亚马逊海岸带城镇的社会驱动风险:以巴西帕尔州的维吉亚·德·纳扎雷涅为例

C. Barreto, M. A. Pimentel
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引用次数: 0

摘要

Vigia de nazar是一个位于巴西帕尔州东北部的小镇,位于帕尔海岸带,是亚马逊海岸带的一个次区域。小镇坐落在该地区较低层次的梯田和河流海洋平原上。其社会空间演变的不同阶段反映了本文所分析的问题,特别是河流-海洋平原的占领和城市发展,这是大量家庭自发占领的,其中大多数家庭是社会弱势群体。本研究基于综合的历史地理方法和环境固有的不稳定性,调查了导致城市空间易受水文气象灾害影响的物理和社会过程。数据分析显示,该地区年降水水平较高,1月至5月是一个明确的雨季(月平均降水量超过300毫米),其环境以半日宏观潮汐为主,振幅可达4.5米。在2022年,60次高潮达到至少4.2米,这是可能由降雨引起的潮涌的警戒水平。最近对市区的占领集中在河流海洋平原的低洼地区,最近占城市中心的三分之一。这些地区暴露在当地河口环境的水文动力学中,导致环境退化和水形态动力学过程的改变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Socially-driven risk in a town of the Amazon coastal zone: the case of Vigia de Nazaré, in Pará state, Brazil
Vigia de Nazaré is a town located in the northeastern extreme of the Brazilian state of Pará, in the Pará Coastal Zone, a sub-region of the Amazon Coastal Zone. The town sits on the lower levels of the region’s terraces, and on fluviomarine plains. The different stages of its sociospatial evolution reflect the problem analyzed here, in particular, the occupation and urban development of the fluvial-marine plains, which was occupied spontaneously by large numbers of families, most of which are socially vulnerable. The present study investigated the physical and social processes that led this urban space’s vulnerability to hydrometeorological hazards, based on an integrated historical-geographic approach and the inherent precariousness of the environment. The data analysis revealed high levels of annual precipitation in the region, with a well-defined rainy season between January and May (mean monthly precipitation of over 300 mm), in an environment dominated by semidiurnal macro tides with amplitudes of up to 4.5 meters. In 2022, the high tide reached at least 4.2 meters in 60 occasions — the level of alert for possible rainfall-induced tidal surges. The recent occupation of the urban zone is concentrated on the low-lying areas of the fluviomarine plain, which recently account for one-third of the urban center. These areas are exposed to the hydrological dynamics of the local estuarine environment, which result in environmental degradation and hydro-morphodynamic processes alteration.
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