首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Offshore limit of coastal ocean variability identified from hydrography and altimeter data in the eastern Arabian Sea
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Offshore limit of coastal ocean variability identified from hydrography and altimeter data in the eastern Arabian Sea

机译:根据阿拉伯海东部的水文和高度计数据确定的沿海海洋变化的近海界限

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In this communication, we describe a hitherto-unknown offshore limit to the coastal ocean variability signatures away from the continental shelf in the eastern Arabian Sea, based on hydrographic observations and satellite altimeter (TOPEX/Poseidon) information. Vertical sections of temperature from two contrasting seasons-south-west (SW) and north-east (NE) monsoons-when projected together are found to intersect offshore at 350-400 km from the coast along a transect in the eastern Arabian Sea during 1996. Formation of such intersections along transects from south to north in the entire eastern Arabian Sea is noticed in the hydrographic data of 1987-88 also. Existence of these intersections has further been authenticated by the altimeter-derived sea level anomalies during 1992-97. It is proposed that these intersections arise due to the westward propagation of Rossby waves from the coastal Kelvin wave guide in the eastern Arabian Sea where alternate upwelling and downwelling processes occur during the contrasting seasons of SW and NE monsoons. We interpret these intersections as the offshore limit of variability of the water properties in the coastal region. Indications are that areas of high productivity in the coastal regions overlap a major portion of the width of intersection implying extension of the upwelling features towards offshore requiring revised estimates of primary productivity and carbon budgeting. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 13]
机译:在此通讯中,我们基于水文观测和卫星高度计(TOPEX / Poseidon)信息,描述了迄今为止阿拉伯海岸东部远离大陆架的沿海海洋变化特征的近海界限。在1996年期间,西南风(SW)和东北风(NE)的两个相反季节的温度垂直剖面在一起投影时发现沿海岸在阿拉伯海东部与海岸线相距350-400 km的近海相交。 1987-88年的水文数据中也注意到整个阿拉伯海东部从南到北沿着样带形成的这些交点。这些交集的存在已由1992-97年间由高度计得出的海平面异常进一步证实。提出这些交叉点是由于阿拉伯海东部沿海开尔文波导管的罗斯比波向西传播而造成的,在西南风和东北风季风的对比季节,交替的上升和下降过程发生。我们将这些交叉点解释为沿海地区水属性变化的近海极限。有迹象表明,沿海地区的高产区在交汇点宽度的大部分上重叠,这意味着上升特征向近海扩展,需要对初级生产力和碳预算进行修订后的估算。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:13]

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