| dbo:abstract |
The 1949 Pacific typhoon season has no official bounds; it ran year-round in 1949, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1949 Pacific hurricane season. At the time, tropical storms that formed within this region of the western Pacific were identified and named by the United States Armed Services, and these names are taken from the list that USAS publicly adopted before the 1945 season started. (en) 1949年太平洋颱風季泛指在1949年全年內的任何時間，於赤道以北及國際換日線以西的太平洋水域，以及南中國海所產生的熱帶氣旋。雖然有關方面並沒有設下本颱風季的指定期限，但大部份於西北太平洋的熱帶氣旋通常都會於五月至十二月期間形成。 本條目的範圍僅侷限於赤道以北及國際換日線以西的太平洋及南海的水域。於赤道以北及國際換日線以東的太平洋水域產生的風暴則被稱為颶風，並被列入。在西太平洋產生的熱帶風暴是由聯合颱風警報中心命名，國際編號為49xx。而凡進入或產生於菲律賓風暴責任範圍以內的熱帶低氣壓，菲律賓大氣地理天文部門 (PAGASA) 都會為它們訂立一個菲律賓名稱，作當地警報用途；因此同一個風暴有時候會有兩個不同的名稱。 以下各熱帶氣旋資訊以熱帶氣旋存在期間的最強形態為準。 (zh) |
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> (en) |
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1949 (xsd:integer) |
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34 (xsd:integer) |
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14 (xsd:integer) |
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0 (xsd:integer) |
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226 (xsd:integer) |
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1949 (xsd:integer) Allyn 1949 track.png (en) |
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| rdfs:comment |
1949年太平洋颱風季泛指在1949年全年內的任何時間，於赤道以北及國際換日線以西的太平洋水域，以及南中國海所產生的熱帶氣旋。雖然有關方面並沒有設下本颱風季的指定期限，但大部份於西北太平洋的熱帶氣旋通常都會於五月至十二月期間形成。 本條目的範圍僅侷限於赤道以北及國際換日線以西的太平洋及南海的水域。於赤道以北及國際換日線以東的太平洋水域產生的風暴則被稱為颶風，並被列入。在西太平洋產生的熱帶風暴是由聯合颱風警報中心命名，國際編號為49xx。而凡進入或產生於菲律賓風暴責任範圍以內的熱帶低氣壓，菲律賓大氣地理天文部門 (PAGASA) 都會為它們訂立一個菲律賓名稱，作當地警報用途；因此同一個風暴有時候會有兩個不同的名稱。 以下各熱帶氣旋資訊以熱帶氣旋存在期間的最強形態為準。 (zh) The 1949 Pacific typhoon season has no official bounds; it ran year-round in 1949, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. (en) |
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1949 Pacific typhoon season (en) 1949年太平洋颱風季 (zh) |
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