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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >First direct measurements of currents on the continental shelf of Southern Brazil
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First direct measurements of currents on the continental shelf of Southern Brazil

机译:首次对巴西南部大陆架上的洋流进行直接测量

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摘要

We examine the first in situ velocity data collected on the shelf of Southern Brazil. The mooring station with two current meters was deployed at 32degrees41'S, 51degrees27'W on March 4, 1997, and recovered on August 2, 1997. Also analyzed are wind data for the same period obtained at a nearby coastal meteorological station. The observed velocity series can be interpreted as a sum of highly variable flow correlated with local wind stress and a "residual" mean current flowing northward along the shore at a few centimetres per second. In winter, the Currents observed in the bulk of the water column exhibited a dramatic decrease in magnitude, as compared to the remainder of the series, although there was no similar decay of winds. We hypothesize that this is due to the impact of very stable salinity controlled winter stratification in a narrow subsurface layer because of enhanced river discharges that effectively isolates the deeper layers from atmospheric forcing. The frequency band corresponding to the periods from 2 to 10 days, presumably associated with meteorological forcing, dominated the velocity spectrum. The tidal Currents were weak and predominantly diurnal. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 18]
机译:我们检查了在巴西南部陆架上收集的第一批原位速度数据。带有两个水表的系泊站于1997年3月4日部署在32°41'S,51°27'W处,并于1997年8月2日恢复。还分析了附近海岸气象站同期的风数据。观测到的速度序列可以解释为与局部风应力相关的高度可变的流量和每秒(几厘米)沿着海岸向北流动的“剩余”平均电流之和。在冬季,尽管没有类似的风衰减,但与其余系列相比,在水柱大部分中观测到的洋流表现出幅度的显着下降。我们假设这是由于在狭窄的地下层中非常稳定的盐分控制的冬季分层的影响所致,这是因为河水流量的增加有效地将深层与大气强迫隔离开来。可能与气象强迫有关的2至10天周期对应的频段主导了速度谱。潮流潮流微弱,主要是昼间的。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:18]

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