Seasonal variation of the sea surface salinity in the western tropical North Atlantic on two contrasting years of precipitation in the Amazon Basin

IF 2.2 3区 地球科学 Q2 OCEANOGRAPHY
Atila Matias, Clemente Tanajura, Janini Pereira, Felipe Costa
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Abstract

Motivated by the extreme hydrological events that caused an abnormal reduction and increase in discharge from the Amazon River in 2010 and 2012, respectively, this work investigates the seasonal variability of the sea surface salinity (SSS) in the western tropical Atlantic Ocean over these years. SMOS satellite data and a 1/12\(^{\circ }\) horizontal resolution of the coordinate ocean model (HYCOM) are used to investigate the SSS seasonal variation and assess the balance of mixed layer salinity (MLS) and the mechanisms that rule the SSS seasonal cycle. Two simulations with the same configuration, but with and without tides effects, are employed to investigate the impact of tides on the MLS balance in the region. The results show that the SSS of the Amazon River plume (ARP) was about 1.0 larger and covered a smaller area during the summer and early year boreal autumn of 2012 compared to 2010 in the area located to northwest of the North Brazil Current (NBC) retroflection region, even with the expressive increase in the supply of fresh water from the Amazon River in 2012 compared to 2010. This variability in SSS occurs shortly after the maximum discharge of the Amazon River and is associated with the highest input of freshwater precipitation from the Intertropical Convergence Zone (ITCZ) during the 2010 boreal spring and summer. The impact of tidal swings on the MLS balance in the western region of the tropical Atlantic Ocean occurs mainly in the area near the mouth of the Amazon and Pará Rivers, especially in the northwest portion of the mouth of the Amazon River until approximately Cabo Cassiporé. The forced tidal model shows an increase in MLS over the entire seasonal cycle of about 1.2, as well as a decrease in the contribution of zonal advection to the MLS balance, which reduces the zonal component from the west and increases the meridional component towards the north.

Abstract Image

亚马孙流域两个降水量对比年份热带北大西洋西部海面盐度的季节性变化
受 2010 年和 2012 年分别导致亚马逊河流量异常减少和增加的极端水文事件的影响,本研究调查了这两年热带大西洋西部海面盐度(SSS)的季节变化。研究利用SMOS卫星数据和1/12(^{\circ }\)水平分辨率的坐标海洋模式(HYCOM)来研究SSS的季节变化,评估混合层盐度(MLS)的平衡和SSS季节周期的作用机制。在相同配置下,采用了有潮汐效应和无潮汐效应的两种模拟,以研究潮汐对该地区混合层盐度平衡的影响。结果表明,与 2010 年相比,亚马逊河羽流(ARP)的 SSS 在 2012 年夏季和北巴西洋流(NBC)逆流区西北部地区的覆盖面积小了约 1.0,即使 2012 年亚马逊河淡水供应量比 2010 年有明显增加。SSS 的这种变化发生在亚马逊河最大排泄量之后不久,与 2010 年北方春季和夏季来自热带辐合带(ITCZ)的淡水降水输入量最大有关。潮汐摆动对热带大西洋西部地区 MLS 平衡的影响主要发生在亚马孙河和帕拉河河口附近地区,尤其是亚马孙河河口西北部地区,直到卡西波雷角附近。强制潮汐模型显示,在整个季节周期内,多级层流增加了约 1.2,同时,带状平流对多级层流平衡的贡献减少,这减少了来自西部的带状分量,增加了向北的经向分量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Ocean Dynamics
Ocean Dynamics 地学-海洋学
CiteScore
5.40
自引率
0.00%
发文量
37
审稿时长
6-12 weeks
期刊介绍: Ocean Dynamics is an international journal that aims to publish high-quality peer-reviewed articles in the following areas of research: Theoretical oceanography (new theoretical concepts that further system understanding with a strong view to applicability for operational or monitoring purposes); Computational oceanography (all aspects of ocean modeling and data analysis); Observational oceanography (new techniques or systematic approaches in measuring oceanic variables, including all aspects of monitoring the state of the ocean); Articles with an interdisciplinary character that encompass research in the fields of biological, chemical and physical oceanography are especially encouraged.
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