WEKO3
アイテム
Diffusion coefficients derived from the Lagrangian statistics
https://doi.org/10.15094/00003559
https://doi.org/10.15094/00003559ad528e9a-a10d-42fa-8065-fb841d76e141
名前 / ファイル | ライセンス | アクション |
---|---|---|
KJ00000035525 (1.3 MB)
|
Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||||
---|---|---|---|---|---|---|---|---|
公開日 | 1989-08-01 | |||||||
タイトル | ||||||||
タイトル | Diffusion coefficients derived from the Lagrangian statistics | |||||||
言語 | ||||||||
言語 | eng | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.15094/00003559 | |||||||
ID登録タイプ | JaLC | |||||||
ページ属性 | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | P(論文) | |||||||
著者名(英) |
Yamazaki, Koji
× Yamazaki, Koji
|
|||||||
著者所属(英) | ||||||||
en | ||||||||
Meteorological Research Institute | ||||||||
抄録(英) | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | Diffusion coefficients are derived from trajectory analyses. Derived horizontal diffusivity in the lower stratosphere varies with season and confirmed the results obtained in YAMAZAKI (Proc. NIPR Symp. Polar Meteorol. Glaciol., 1,39,1987). Large horizontal diffusivity appears in the region of enhanced wave activity and/or weak zonal wind. The horizontal and vertical diffusivities in the troposphere are large in middle latitudes. The pattern and magnitude of derived diffusivity generally agree with the results of GFDL General Circulation/Transport Model by PLUMB and MAHLMAN (J. Atmos. Sci., 44,298,1987). Dispersion from the antarctic troposphere is very rapid and the residence time over Antarctica is about 3 days. | |||||||
雑誌書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AA10756213 | |||||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 2, p. 16-24, 発行日 1989-08 |
|||||||
出版者 | ||||||||
出版者 | National Institute of Polar Research |