用区域海洋模拟系统绘制伊比利亚西北海岸的海流图

IF 1.7 3区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
T. Costa, Laudenor Pereira, M. Marta‐Almeida, Carlos Soares
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引用次数: 6

摘要

研究了2002-2004年伊比利亚西北边缘不同深度速度场的结构和时间变化。区域海洋模拟系统以高分辨率模拟海流,该系统与HYbrid坐标海洋模式再分析的输入数据、气候预报系统再分析的大气强迫以及TPXO全球潮汐解决方案的潮汐强迫兼容。在对数值模型结果进行初步验证后,绘制速度场图,以确定该地区的主要流特征及其季节和年际变化,以便找到具有强流的区域,这些区域可能对探索潮汐流能量有兴趣。数值域中存在3个不同水平的速度值高于周围的主要区域:(1)位于9.5°W左右的南向地表,与夏季上升流急流有关;(ii)位于离海岸较远的加利西亚海岸附近,以较深的水位向北流动,在一年中的大部分时间都可以看到;(iii)在Ría de awaka内,也全年可见。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mapping of currents off the northwestern Iberian coast with the Regional Ocean Modelling System
ABSTRACT The structure and the temporal variability of modelled velocity fields at different depths are studied for the years 2002–2004 in the Northwestern Iberian Margin. The currents are simulated with the Regional Ocean Modeling System in a high resolution that is compatible with the input data from the HYbrid Coordinate Ocean Model reanalysis and the atmospheric forcing from the Climate Forecast System Reanalysis, as well as with the tidal forcing from the TPXO Global Tide Solution. After an initial validation of the numerical model results, the velocity field is mapped to identify the region's main flow characteristics and its seasonal and interannual variability, in order to find areas that have strong currents, which could be of interest for exploring tidal stream energy. There are three main regions within the numerical domain, at different levels, where velocity values reach higher values than their surroundings: (i) located at the surface flowing south around 9.5°W, related to the summer Upwelling Jet; (ii) located further offshore near the Galician Bank, flowing north at deeper water levels which is visible during most part of the year and; (iii) within Ría de Arousa, also visible all year round.
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来源期刊
CiteScore
7.50
自引率
9.70%
发文量
8
审稿时长
>12 weeks
期刊介绍: The Journal of Operational Oceanography will publish papers which examine the role of oceanography in contributing to the fields of: Numerical Weather Prediction; Development of Climatologies; Implications of Ocean Change; Ocean and Climate Forecasting; Ocean Observing Technologies; Eutrophication; Climate Assessment; Shoreline Change; Marine and Sea State Prediction; Model Development and Validation; Coastal Flooding; Reducing Public Health Risks; Short-Range Ocean Forecasting; Forces on Structures; Ocean Policy; Protecting and Restoring Ecosystem health; Controlling and Mitigating Natural Hazards; Safe and Efficient Marine Operations
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