Observations of intraseasonal variability in the Sunda Strait throughflow

Observations of intraseasonal variability in the Sunda Strait throughflow
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巽他海峡通流季节内变化的观测

DOI:
10.1007/s10872-018-0476-y
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发表时间:
2018-05
影响因子:
2.3
通讯作者:
Guohong Fang
Guohong Fang
中科院分区:
地球科学4区
文献类型:
--
作者:
Shujiang Li;Zexun Wei;R. Dwi Susant;Yaohua Zhu;Agus Setiawan;Tengfei Xu;Bin Fan;Teguh Agustiadi;Mukti Trenggono;Guohong Fang

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利用安装在底部的ADCP观测到的速度剖面,我们发现舜达海峡通过流具有很强的季节内变异性。这种季节内的变化,典型的周期为20-40天,最强的能量出现在北方的春季,可以逆转舜达海峡的通过流。进一步的分析表明,这种季节内变化与当地纬向风和海峡沿岸的海平面梯度密切相关。这些观测首次证实了Sunda海峡中存在从赤道印度洋传播的类似开尔文波的信号。这项研究还为开尔文波对舜天海峡通过流的影响提供了新的见解。
Using velocity profiles observed by bottom-mounted ADCPs, we identified strong intraseasonal variability in the Sunda Strait throughflow. This intraseasonal variability, with typical periods of 20–40days and the strongest energy occurring in the boreal spring, can reverse the Sunda Strait throughflow. Further analysis showed this intraseasonal variability to be closely related to local zonal wind and the sea level gradient along the strait. These observations confirm for the first time the existence of Kelvin-wave-like signals in the Sunda Strait, propagating from the equatorial Indian Ocean. This study also provides new insights into the effects of Kelvin waves on the Sunda Strait throughflow.
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