Identifikasi Massa Air Di Perairan Timur Laut Samudera Hindia

M. A. Ayubi, Heron Surbakti, La Ode Nurman Mbay
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Abstract

The northeast Indian Ocean is a region crossed by the monsoon winds and bordered by mainland on northern and eastern side that allegedly the water mass is influenced by these two factors. This research aims to study the vertical dan cross section distribution of physical parameters such as temperature, salinity, and density and also to identify the types of water masses in the region. The data used are the data of temperature, salinity, and density during 2007-2010 is obtained from sensors located on spacecraft of ATLAS Mooring. There are six stations located on the 90oE and from 0-15 oN, with 4 year observation and there are 4 periods each year. The results of observations of temperature on the surface indicates the period from December to February and March to May have a similar pattern. While the pattern in the period from June to August is similar to September-November. In other hand, the temperatures around depth of 140 m to the bottom shows the same pattern throughout the year. Value of the sea surface temperature of the period from March to May is generally the highest. Observations of sea surface salinity and water column generally are the same in each period, the salinity values decreased from a low-latitude station towards the high-latitude stations. The differences found are the highest surface salinity values are more common in the period from December to February, which is found on the station I and III. The result of value sea surface density observations show a decline pattern of low-latitudes stations in to higher latitudes stations throughout the year, or a pattern that tends to the same of salinity pattern. Analysis of the TS diagram refer to Wyrtki (1961) and Emery (2003) indicates there are some type of water masses, ther are namely the Bengal Bay Water (BBW), South Indian Central Water (SICW), Indian Equatorial Water (IEW), Subtropical Lower Water (SLW), and Northern Salinity Minimum (NSM). Those water masses is found in every period, only period from December to February have differrent type of water masses, that is the Arabian Sea Water (ASW). Keywords: ATLAS Mooring, Diagram TS, Indian Ocean, Water Mass
确定印度洋东北部水域的水质量
东北印度洋是一个被季风穿过的区域,在北部和东部与大陆接壤,据称水团受这两个因素的影响。本研究旨在研究该区域温度、盐度、密度等物理参数的垂直剖面分布,并识别该区域的水团类型。使用的数据是2007-2010年期间的温度、盐度和密度数据,这些数据来自ATLAS系泊航天器上的传感器。在东经90度和东经0 ~ 15度有6个台站,观测时间为4年,每年有4个周期。Â对地表温度的观测结果表明,12月至2月和3月至5月的温度变化具有相似的规律。而6月至8月期间的模式与9月至11月相似。另一方面,底部140米深处的温度全年呈现相同的模式。3 ~ 5月的海温值一般最高。各时段海面盐度和水柱的观测值基本相同,盐度值由低纬度站向高纬度站递减。发现的差异是,最高的地表盐度值在12月至2月期间更为常见,这在站1和站3上发现。海表密度值观测结果显示,低纬度站向高纬度站呈下降趋势,或呈与盐度趋势相同的趋势。Â参考Wyrtki(1961)和Emery(2003)对TS图的分析表明存在一些类型的水团,即孟加拉湾水(BBW),南印度中部水(SICW),印度赤道水(IEW),亚热带低洼水(SLW)和北部最低盐度(NSM)。这些水团在每个时期都存在,只有12月至2月的水团类型不同,即阿拉伯海水(ASW)。关键词:ATLAS系泊,图TS,印度洋,水团
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