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首页> 外文期刊>Journal of oceanography >Observation of temperature and velocity from a surface buoy moored in the Shikoku Basin (OMLET-88) —An oceanic response to a Typhoon
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Observation of temperature and velocity from a surface buoy moored in the Shikoku Basin (OMLET-88) —An oceanic response to a Typhoon

机译:从四国盆地中系泊的浮标观察温度和速度(OMLET-88)—对台风的海洋反应

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A surface buoy was moored from 20 April to 2 November 1988 at 28°48′ N and 135°01′ E where the water depth was 4900 m to measure temperature and velocity in the upper 150 m. The Typhoon 8824 passed at 0300 (JST) on 8 October about 50 km north to the mooring station with a maximum wind speed of 43.5 m s?1. The buoy was shifted about 30 km to southwest, and the instruments were damaged. The records of temperature at 0.5 m and velocity at 50 m were obtained. The inertial oscillation caused by the typhoon is described using the current record. The oscillation endured for about 20 days. Deep mixing and vertical, heart transport by the typhoon are discussed based on the data from the Ocean Data Buoy of the Japan Meteorological Agency moored at 29°N and 135°E.
机译:1988年4月20日至11月2日,在28°48'N和135°01'E处停泊了一个表面浮标,其中水深为4900 m,以测量上部150 m的温度和速度。 8824号台风于10月8日在0300(日本标准时间)通过,向北约50公里处到达系泊站,最大风速为43.5 m s?1。浮标移至西南约30公里,仪器损坏。获得了0.5 m处的温度和50 m处的速度的记录。使用当前记录描述由台风引起的惯性振荡。振荡持续了约20天。根据日本气象厅海洋数据浮标在29°N和135°E处停泊的数据,讨论了台风的深层混合和垂直心脏传输。

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