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  1. H300 宇宙地球環境研究所
  2. H300a 雑誌掲載論文
  3. 学術雑誌

Sixteen year variation of horizontal phase velocity and propagation direction of mesospheric and thermospheric waves in airglow images at Shigaraki, Japan

http://hdl.handle.net/2237/27260
http://hdl.handle.net/2237/27260
6a40135c-ccf6-49c9-be8a-bff5124088d8
名前 / ファイル ライセンス アクション
Takeo_et_al-2017-Journal_of_Geophysical_Research_Space_Physics.pdf Takeo_et_al-2017-Journal_of_Geophysical_Research_Space_Physics.pdf ファイル公開日:2018/02/01 (4.3 MB)
アイテムタイプ 学術雑誌論文 / Journal Article(1)
公開日 2018-01-10
タイトル
タイトル Sixteen year variation of horizontal phase velocity and propagation direction of mesospheric and thermospheric waves in airglow images at Shigaraki, Japan
言語 en
著者 Takeo, D.

× Takeo, D.

WEKO 74699

en Takeo, D.

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Shiokawa, K.

× Shiokawa, K.

WEKO 74700

en Shiokawa, K.

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Fujinami, H.

× Fujinami, H.

WEKO 74701

en Fujinami, H.

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Otsuka, Y.

× Otsuka, Y.

WEKO 74702

en Otsuka, Y.

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Matsuda, TS.

× Matsuda, TS.

WEKO 74703

en Matsuda, TS.

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Ejiri, MK.

× Ejiri, MK.

WEKO 74704

en Ejiri, MK.

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Nakamura, T.

× Nakamura, T.

WEKO 74705

en Nakamura, T.

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Yamamoto, M.

× Yamamoto, M.

WEKO 74706

en Yamamoto, M.

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
権利情報 © 2017 American Geophysical Union
言語 en
抄録
内容記述タイプ Abstract
内容記述 We analyzed the horizontal phase velocity of gravity waves and medium-scale traveling ionospheric disturbances (MSTIDs) by using the three-dimensional fast Fourier transform method developed by Matsuda et al. (2014) for 557.7 nm (altitude: 90–100 km) and 630.0 nm (altitude: 200–300 km) airglow images obtained at Shigaraki MU Observatory (34.8°N, 136.1°E, dip angle: 49°) over ∼16 years from 16 March 1999 to 20 February 2015. The analysis of 557.7 nm airglow images shows clear seasonal variation of the propagation direction of gravity waves in the mesopause region. In spring, summer, fall, and winter, the peak directions are northeastward, northeastward, northwestward, and southwestward, respectively. The difference in east-west propagation direction between summer and winter is probably caused by the wind filtering effect due to the zonal mesospheric jet. Comparison with tropospheric reanalysis data shows that the difference in north-south propagation direction between summer and winter is caused by differences in the latitudinal location of wave sources due to convective activity in the troposphere relative to Shigaraki. The analysis of 630.0 nm airglow images shows that the propagation direction of MSTIDs is mainly southwestward with a minor northeastward component throughout the 16 years. A clear negative correlation is seen between the yearly power spectral density of MSTIDs and F10.7 solar flux. This negative correlation with solar activity may be explained by the linear growth rate of the Perkins instability and secondary wave generation of gravity waves in the thermosphere.
言語 en
出版者
出版者 American Geophysical Union
言語 en
言語
言語 eng
資源タイプ
資源タイプresource http://purl.org/coar/resource_type/c_6501
タイプ journal article
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 https://doi.org/10.1002/2017JA023919
ISSN
収録物識別子タイプ EISSN
収録物識別子 2169-9402
書誌情報 en : Journal of Geophysical Research-Space Physics

巻 122, 号 8, p. 8770-8780, 発行日 2017-08
著者版フラグ
値 publisher
URI
識別子 http://doi.org/10.1002/2017JA023919
識別子タイプ DOI
URI
識別子 http://hdl.handle.net/2237/27260
識別子タイプ HDL
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