...
首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >The seasonal variability of the northern Benguela undercurrent and its relation to the oxygen budget on the shelf
【24h】

The seasonal variability of the northern Benguela undercurrent and its relation to the oxygen budget on the shelf

机译:本格拉北部暗流的季节性变化及其与陆架氧气收支的关系

获取原文
获取原文并翻译 | 示例
           

摘要

The seasonal variations in the advection and mixing of water masses in the northern Benguela were studied in relation to the oxygen minimum zone over the Namibian shelf. The used data set consists of hydrographic and current measurements from an oceanographic mooring 20 nm off Walvis Bay, monthly CTD transects from the Namibian 23 degrees S monitoring line and recent large-scale hydrographic surveys. The current time series showed an intermittent southward continuation of the Angola Current (AC) through the Angola-Benguela frontal zone (ABFZ) into the northern Benguela, commonly known as poleward undercurrent. In austral summer hypoxic, nutrient rich South Atlantic central water (SACW) from the Angola Gyre is transported into the northern Benguela, whereas during the winter season the oxygen rich Eastern SACW (ESACW) spreads northward. The water mass analysis reveals a mixing between both water masses in the northern Benguela between the ABFZ and the Luderitz upwelling cell (27 degrees S). The oxygen balance over the Namibian shelf depends to a high extent on the water mass composition of the upper central water layer, controlled by the large scale and local circulation. The deviation of the measured oxygen concentration from its mixing concentration, calculated with the source water mass properties, was used to quantify the oxygen consumption. A new local definition SACW was derived to exclude biogeochemical processes, taking place in the Angola Gyre. The oxygen deficit in the northern Benguela central water amounted to about 60-80 mu mol1(-1) at the shelf edge and increased up to 150 mu mol 1(-1) on the shelf, due to local oxygen consumption. In the austral summer anoxic bottom waters are observed at the central Namibian shelf, which correlate to an SACW fraction > 55%. Periods with high SACW fraction in the water mass composition were congruent with hydrogen sulphide events detected by remote sensing. (c) 2007 Elsevier Ltd. All rights reserved.
机译:研究了本格拉北部北部对流和混合水的季节性变化与纳米比亚陆架上的最小氧气区的关系。使用的数据集包括来自沃尔维斯湾20海里的海洋系泊的水文和当前测量值,来自纳米比亚23度监测线的每月CTD横断面以及近期的大规模水文调查。当前的时间序列显示,安哥拉洋流(AC)通过安哥拉-孟加拉国额带(ABFZ)间歇性地向南延续,进入本格拉北部,这通常被称为极向逆流。在夏季南半球缺氧的情况下,来自安哥拉回旋区的营养丰富的南大西洋中央水(SACW)被输送到本格拉北部,而在冬季,富氧的东部SACW(ESACW)向北扩散。水质分析揭示了本格拉北部的两个水质在ABFZ和Luderitz上升流单元之间(27度)之间的混合。纳米比亚陆架上的氧气平衡在很大程度上取决于上部中央水层的水质量组成,并受大规模和局部循环的控制。用源水质量特性计算得出的测得的氧气浓度与其混合浓度的偏差用于量化氧气消耗量。推导出了新的本地定义SACW,以排除发生在安哥拉涡旋中的生物地球化学过程。在本格拉北部中央水域,缺氧量约占架子边缘的60-80μmol1(-1),由于局部耗氧量,使架子上的缺氧量增加至150μmol 1(-1)。在南部夏季,在纳米比亚中部大陆架观察到缺氧底部水,这与SACW分数> 55%相关。在水质组成中SACW分数高的时期与通过遥感检测到的硫化氢事件是一致的。 (c)2007 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号