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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Interannual variability of summer coastal upwelling in the Taiwan Strait
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Interannual variability of summer coastal upwelling in the Taiwan Strait

机译:台湾海峡夏季沿海上升流的年际变化

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This study dealt with the interannual variability of summer coastal upwelling in the Taiwan Strait, based on empirical orthogonal function (EOF) analysis. Three datasets were used for the analysis: the National Oceanic and Atmospheric Administration (NOAA), Advanced Very High Resolution Radiometer (AVHRR) sea surface temperature dataset from 1985 to 2005; hydrographic records at two coastal stations from 1970 to 2001; and cruise measurements in 1988 and 2004. The results indicated that the first mode (85.3%) of the spatial variance showed a persistent front, which was generally aligned northeast-southwestward in the western Taiwan Strait. This front separated colder water on the west side from warmer water on the east side. The eigenvector time series showed that the variability of this front with time was closely correlated with the change in the wind stress anomaly of the alongshore wind component, derived from 17 years of the European remote sensing (ERS) satellite and QuickScat wind dataset from 1992 to 2005. Records of water temperature and salinity anomaly at Pingtan Island (is.) located in the northwestern Taiwan Strait, and Dongshan Is. located in the southwestern Taiwan Strait, showed that a negative temperature anomaly appeared along with a positive salinity anomaly in some years. This suggested a dominant influence of cold and saline upwelling water at the surface. The years of notable cooling events derived from the station measurements were generally consistent with the time series of the EOF Mode 1. The change in upwelling derived from cruise measurements further confirmed the change shown by the EOF Mode I time series. These 1985-2005 results indicated that for the entire western Taiwan Strait summer coastal upwelling was strong in 1987,1993, and 1998, and that upwelling in the northwest and the southwest Taiwan Strait showed different behavior. A delayed ENSO (El Nino Southern Oscillation) effect was suggested as a major mechanism for the interannual variability of Taiwan Strait coastal upwelling. Crown Copyright (C) 2008 Published by Elsevier Ltd. All rights reserved.
机译:本研究基于经验正交函数(EOF)分析,处理了台湾海峡夏季沿海上升流的年际变化。分析使用了三个数据集:美国国家海洋和大气管理局(NOAA),1985年至2005年的超高分辨率高分辨率辐射计(AVHRR)海面温度数据集;以及1970年至2001年两个沿海站的水文记录;以及1988年和2004年的巡航测量结果。结果表明,空间方差的第一个模式(85.3%)显示出持续的前锋,在台湾海峡西部总体上呈东北-西南方向排列。该前沿将西侧的较冷水与东侧的较暖水分隔开。特征向量时间序列表明,该锋面随时间的变化与沿海风分量的风应力异常变化密切相关,后者源自欧洲遥感(ERS)卫星和QuickScat风数据集从1992年至17年的17年2005.台湾海峡西北部的平潭岛和东山岛的水温和盐度异常记录。位于台湾海峡西南部的海域显示,在几年中出现了负温度异常和正盐度异常。这表明表层的冷盐水和盐水上升流的主要影响。从台站测量得出的明显降温事件的年份通常与EOF模式1的时间序列一致。从巡航测量得出的上升流变化进一步证实了EOF模式I时间序列显示的变化。 1985-2005年的这些结果表明,在整个台湾海峡,夏季沿海上升趋势在1987、1993和1998年都很强烈,在台湾海峡西北部和西南部表现出不同的行为。延迟的ENSO(厄尔尼诺南方涛动)效应被认为是台湾海峡沿岸上升趋势年际变化的主要机制。 Crown版权所有(C)2008,由Elsevier Ltd.发行。保留所有权利。

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