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| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
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完全メタデータレコード
| DCフィールド | 値 | 言語 |
|---|---|---|
| dc.contributor.author | Takemura, Kazushi | en |
| dc.contributor.author | Ishioka, Keiichi | en |
| dc.contributor.author | Shige, Shoichi | en |
| dc.contributor.alternative | 石岡, 圭一 | ja |
| dc.contributor.alternative | 重, 尚一 | ja |
| dc.date.accessioned | 2016-06-23T01:14:31Z | - |
| dc.date.available | 2016-06-23T01:14:31Z | - |
| dc.date.issued | 2016-01 | - |
| dc.identifier.issn | 1530-261X | - |
| dc.identifier.uri | http://hdl.handle.net/2433/215147 | - |
| dc.description.abstract | In a high-resolution atmospheric model, the terrain is resolved in detail, and thus steeper and more complex terrain can be represented. Thus, we developed an atmospheric model that represents the terrain by using the Chimera grid method, which represents the computational region as a composite of overlapping grids. To test this model, we simulated a lee wave over a semicircular mountain and one over a tall semi-elliptical mountain. The results show that the Chimera grid method can be used to represent a very steep terrain which terrain-following coordinates and numerically generated coordinates cannot represent appropriately. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | John Wiley and Sons Ltd. | en |
| dc.rights | © 2015 The Authors. Atmospheric Science Letters published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society. | en |
| dc.rights | This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. | en |
| dc.subject | Chimera grid method | en |
| dc.subject | overlapping grid method | en |
| dc.subject | non-hydrostatic model | en |
| dc.subject | high-resolution model | en |
| dc.subject | representation of a steep terrain | en |
| dc.subject | numerically generated coordinate | en |
| dc.title | Development of a non-hydrostatic atmospheric model using the Chimera grid method for a steep terrain | en |
| dc.type | journal article | - |
| dc.type.niitype | Journal Article | - |
| dc.identifier.jtitle | Atmospheric Science Letters | en |
| dc.identifier.volume | 17 | - |
| dc.identifier.spage | 109 | - |
| dc.identifier.epage | 114 | - |
| dc.relation.doi | 10.1002/asl.633 | - |
| dc.textversion | publisher | - |
| dcterms.accessRights | open access | - |
| 出現コレクション: | 学術雑誌掲載論文等 | |
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