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Physical Drivers And Dominant Oceanographic Processes On The Uruguayan Margin (Southwestern Atlantic): A Review And A Conceptual Model

Journal of marine science and engineering(2021)SCI 3区SCI 4区

Univ Republica | Univ Republ | Univ Sao Paulo | Minist Ganaderia Agr & Pesca

Cited 4|Views21
Abstract
The Uruguayan continental margin (UCM), located in the Southwestern Atlantic margin's subtropical region, is positioned in a critical transitional region regarding the global ocean circulation (Rio de la Plata (RdlP) outflow and Brazil-Malvinas Confluence), as also reflected in seafloor features (northernmost distribution of a large depositional contourite system and RdlP paleovalley). This complex oceanographic scenario occurring in a relatively small area highlights the advantage of considering the UCM as a natural laboratory for oceanographic research. The present work provides the first conceptual "control" model of the physical drivers (i.e., climate, geomorphology) and main oceanographic processes (i.e., hydrodynamics, sediment, and carbon dynamics) occurring along the UCM, reviewing and synthesizing available relevant information based on a functional integrated approach. Despite the conspicuous knowledge gaps on critical processes, a general picture of the system's functioning is emerging for this complex biophysical setting. This includes conceptualizations of the actual controls, main processes, feedbacks, and interactions responsible for system dynamics. The structure adopted for developing our conceptual models allows permanent improvement by empirical testing of the working hypothesis and incorporating new information as scientific knowledge advances. These models can be used as a baseline for developing quantitative models and, as representations of relatively "pristine" conditions, for stressors models by identifying sources of stress and ecological responses of key system attributes under a transboundary approach.
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Uruguayan margin, Southwestern Atlantic, conceptual models
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要点】:本文综述了位于南大西洋subtropical区域的乌拉圭大陆边缘(Uruguayan continental margin, UCM)的物理驱动因素和主导海洋学过程,并提出了一个概念性模型,突显了气候、地质地貌因素以及水动力学、沉积物和碳动态等主要海洋学过程的综合作用。

方法】:本文采用功能整合方法,回顾和综合了基于物理驱动因素和主要海洋学过程的相关信息,并构建了首个概念性“控制”模型。

实验】:通过对乌拉圭大陆边缘的沉积物和碳动态进行研究,以及使用功能整合方法对气候、地质地貌等因素进行综合分析,构建了一个关于该区域物理驱动因素和主要海洋学过程的概念模型。该模型可以作为定量模型的基础,并作为相对“原始”条件下的压力模型,用于识别压力源和关键系统属性的跨界生态响应。