Percampuran vertikal di Perairan Laut Maluku dan Talaud pada bulan Februari 2021

Adi Purwandana, Mochamad Riza Iskandar, Edi Kusmanto, M. Fadli, Priyadi Dwi Santoso, Corry Corvianawatie, Muhadjirin Muhadjirin, Marlin Chrisye Wattimena, Wang Zheng
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引用次数: 2

Abstract

Vertical mixing in the northern Maluku Sea and Talaud Waters in February 2021. The spatial variability of water mass mixing in the northern Maluku Sea and Talaud waters are presented based on the results of Eastern Indonesia Expedition (EIT) 2021 using RV Baruna Jaya VIII-LIPI. The turbulent kinetic energy dissipation rate was obtained using the Kunze-Williams-Briscoe (KWB) Method calculated from CTD (Conductivity, Temperature, Depth) and LADCP (Lowered Acoustic Doppler Current Profiler) datasets. We found the dissipation rate in the core layer of North Pacific Subtropical Water (NPSW) and North Pacific Intermediate Water (NPIW) are in the order of 10-6 W/kg and 10-8 W/kg, respectively. The KWB Method used in this study is also proven comparable with the Thorpe Method.
2021年2月北部马鲁古海和塔劳德水域的垂直混合。利用RV Baruna Jaya 8 - lipi,基于东印度尼西亚考察(EIT) 2021的结果,给出了马鲁古海北部和塔劳德水域水团混合的空间变异。湍流动能耗散率采用Kunze-Williams-Briscoe (KWB)方法,由CTD(电导率、温度、深度)和LADCP(低声多普勒电流剖面仪)数据集计算得到。北太平洋副热带水(NPSW)和北太平洋中间水(NPIW)核心层的消散速率分别为10-6 W/kg和10-8 W/kg。本研究中使用的KWB方法也被证明与索普方法具有可比性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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