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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Physico-chemical parameters of the SW and post NE monsoon (2009) seawater along the continental slope, Tamil Nadu, east coast of India, Bay of Bengal
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Physico-chemical parameters of the SW and post NE monsoon (2009) seawater along the continental slope, Tamil Nadu, east coast of India, Bay of Bengal

机译:西南大陆和泰米尔纳德邦,印度东海岸,孟加拉湾西南斜坡和西南季风后(2009年)海水的理化参数

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摘要

Variations in sea water temperature, salinity, light intensity and availability of nutrients strongly influence the phytoplankton distribution that forms an important part of the coastal food chain. In this paper, we present the results of the physico-chemical parameters and nutrient concentrations in seawaters sampled during the 2009 South West (SW) and post North East (NE) monsoon periods along the continental shelf from Chennai to Nagapattinam, east coast, Tamil Nadu. This study was conducted to assess the status of the coastal biogeochemical environment and for this purpose, seawater samples were collected from the sea surface and also at varying depths (surface to 150 m depth) at six different locations. The nutrient analyses and the CTD data reveal a distinct variation with water depth along the continental slope and also the physico-chemical properties of seawater are not homogenous. The observed values of nutrients for the post NE monsoon period are low compared to the SW monsoon period. Contour plots indicate seasonal and spatial variations in physico-chemical parameters along the continental shelf of the east coast of India. The data suggests that during the 2009 SW monsoon period, a significant increase of freshwater input into the Bay of Bengal could have elevated nutrient concentration compared to that observed during the post 2009 NE monsoon.
机译:海水温度,盐度,光照强度和养分利用率的变化极大地影响了构成沿岸食物链重要组成部分的浮游植物分布。在本文中,我们介绍了从西南地区(金奈到纳加帕蒂纳姆,东海岸,泰米尔)的大陆架,在2009年西南(SW)和东北后(NE)季风期间抽取的海水中的理化参数和营养物浓度的结果那都进行这项研究是为了评估沿海生物地球化学环境的状况,为此,从海表以及六个不同位置的不同深度(地表至150 m深度)收集了海水样本。营养成分分析和CTD数据显示,沿大陆坡的水深有明显的变化,海水的理化特性也不均一。与西南季风期相比,东北季风后时期的营养素观测值较低。等高线图显示了印度东海岸大陆架沿线理化参数的季节性和空间变化。数据表明,在2009年西南季风期间,与2009年东北季风后观测到的相比,向孟加拉湾输入的淡水显着增加可能会增加养分浓度。

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