Comparison of the tidal signatures in sporadic E and vertical ion convergence rate, using FORMOSAT-3/COSMIC radio occultation observations and GAIA model

• 資料種別: 記事
• タイトル: Comparison of the tidal signatures in sporadic E and vertical ion convergence rate, using FORMOSAT-3/COSMIC radio occultation observations and GAIA model
• 著者・編者: Sahar Sobhkhiz-Miandehi; Yosuke Yamazaki; Christina Arras
• 出版事項: 日本 : The Society of Geomagnetism and Earth, Planetary and Space Sciences
• 出版年月日等: 2022-06-07
• 出版年（W3CDTF）: 2022-06-07
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 74(88)
• 掲載巻: 74(88)
• ISSN（掲載誌）: 1880-5981
• ISSN-L（掲載誌）: 1343-8832
• 本文の言語コード: eng
• DOI: 10.1186/s40623-022-01637-y; https://doi.org/10.1186/s40623-022-01637-y
• 国立国会図書館永続的識別子: info:ndljp/pid/12685375; https://dl.ndl.go.jp/pid/12685375
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• コレクション（個別）: 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2023-03-07T16:17:01+09:00
• 保存日（W3CDTF）: 2023-03-07
• 記録形式（IMT）: application/pdf
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• デジタル化資料送信: 図書館・個人送信対象外
• 遠隔複写可否（NDL）: 可
• 掲載誌（URI）: https://earth-planets-space.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/12287068; https://dl.ndl.go.jp/pid/12287068
• 連携機関・データベース: 国立国会図書館 : 国立国会図書館デジタルコレクション; https://dl.ndl.go.jp

• 要約等: コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
• DOI: 10.1186/s40623-022-01637-y; https://doi.org/10.1186/s40623-022-01637-y; 10.21203/rs.3.rs-1029914/v1; https://doi.org/10.21203/rs.3.rs-1029914/v1; 10.5194/egusphere-egu22-1942; https://doi.org/10.5194/egusphere-egu22-1942
• オンライン閲覧公開範囲: インターネット公開
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/12685375; https://dl.ndl.go.jp/pid/12685375; https://link.springer.com/content/pdf/10.1186/s40623-022-01637-y.pdf; https://link.springer.com/article/10.1186/s40623-022-01637-y/fulltext.html
• 参照: Special issue “DynamicEarth: Earth’s interior, surface, ocean, atmosphere, and near space interactions”; https://cir.nii.ac.jp/crid/1360302866841182336; Numerical Simulations of Metallic Ion Density Perturbations in Sporadic E Layers Caused by Gravity Waves; https://cir.nii.ac.jp/crid/1360865815487031040
• 参照: Global distribution of neutral wind shear associated with sporadic <i>E</i> layers derived from GAIA; https://cir.nii.ac.jp/crid/1360004229806302976; Midlatitude Sporadic E. A Typical Paradigm of Atmosphere-Ionosphere Coupling; https://cir.nii.ac.jp/crid/1360011146046574720; Estimation of ionospheric sporadic E intensities from GPS radio occultation measurements; https://cir.nii.ac.jp/crid/1360013172134717312; The seasonal distribution of sporadic E layers observed from radio occultation measurements and its relation with wind shear measured by TIMED/TIDI; https://cir.nii.ac.jp/crid/1360013172248978304; Terdiurnal tidelike variability in sporadic <i>E</i> layers; https://cir.nii.ac.jp/crid/1360016868435634944; Quarterdiurnal signature in sporadic E occurrence rates and comparison with neutral wind shear; https://cir.nii.ac.jp/crid/1360016868473907584; Lunar Tides in the Ionosphere; https://cir.nii.ac.jp/crid/1360017286213562624; The complete spectrum of the equatorial electrojet related to solar tides: CHAMP observations; https://cir.nii.ac.jp/crid/1360017287613967872; ENSO effects on MLT diurnal tides: A 21 year reanalysis data‐driven GAIA model simulation; https://cir.nii.ac.jp/crid/1360285704784839424; Examining the Wind Shear Theory of Sporadic E With ICON/MIGHTI Winds and COSMIC‐2 Radio Occultation Data; https://cir.nii.ac.jp/crid/1360294643820385280; The Wind‐Shear Theory of Temperate Zone Sporadic <i>E</i>; https://cir.nii.ac.jp/crid/1360294646998628096; Comparison of global morphologies of vertical ion convergence and sporadic E occurrence rate; https://cir.nii.ac.jp/crid/1360294647815345664; A study of tidal and planetary wave periodicities present in midlatitude sporadic <i>E</i> layers; https://cir.nii.ac.jp/crid/1360298760753981568; Vertical connection from the tropospheric activities to the ionospheric longitudinal structure simulated by a new Earth's whole atmosphere-ionosphere coupled model; https://cir.nii.ac.jp/crid/1360565166661744640; Sporadic <i>E</i> morphology from GPS‐CHAMP radio occultation; https://cir.nii.ac.jp/crid/1360574093934154624; Seasonal variability and descent of mid-latitude sporadic E layers at Arecibo; https://cir.nii.ac.jp/crid/1360574095881122816; Sporadic E tidal variabilities and characteristics observed with the Cyprus Digisonde; https://cir.nii.ac.jp/crid/1360576122141011584; Wavenumber‐4 Patterns of the Sporadic E Over the Middle‐ and Low‐Latitudes; https://cir.nii.ac.jp/crid/1360580234808147328; Lunar effects on the equatorial Es; https://cir.nii.ac.jp/crid/1360580236596491264; Terdiurnal signatures in sporadic &lt;i&gt;E&lt;/i&gt; layers at midlatitudes; https://cir.nii.ac.jp/crid/1360580236598479744; Lunar Tidal Variations of Sporadic E; https://cir.nii.ac.jp/crid/1360861711219885440; Evidence for planetary wave effects on midlatitude backscatter and sporadic <i>E</i> layer occurrence; https://cir.nii.ac.jp/crid/1360861711220409344; Planetary waves and midlatitude sporadic <i>E</i> layers: Strong experimental evidence for a close relationship; https://cir.nii.ac.jp/crid/1360861711220410624; The lunar tide in sporadic E; https://cir.nii.ac.jp/crid/1360861713078823808; The Lunar Tide in ƒ_<i>b</i><i>E</i>_s; https://cir.nii.ac.jp/crid/1360861714464364544; Lunar Influences on Sporadic <i>E</i>; https://cir.nii.ac.jp/crid/1360861714464365312; Evidence of a role for modulated atmospheric tides in the dependence of sporadic <i>E</i> layers on planetary waves; https://cir.nii.ac.jp/crid/1361137046531424128; Semidiurnal tidal signature in sporadic E occurrence rates derived from GPS radio occultation measurements at higher midlatitudes; https://cir.nii.ac.jp/crid/1361699994195932160; Recent work on mid-latitude and equatorial sporadic-E; https://cir.nii.ac.jp/crid/1361699995643516928; Tidal variability in the ionospheric dynamo region; https://cir.nii.ac.jp/crid/1361699996068119168; International Geomagnetic Reference Field: the eleventh generation; https://cir.nii.ac.jp/crid/1361981468504417024; A global climatology of ionospheric irregularities derived from GPS radio occultation; https://cir.nii.ac.jp/crid/1361981469597358208; Sporadic E: current views and recent progress; https://cir.nii.ac.jp/crid/1361981470151609984; An explanation for the seasonal dependence of midlatitude sporadic <i>E</i> layers; https://cir.nii.ac.jp/crid/1361981470997923456; Upper atmosphere tides and the vertical motion of ionospheric sporadic layers at Arecibo; https://cir.nii.ac.jp/crid/1361981471422727424; DWM07 global empirical model of upper thermospheric storm‐induced disturbance winds; https://cir.nii.ac.jp/crid/1362544419059298816; Production and prediction of sporadic <i>E</i>; https://cir.nii.ac.jp/crid/1362544419061904768; Global sounding of sporadic E layers by the GPS/MET radio occultation experiment; https://cir.nii.ac.jp/crid/1362544420797762560; Explanation of the sporadic‐<i>E</i> layer formation by comparing FORMOSAT‐3/COSMIC data with meteor and wind shear information; https://cir.nii.ac.jp/crid/1363388844842194944; Morphology of sporadic <i>E</i> layer retrieved from COSMIC GPS radio occultation measurements: Wind shear theory examination; https://cir.nii.ac.jp/crid/1363670319639035776; A Tutorial Review on Sporadic E Layers; https://cir.nii.ac.jp/crid/1363951793810260992; The formation of the sporadic-E layer in the temperate zones; https://cir.nii.ac.jp/crid/1363951795536116992; Sporadic &lt;i&gt;E&lt;/i&gt; signatures revealed from multi-satellite radio occultation measurements; https://cir.nii.ac.jp/crid/1363951795702966528; Excitation mechanism of non-migrating tides; https://cir.nii.ac.jp/crid/1364233269664832896; Semi-Diurnal Lunar Variations in the Sporadic-E; https://cir.nii.ac.jp/crid/1390001206509497728; First simulations of day-to-day variability of mid-latitude sporadic E layer structures; https://cir.nii.ac.jp/crid/2051433317028469504; Global distribution of the migrating terdiurnal tide seen in sporadic E occurrence frequencies obtained from GPS radio occultations; https://cir.nii.ac.jp/crid/2051996267023641984
• 参照（URI）: https://cir.nii.ac.jp/crid/1370017279854174985; https://cir.nii.ac.jp/crid/1370017279854174994
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 12685375; http://id.ndl.go.jp/bib/12685375