ダウンロード数: 136

このアイテムのファイル:
ファイル 記述 サイズフォーマット 
angeo-34-543-2016.pdf6.61 MBAdobe PDF見る/開く
タイトル: Properties of inertia-gravity waves in the lowermost stratosphere as observed by the PANSY radar over Syowa Station in the Antarctic
著者: Mihalikova, Maria
Sato, Kaoru
Tsutsumi, Masaki
Sato, Toru  KAKEN_id  orcid https://orcid.org/0000-0002-2092-7335 (unconfirmed)
著者名の別形: 佐藤, 亨
発行日: 10-May-2016
出版者: European Geosciences Union (EGU)
誌名: Annales Geophysicae
巻: 34
号: 5
開始ページ: 543
終了ページ: 555
抄録: Inertia-gravity waves (IGWs) are an important component for the dynamics of the middle atmosphere. However, observational studies needed to constrain their forcing are still insufficient especially in the remote areas of the Antarctic region. One year of observational data (January to December 2013) by the PANSY radar of the wind components (vertical resolution of 150m and temporal resolution of 30 min) are used to derive statistical analysis of the properties of IGWs with short vertical wavelengths (≤4 km) and ground-based periods longer than 4 h in the lowermost stratosphere (height range 10 to 12 km) with the help of the hodograph method. The annual change of the IGWs parameters are inspected but no pronounced year cycle is found. The year is divided into two seasons (summer and winter) based on the most prominent difference in the ratio of Coriolis parameter (f ) to intrinsic frequency (ω) distribution. Average of f/ω for the winter season is 0.40 and for the summer season 0.45 and the average horizontal wavelengths are 140 and 160 km respectively. Vertical wavelengths have an average of 1.85 km through the year. For both seasons the properties of IGWs with upward and downward propagation of the energy are also derived and compared. The percentage of downward propagating waves is 10.7 and 18.4% in the summer and winter season respectively. This seasonal change is more than the one previously reported in the studies from mid-latitudes and model-based studies. It is in agreement with the findings of past radiosonde data-based studies from the Antarctic region. In addition, using the so-called dualbeam technique, vertical momentum flux and the variance of the horizontal perturbation velocities of IGWs are examined. Tropospheric disturbances of synoptic-scale are suggested as a source of episodes of IGWs with large variance of horizontal perturbation velocities, and this is shown in a number of cases.
著作権等: © Author(s) 2016. This work is distributed under the Creative Commons Attribution 3.0 License.
URI: http://hdl.handle.net/2433/216391
DOI(出版社版): 10.5194/angeo-34-543-2016
出現コレクション:学術雑誌掲載論文等

アイテムの詳細レコードを表示する

Export to RefWorks


出力フォーマット 


このリポジトリに保管されているアイテムはすべて著作権により保護されています。