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タカヤ コウタロウ
TAKAYA KOTARO
高谷 康太郎 所属 京都産業大学 理学部 宇宙物理・気象学科 職種 教授 |
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| 言語種別 | 英語 |
| 発行・発表の年月 | 2005/12 |
| 形態種別 | 研究論文 |
| 査読 | 査読あり |
| 標題 | Geographical dependence of upper-level blocking formation associated with intraseasonal amplification of the Siberian high |
| 執筆形態 | その他 |
| 掲載誌名 | JOURNAL OF THE ATMOSPHERIC SCIENCES |
| 出版社・発行元 | AMER METEOROLOGICAL SOC |
| 巻・号・頁 | 62(12),pp.4441-4449 |
| 著者・共著者 | K Takaya,H Nakamura |
| 概要 | Intraseasonal amplification events of the surface Siberian high in winter are generally associated with blocking ridge formation in the upper troposphere. Composite analysis applied to the 20 strongest intraseasonal events of upper-level anticyclonic anomalies at every grid point over Siberia reveals that the blocking formation differs fundamentally between the east and west of the climatological upper-level trough over the Far East. To the west, what can be called "wave-train (Atlantic-origin)" type is common, where a blocking ridge develops from anomalies as a component of a quasi-stationary Rossby wave train propagating across the Eurasian continent under modest feedback forcing from transient eddies. To the east of the trough, what can be called " Pacific-origin" type dominates, where a blocking ridge forms in association with westward development of anticyclonic anomalies from the North Pacific under stronger feedback forcing from the Pacific storm track. Regardless of a particular type of blocking formation in the upper troposphere, a cold air outbreak tends to occur once anomalously cold air reaches the northeastern slope of the Tibetan Plateau. |
| ISSN | 0022-4928 |