Morphology and dynamics of daytime mid-latitude sporadic-E patches revealed by GPS total electron content observations in Japan
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DOI[10.1186/s40623-015-0257-4]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Jun MaedaKosuke Heki
- Publication, Distribution, etc.
- Publication Date
- 2015-06-11
- Publication Date (W3CDTF)
- 2015-06-11
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 67(89)
- Volume
- 67(89)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-015-0257-4
- Persistent ID (NDL)
- info:ndljp/pid/9497168
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2015-09-15T20:13:28+09:00
- Date Captured (W3CDTF)
- 2015-08-20
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/9227920
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Collection (particular)
- 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
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Holding library
- 国立国会図書館
- Call No.
- Z54-J298
- Related Material (URI)
- Related Material (Persistent ID (NDL))
- info:ndljp/pid/8968858
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館雑誌記事索引
- Bibliographic ID (NDL)
- 9497168
- Bibliographic Record Category (NDL)
- 632
- Summary, etc.
- Morphological characteristics of daytime mid-latitude sporadic-E (Es) patches are studied by two-dimensional total electron content (TEC) maps drawn using the Japanese dense network of Global Positioning System (GPS) receivers. By analyzing over 70 cases, we found that their horizontal shapes are characterized by frontal structure typically elongated in east-west by similar to 100 km. They are observed to migrate mainly northward in the morning and southward in the afternoon with speeds of 30-100 m/s. This may reflect the velocities of neutral winds controlled by the atmospheric tides. Such frontal structures are often found to include smaller scale structures.
- DOI
- 10.1186/s40623-015-0257-4
- Access Restrictions
- インターネット公開
- Rights (production)
- Creative Commons Attribution 4.0 International
- Related Material (URI)
- Is Referenced By
- Simulation of horizontal sporadic E layer movement driven by atmospheric tidesMw dependence of preseismic ionospheric electron enhancementsHigh‐Resolution 3‐D Imaging of Daytime Sporadic‐E Over Japan by Using GNSS TEC and IonosondesOn using a double-thin-shell approach and TEC perturbation component to sound night-time mid-latitude E–F couplingNighttime Midlatitude E‐F Coupling in Geomagnetic Conjugate Ionospheres: A Double Thin Shell Model and a Multi‐Source Data InvestigationAtmospheric modes excited by the 2021 August eruption of the Fukutoku-Okanoba volcano, Izu–Bonin Arc, observed as harmonic TEC oscillations by QZSSImaging the midlatitude sporadic <i>E</i> plasma patches with a coordinated observation of spaceborne InSAR and GPS total electron contentTemporal Evolution of Three‐Dimensional Structures of Metal Ion Layer Around Japan Simulated by a Midlatitude Ionospheric ModelThe Possible Role of Turbopause on Sporadic‐E Layer Formation at Middle and Low LatitudesThe Characteristics of Summer Descending Sporadic E Layer Observed With the Ionosondes in the China RegionNumerical Simulations of Metallic Ion Density Perturbations in Sporadic E Layers Caused by Gravity WavesA Statistical Study of Anomalous VHF Propagation Due to the Sporadic‐E Layer in the Air‐Navigation BandPropagation characteristics of sporadic E and medium-scale traveling ionospheric disturbances (MSTIDs) : statistics using HF Doppler and GPS-TEC data in Japan
- References
- Two-dimensional observations of midlatitude sporadic<i>E</i>irregularities with a dense GPS array in JapanA direction‐dependent instability of sporadic‐<i>E</i> layers in the nighttime midlatitude ionosphereCommon volume coherent and incoherent scatter radar observations of mid-latitude sporadic E-layers and QP echoesRadar observations of field-aligned plasma irregularities in the SEEK-2 campaignMidlatitude Sporadic E. A Typical Paradigm of Atmosphere-Ionosphere CouplingA possible mechanism for echo striation generation of radar backscatter from midlatitude sporadic <i>E</i>Horizontal structure of sporadic <i>E</i> layer observed with a rocket‐borne magnesium ion imagerDouble atmospheric gravity wave frequency oscillations of sporadic E formed in a horizontal shear flowIonospheric holes made by ballistic missiles from North Korea detected with a Japanese dense GPS arraySporadic <i>E</i> layer observations over Arecibo using coherent and incoherent scatter radar: Assessing dynamic stability in the lower thermosphereObservation of three‐dimensional structures of quasi‐periodic echoes associated with mid‐latitude sporadic‐E layers by MU radar ultra‐multi‐channel systemWinds and shears in the mesosphere and lower thermosphere: Results from four decades of chemical release wind measurementsObservations of quasi‐periodic scintillations and their possible relation to the dynamics of <i>E<sub>s</sub></i> plasma blobsSeek S310‐25: Quasi‐periodic echoes and polarization electric fieldsGravity wave modulation of gradient drift instabilities in mid‐latitude sporadic <i>E</i> irregularitiesSemidiurnal tidal signature in sporadic E occurrence rates derived from GPS radio occultation measurements at higher midlatitudesCoordinated sporadic E layer observations made with Chung-Li 30MHz radar, ionosonde and FORMOSAT-3/COSMIC satellitesShapes of irregularities in the sporadic <i>E</i> layer producing quasi‐periodic scintillationsRecent work on mid-latitude and equatorial sporadic-EMid‐latitude <i>E</i> region field‐aligned irregularities observed with the MU radarThe modulation of sporadic-E layers by Kelvin–Helmholtz billows in the neutral atmosphereA global climatology of ionospheric irregularities derived from GPS radio occultationSpatial structure of the <i>E</i> region field‐aligned irregularities revealed by the MU radarLarge winds and wind shears caused by the nonlinear interactions between gravity waves and tidal backgrounds in the mesosphere and lower thermosphereSky-wave backscatter observations of sporadic-E over JapanA study of winds between 80 and 100 km in medium latitudesThe SEEK Chemical Release Experiment: Observed neutral wind profile in a region of sporadic EA morphological study on mid-latitude E-region field-aligned irregularities observed with the MU radarFine structure in midlatitude sporadic E layers<i>E<sub>s</sub></i> structure using an HF radarImaging radar observations and theory of type I and type II quasi‐periodic echoesA shear instability seeding mechanism for quasiperiodic radar echoesHorizontal wind systems in the ionospheric E-region deduced from the dynamo theory of the geomagnetic Sq variation part IIHorizontal Wind Systems in the Ionospheric E Region Deduced from the Dynamo Theory of the Geomagnetic Sq Variation Part III
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 9497168
- NAID
- 120005625299