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Variability in water properties and predictability of sea surface temperature along Sanriku coast, Japan

机译:日本三陆沿岸水质变化和海表温度可预测性

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We investigated the main controlling factors and predictability of extreme sea surface temperature changes along the Sanriku coast (the east coast of the northern part of Japan's main island). We analyzed distributions of water properties and flow fields via intensive observations using a conductivity-temperature-depth profiler and a coastal water-temperature monitoring system from January 1998 to December 2012. Satellite altimetry and tide gauge data were also analyzed to investigate more widespread horizontal and temporal variation of the sea surface flow field. Anomalous temperature events (2 degrees C lower and higher than climatological monthly values) were observed in winter 2006 and fall 2010 and 2012 along the Sanriku coast. In winter (fall) 2006 (2010, 2012), we observed both unusually thick and wide cold/fresh (warm/saline) waters, corresponding to the Oyashio (Tsugaru Warm Current) waters. At that time, sea surface velocities of the Oyashio (Tsugaru Warm Current) along the Hokkaido coast (Tsugaru Strait) were also high. We propose new methods for predicting extreme temperature changes a few months in advance, based on current observations. (C) 2015 Elsevier Ltd. All rights reserved.
机译:我们调查了三陆沿岸(日本主岛北部的东海岸)沿海极端温度变化的主要控制因素和可预测性。我们使用电导率-温度-深度廓线仪和沿海水温监测系统,通过密集观测,分析了水质和流场的分布,从1998年1月至2012年12月。还分析了卫星测高仪和潮汐仪数据,以研究更广泛的水平和垂直方向海面流场的时间变化。在2006年冬季以及2010年和2012年秋季的Sanriku海岸,观测到了异常的温度事件(比气候月度值低2个摄氏度)。在2006年冬季(2010年,2012年秋季),我们观察到异常厚厚的冷/新鲜(温暖/咸水)水域,对应于Oyashio(Tsugaru暖流)水域。当时,沿北海道沿岸(春日海峡)的大潮(春日暖流)的海面速度也很高。根据当前的观察结果,我们提前几个月提出了预测极端温度变化的新方法。 (C)2015 Elsevier Ltd.保留所有权利。

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