Freshwater plume’s impact on the thermohaline structure of the water column in the Central Zone of the Strait of Magellan

IF 2.4 4区 环境科学与生态学 Q3 ECOLOGY Regional Studies in Marine Science Pub Date : 2025-04-01 Epub Date: 2025-02-19 DOI:10.1016/j.rsma.2025.104087
Vicente Aravena-Yáñez , José Garcés-Vargas , Iván F. Benavides-Martínez
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Abstract

The Strait of Magellan, a sub-Antarctic channel connecting the Pacific and Atlantic oceans, is divided into three zones based on oceanographic and meteorological characteristics: Eastern, Central, and Western. The Central Zone is influenced by strong northwesterly winds and freshwater inputs from rivers and precipitation, making it crucial to understand its thermal and haline dynamics in response to these forcings. This study examines the seasonal variability of temperature and salinity in the water column at a fixed station in the Central Zone from 2018 to 2022, analyzing key environmental drivers. A detailed assessment of absolute salinity fluctuations in the upper layers was conducted using ocean reflectance from Sentinel-2 satellite data, river discharge, and wind dynamics, modeled with a generalized additive model incorporating delayed effects. Results reveal a seasonal surface temperature pattern, increasing in summer and decreasing in winter due to solar radiation. In winter, the surface layer remained relatively uniform, while summer conditions led to thermal stratification driven by intense solar heating. A winter thermal inversion was observed, attributed to reduced solar radiation and the vertical intrusion of warmer Modified Subantarctic Water from the Pacific. Surface salinity exhibited a seasonal cycle, with lower values and stronger stratification in winter due to freshwater discharge and wind-driven advection of the river plume toward the study site. In contrast, deeper layers remained relatively homogeneous in temperature and salinity, influenced by Pacific-origin Modified Subantarctic Water. Climate change-driven shifts in these forcings could alter the water column structure, impacting ecosystem functioning and Indigenous communities reliant on marine resources. This study provides essential insights into the thermal and haline dynamics of the Central Zone, supporting marine biodiversity management and conservation efforts in the region.
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淡水羽流对麦哲伦海峡中心区水柱温盐结构的影响
麦哲伦海峡是一条连接太平洋和大西洋的亚南极海峡,根据海洋学和气象特征,它被分为三个区域:东部、中部和西部。中部地区受强烈的西北风和来自河流和降水的淡水输入的影响,因此了解其响应这些强迫的热动力学和盐动力学至关重要。本文研究了2018 - 2022年中组区固定站水柱温度和盐度的季节变化,分析了主要环境驱动因素。利用Sentinel-2卫星数据的海洋反射率、河流流量和风动力,采用包含延迟效应的广义加性模型建模,对上层绝对盐度波动进行了详细评估。结果表明,受太阳辐射影响,地表温度呈夏季升高、冬季降低的季节性变化趋势。在冬季,表层保持相对均匀,而在夏季,强烈的太阳加热导致热分层。观测到冬季热逆温,这是由于太阳辐射减少和来自太平洋的暖化亚南极水的垂直侵入。表层盐度表现出季节性循环,冬季由于淡水排放和风驱动的河流羽流向研究地点平流,表层盐度值较低,分层作用较强。相比之下,受源自太平洋的变质亚南极水的影响,较深层在温度和盐度方面保持相对均匀。气候变化驱动的这些作用力变化可能改变水柱结构,影响生态系统功能和依赖海洋资源的土著社区。这项研究为了解中部地区的热和盐动态提供了重要的见解,为该地区的海洋生物多样性管理和保护工作提供了支持。
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来源期刊
Regional Studies in Marine Science
Regional Studies in Marine Science Agricultural and Biological Sciences-Ecology, Evolution, Behavior and Systematics
CiteScore
3.90
自引率
4.80%
发文量
336
审稿时长
69 days
期刊介绍: REGIONAL STUDIES IN MARINE SCIENCE will publish scientifically sound papers on regional aspects of maritime and marine resources in estuaries, coastal zones, continental shelf, the seas and oceans.
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