Earth sciences Earth, ocean, space Exact sciences and technology F region Imaging Joining Longitude MSTIDs Solar activity Winter |
title | Seasonal dependence of MSTIDs obtained from 630.0 nm airglow imaging at Arecibo |
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