2015-2016年El Niño期间秘鲁北部海岸观测到的异常强流

C. Shin, D. Gutiérrez
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引用次数: 0

摘要

秘鲁北部海岸是一个可以快速探测到Niño飓风影响的地区。为了研究2015-2016年El Niño对秘鲁北部海岸海洋环境的影响,研究人员分析了从一个石油平台的系泊设备获得的温度和洋流数据。虽然平均流速为0.10 m·s-1,但有3次观测到超过0.60 m·s-1的沿海强岸流,流向西南偏南。在第一次强流之后,底部温度升高,混合层加深并在El Niño事件期间保持在那里。在强烈的海岸流后,温度达到最大值,然后逐渐下降。风和海面高度异常分析表明,沿海强流是由开尔文波引起的,混合层的加深与局地风无关,而是与来自赤道的沿海开尔文波有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
On Abnormally Strong Currents Observed on the Northern Coast of Peru during the 2015-2016 El Niño
The northern coast of Peru is a region that can rapidly detect the impact of an El Niño. To investigate the effects of the 2015-2016 El Niño on the oceanographic environment of the northern coast of Peru, the temperature and current data obtained from moored equipment at an oil platform were analyzed. Strong coastal along-shore currents of more than 0.60 m·s-1 were observed three times, although the mean current speed was 0.10 m·s-1 flowing toward the south-southwest. After the first strong current, the bottom temperature increased and the mixed layer deepened and remained there during the El Niño event. The temperature reached a maximum after the strong coastal current, then decreased gradually. An analysis of wind and sea surface height anomalies revealed that the coastal strong current was caused by Kelvin waves and the deepening of the mixed layer was not related to local winds, but to coastal Kelvin waves from the equator during the El Niño event.
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