2014年11月印尼海努桑塔拉探险(EWIN)期间的空间流结构

A. Purwandana, D. Surinati, A. Bayhaqi, M. F. Azis Ismail, M. R. Iskandar, C. Corvianawatie, A. S. Budiman, Edikusmanto Edikusmanto, D. Irianto, Muhadjirin Muhadjirin
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引用次数: 0

摘要

根据2014年11月wiya Nusantara远征(EWIN 2014)第1阶段的大量快照观测,绘制了印度尼西亚海域的空间洋流格局。使用RV Baruna Jaya VIII的舰载声学多普勒电流剖面仪(SADCP)测量电流剖面。本研究旨在通过观测揭示印尼海域的洋流系统。观察到印尼通流(ITF)在棉兰老海峡、望加锡海峡南部和利法马托拉海峡的显著流型,包括其在马鲁古海北部和苏拉威西海的再循环。这些结果表明,在东南季候风后期,上层ITF仍显著穿透印尼海域。班达海西部在50 m以上和75 m以下分别有反气旋和气旋环流的迹象
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The spatial current structure in the Indonesian Seas in November 2014, during The Expedition of Widya Nusantara (EWIN)
The spatial current patterns in the Indonesian seas were mapped based on a wide range of snapshot observations during the Expedition of Widya Nusantara (EWIN 2014) Leg 1 in November 2014. The current profiles were measured using the Shipboard Acoustic Doppler Current Profiler (SADCP) of the RV Baruna Jaya VIII. This study is aimed to reveal the current system in the Indonesian seas from observation. Remarkable current patterns of the Indonesian throughflow (ITF) were observed penetrating via the Mindanao Strait, southern Makassar Strait, and Lifamatola Passage, including its recirculation in the northern Maluku Sea and in the Sulawesi Sea. These results suggested that during the late Southeast Monsoon (SEM), the upper layer ITF is still significantly penetrating the Indonesian seas. The indication of anticyclonic and cyclonic circulations in the upper 50 m and lower 75 m, respectively, was also observed in the western Banda Sea
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