書誌事項
- タイトル別名
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- INTERACTION OF LARGE-SCALE ATMOSPHERIC CONDITION AND LOCAL CIRCULATION WHICH AFFECTS CAMBODIAN POST-MONSOON RAINFALLS
説明
Characteristics of the post-monsoon rainfalls in Cambodia are examined through the combined use of NCEP-FNL global reanalysis data and the in-situ raingauge and AWS data. In the western Cambodia, rainfall still occurs during one month after the withdrawal of the Asian summer monsoon. About 30~40% of which was revealed to be brought by the redistribution of water vapor over Cambodia by the local atmospheric circulation. This rainfall occurs only under the period when there exists enough precipitable water. Decrease of precipitable water in China at late November reduces water vapor over Cambodia, resulting in disappearance of the locally-produced rainfall after this period. In addition, even when enough precipitable water exists, if the nighttime land-breeze at the southwest of the lake or the northeast winter monsoon is too weak, it doesn’t rain. Too strong winter monsoon is also unfavorable for local rainfall.
収録刊行物
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- 土木学会論文集Ｂ１（水工学）
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土木学会論文集Ｂ１（水工学） 67 (4), I_463-I_468, 2011
公益社団法人 土木学会
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詳細情報 詳細情報について
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- CRID
- 1390282680330071168
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- NII論文ID
- 130004557615
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- ISSN
- 2185467X
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可
