Relationship between day-to-day variability of equatorial plasma bubble activity from GPS scintillation and atmospheric properties from Ground-to-topside model of Atmosphere and Ionosphere for Aeronomy (GAIA) assimilation

• Material Type: 記事
• Title: Relationship between day-to-day variability of equatorial plasma bubble activity from GPS scintillation and atmospheric properties from Ground-to-topside model of Atmosphere and Ionosphere for Aeronomy (GAIA) assimilation
• Author/Editor: Mamoru Yamamoto; Yuichi Otsuka; Hidekatsu Jin
• Publication, Distribution, etc.: 日本 : Springer Nature
• Publication Date: 2018-05-02
• Publication Date (W3CDTF): 2018-05-02
• Periodical title: Progress in earth and planetary science
• No. or year of volume/issue: 5(26)
• Volume: 5(26)
• ISSN (Periodical Title): 2197-4284
• ISSN-L (Periodical Title): 2197-4284
• Text Language Code: eng
• DOI: 10.1186/s40645-018-0184-7; https://doi.org/10.1186/s40645-018-0184-7
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• Date Accepted (W3CDTF): 2018-08-13T20:13:35+09:00
• Date Captured (W3CDTF): 2018-08-13
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• Periodical Title (URI): https://progearthplanetsci.springeropen.com/articles
• Periodical Title (Persistent ID (NDL)): info:ndljp/pid/11018906; https://dl.ndl.go.jp/pid/11018906
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• Summary, etc.: The relationship between day-to-day variability of equatorial plasma bubbles (EPBs) and the neutral atmosphere is studied. This study is based on the previous study in which the GPS scintillation index and the tropospheric cloud-top temperature are used as proxies for EPB activity and atmospheric perturbations, respectively, and a correlation was found between their day-to-day variations. In this paper, we maintained the same GPS scintillation data but substituted the atmospheric data via an assimilation run of the Ground-to-topside model of Atmosphere and Ionosphere for Aeronomy (GAIA). Cross-correlation between the EPB activity and the atmospheric temperature is similar to the results in Ogawa et al. (Earth Planets Space 61:397–410, 2009). The new findings from our study include (1) an enhanced correlation between the EPB activity and the neutral atmosphere is found in horizontally and vertically large areas, (2) the longitudinal disturbance of atmospheric temperature and wind velocity during the EPB-active days is enhanced, and (3) the enhancement of atmospheric disturbance during the EPB-active days shows a similarity to the characteristics of large-scale wave structures in the ionosphere. These results more clearly support couplings between EPBs and the neutral atmosphere.
• DOI: 10.1186/s40645-018-0184-7; https://doi.org/10.1186/s40645-018-0184-7
• Access Restrictions: インターネット公開
• Rights (production): © The Author(s). 2018. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
• Related Material (URI): http://hdl.handle.net/2433/234564; http://id.ndl.go.jp/digimeta/11126148; https://dl.ndl.go.jp/pid/11126148; http://link.springer.com/content/pdf/10.1186/s40645-018-0184-7.pdf; http://link.springer.com/article/10.1186/s40645-018-0184-7/fulltext.html
• Is Referenced By: Challenges to Equatorial Plasma Bubble and Ionospheric Scintillation Short-Term Forecasting and Future Aspects in East and Southeast Asia; https://cir.nii.ac.jp/crid/1360298757412383488
• References: On the application of differential phase measurements to study the zonal large scale wave structure (LSWS) in the ionospheric electron content; https://cir.nii.ac.jp/crid/1050282810705997952; Control of the seasonal and longitudinal occurrence of equatorial scintillations by the longitudinal gradient in integrated <i>E</i> region Pedersen conductivity; https://cir.nii.ac.jp/crid/1360001114027745408; Characteristics of large‐scale wave structure observed from African and Southeast Asian longitudinal sectors; https://cir.nii.ac.jp/crid/1360002214348512384; The neutral dynamics during the 2009 sudden stratosphere warming simulated by different whole atmosphere models; https://cir.nii.ac.jp/crid/1360004229800655360; First observations of large‐scale wave structure and equatorial spread F using CERTO radio beacon on the C/NOFS satellite; https://cir.nii.ac.jp/crid/1360282588962526080; Gravity wave initiation of equatorial spread F/plasma bubble irregularities based on observational data from the SpreadFEx campaign; https://cir.nii.ac.jp/crid/1360292620413432448; Enhanced ionospheric plasma bubble generation in more active ITCZ; https://cir.nii.ac.jp/crid/1360565164303828096; 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; On the enigma of day‐to‐day variability in equatorial spread <i>F</i>; https://cir.nii.ac.jp/crid/1360574093448180096; Spread F – an old equatorial aeronomy problem finally resolved?; https://cir.nii.ac.jp/crid/1360574096291054592; Thermal and dynamical changes of the zonal mean state of the thermosphere during the 2009 SSW: GAIA simulations; https://cir.nii.ac.jp/crid/1360848654732352640; Medium‐scale gravity wave activity in the bottomside <i>F</i> region in tropical regions; https://cir.nii.ac.jp/crid/1360848654737944064; Equatorial GPS ionospheric scintillations over Kototabang, Indonesia and their relation to atmospheric waves from below; https://cir.nii.ac.jp/crid/1362262946037419648; Relationship of the onset of equatorial <i>F</i> region irregularities with the sunset terminator observed with the Equatorial Atmosphere Radar; https://cir.nii.ac.jp/crid/1363107369120239104; Gravity wave and tidal influences on equatorial spread F based on observations during the Spread F Experiment (SpreadFEx); https://cir.nii.ac.jp/crid/1363107370945442944; Longitudinal variability of annual changes in activity of equatorial spread <i>F</i> and plasma bubbles; https://cir.nii.ac.jp/crid/1363670320158469888; Equatorial spread F/plasma bubble irregularities under storm time disturbance electric fields; https://cir.nii.ac.jp/crid/1363951794926925440; The influence of burn severity on postfire vegetation recovery and albedo change during early succession in North American boreal forests; https://cir.nii.ac.jp/crid/1363951795516027264; Ionospheric Disturbances Over Indonesia and Their Possible Association With Atmospheric Gravity Waves From the Troposphere(<Special Issue>CPEA-Coupling Processes in the Equatorial Atmosphere); https://cir.nii.ac.jp/crid/1390282681479846528; Correlation between the global occurrences of ionospheric irregularities and deep atmospheric convective clouds in the intertropical convergence zone (ITCZ); https://cir.nii.ac.jp/crid/2050870367116811776; Upwelling : a unit of disturbance in equatorial spread F; https://cir.nii.ac.jp/crid/2051996267026445056
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• Bibliographic ID (NDL): 11126148; http://id.ndl.go.jp/bib/11126148
• NAID: 120006522879