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Local deforestation patterns and driving forces in a tropical dry forest in two municipalities of southern Oaxaca, Mexico (1985-2006)) 墨西哥瓦哈卡州南部两个城市热带干燥森林的森林砍伐模式和驱动力(1985-2006)
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.50918
R. Corona , L. Galicia , J.L. Palacio-Prieto , Matias Bürgi , Anna Hersperger

The tropical dry forest is an ecosystem that is undergoing rapid changes. Although global driving forces behind these changes have been addressed at a local scale, spatio-temporal dynamics are still largely unknown. The main objective of this study was to identify the causes governing the dynamics of changes in land use and land cover in the tropical dry forest in two municipalities in Southern México. Satellite imagery and air photographs were used in a gis context to produce maps of land use and land cover for 1985, 1995 and 2006. A number of statistical methods (Markov chains, general lineal models and regression tree analysis) were applied to identify the proximate and the underlying causes of deforestation, agriculture being the most important one. When agriculture is mainly for self consumption, topographic factors determine its location. Increasing job opportunities in the tourism sector has resulted in the abandonment of agricultural land; consequently, the forest has recovered. Different studies have examined the dynamics of local deforestation and its driving forces in México; however, this study considered both spatial and temporal elements in order to identify the most important underlying driving forces of deforestation and its dynamics at local scale, and also compared two neighboring municipalities.

热带干林是一个正在经历快速变化的生态系统。虽然这些变化背后的全球驱动力已经在局部尺度上得到了解决,但时空动态在很大程度上仍然未知。这项研究的主要目的是查明在莫桑比克南部两个城市的热带干燥森林中控制土地利用和土地覆盖变化动态的原因。卫星图像和航空照片在地理信息系统背景下用于制作1985年、1995年和2006年的土地利用和土地覆盖地图。采用了许多统计方法(马尔可夫链、一般线性模型和回归树分析)来确定森林砍伐的近因和根本原因,其中农业是最重要的原因。当农业以自用为主时,地形因素决定了其区位。旅游业就业机会的增加导致了农业用地的放弃;因此,森林已经恢复。不同的研究调查了当地森林砍伐的动态及其驱动力;然而,本研究同时考虑了空间和时间因素,以确定森林砍伐的最重要的潜在驱动力及其在地方尺度上的动态,并比较了两个相邻的城市。
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引用次数: 19
Exposición fotográfica: “La fotografía aérea de la Fundación ICA”, Instituto de Geografía, Universidad Nacional Autónoma de México, Ciudad Universitaria, Cd. Mx., agosto-noviembre 2016 摄影展:“ICA基金会的航空摄影”,墨西哥国立自治大学地理研究所,Ciudad Universitaria, Cd. Mx。2016年8月至11月
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.57887
Héctor Mendoza Vargas
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引用次数: 0
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.57878
Teresa Zweifel
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引用次数: 0
Los puertos de montaña de Atlatlahuca: un espacio estratégico en el siglo XVI 阿特拉拉胡卡山口:16世纪的战略空间
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.53179
Gustavo Garza Merodio , Federico Fernández Christlieb

The environmental characteristics of the upper Lerma river basin and the accessibility to the Balsas midelevation basin from its southern margins facilitated the settlement of different human groups since the early history of Mesoamerica. The mountain passes of Atlatlahuca were one of the most strategic ancient routes that communicated these basins, since no steep slopes had to be walked to descend or climb up over 700 meters, from the pre-Hispanic village of Atlatlahuca to the valley of Tenancingo. So far, the relevance of these mountain passes has not been recognized by the studies focused on the territorial evolution of the upper Lerma basin and neighboring regions.

The fifteenth and sixteenth centuries were the time when the strategic quality of these mountain passes reached its peak, first under the rule of the Matlatzinca federation, and later by the Aztecs and their allies. Historical approaches to the territorial evolution of the upper Lerma basin have focused on the lacustrine area that used to cover the lowlands; in our view, this approach is insufficient to explain the territorial evolution of this basin. An approach beyond watersheds or contemporary administrative limits, encompassing broader temporal and spatial scales, has revealed the strategic character of these mountain passes. Understanding these territorial priorities also requires to acknowledge the changes in landscape of the main historical settlements that controlled the access to these mountain passes: Tenango and Atlatlahuca. Our goal is not to outline a definitive version of this territorial structure; instead, we want to set the grounds for a discussion from a geographical viewpoint ranging several historic stages.

Our explanation is based on the principles of contemporary Cultural Geography and their application to areas of Mesoamerican tradition, and was derived from a continuous temporal analysis encompassing the Mesoamerican Post-Classic period and most of the 16th century. The cultural approach in geography aims to understand the thoughts and priorities of local inhabitants within their territorial context in different historical stages. In our case, the territorial structure we aim to explain involves physical changes in landscape, as well as changes in land use or in the way the environment is perceived according to different cultural practices.

In physical and biological terms, our case of study is located in the transition zone between Nearctic and Neotropical regions in southern-central Mexico. The mountain passes of Atlatlahuca descend from around 2 700 m a.s.l. to approximately 2 000 m in the valley of Tenancingo within less than 15 kilometers. The physical characteristics that assured a broad range of supplies and the control of vast territories. In our cultural reconstruction, besides physical and biological conditions, it is also necessary to understand the concept of altepetl: a nahuatl word that literally means “wa

莱尔玛河上游流域的环境特征和巴尔萨斯中高海拔盆地南缘的可达性为中美洲早期以来不同人类群体的定居提供了便利条件。阿特拉拉胡卡的山口是沟通这些盆地的最具战略意义的古代路线之一,因为从西班牙人之前的阿特拉胡卡村到Tenancingo山谷,700多米的地方不需要走陡峭的斜坡。到目前为止,对上勒玛盆地及其邻近地区的地域演化研究尚未认识到这些山口的相关性。15和16世纪是这些山口的战略价值达到顶峰的时期,最初是在Matlatzinca联邦的统治下,后来是在阿兹特克人及其盟友的统治下。历史上对上勒玛盆地地域演化的研究主要集中在过去覆盖低地的湖泊区域;我们认为,这种方法不足以解释该盆地的地域演化。一种超越流域或当代行政限制的方法,包括更广泛的时间和空间尺度,揭示了这些山口的战略特征。了解这些领土优先事项还需要认识到控制这些山口的主要历史定居点的景观变化:Tenango和Atlatlahuca。我们的目标不是勾勒出这种领土结构的最终版本;相反,我们想从地理角度出发,从几个历史阶段出发,为讨论奠定基础。我们的解释是基于当代文化地理学的原则及其在中美洲传统地区的应用,并来源于包括中美洲后古典时期和16世纪大部分时间的连续时间分析。地理学中的文化方法旨在了解不同历史阶段的地域语境中当地居民的思想和优先事项。在我们的案例中,我们旨在解释的领土结构涉及景观的物理变化,以及土地使用的变化或根据不同文化习俗感知环境的方式。在物理和生物方面,我们的研究案例位于墨西哥中南部新北极地区和新热带地区之间的过渡区。阿特拉特拉胡卡的山口在不到15公里的时间内从海拔约2700米下降到海拔约2000米的Tenancingo山谷。保证广泛供应和控制广大领土的物理特性。在我们的文化重建中,除了物理和生物条件外,还需要理解altepetl的概念:一个纳瓦特尔语,字面意思是“水山”,定义了中美洲后古典时代的城市空间。西班牙人发现的大部分阿尔特佩特在16世纪变成了印第安人村庄。在1470年阿兹特克征服该地区之前的主要语言Matlatzinca语言中,altepetl被翻译成inpuhetzi。我们试图解释的领土结构是基于几个因普赫特人在中美洲后古典时代早期的定居点,一些在内华达德托卢卡山前,另一些在勒玛盆地上游的孤立山上:Tenango和atlaltlahuha是这些定居点之一。这个位置使Matlatzinca人能够保护自己免受来自墨西哥盆地的攻击。然而,这种辩解并不能解释几个世纪以来马特拉津卡的永恒和辉煌。对我们来说,控制阿特拉特拉胡卡山口是取得如此宏伟成就的关键,这是与沿跨墨西哥火山带定居的其他国家共享的领土格局。在这种领土逻辑中,巨大的火山或陡峭的峡谷不是领土边界,而是连接手段。阿特拉特拉胡卡山口地区的重要性也源于在西班牙征服之前有大量的政治和行政单位在那里定居。在不到200平方公里的土地上,有6个阿尔特佩特尔和2个由塔库巴直接统治的村庄,塔库巴是阿兹特克人的一个小伙伴。西班牙人的征服导致这条古老的路线被遗弃。首先,从军事角度来看,它的战略价值在整个墨西哥中部被西班牙控制后消失了。其次,整个16世纪的人口减少和西班牙人对健康高地的优先考虑导致了大多数古代商业路线的放弃。
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引用次数: 3
Ciclo de conferencias “Vivienda y migración. Una mirada desde la geografía crítica”, Instituto de Geografía, Universidad Nacional Autónoma de México, Ciudad Universitaria, Cd. Mx., 22 y 26 de septiembre de 2016 “住房和移民”系列讲座。《来自批判地理的观点》,墨西哥国立自治大学地理研究所,Ciudad Universitaria, Cd. Mx。, 2016年9月22日和26日
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.57886
Luis Alberto Salinas Arreortua, Ana Melisa Pardo Montaño
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引用次数: 0
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.57882
Edgar Talledos Sánchez
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引用次数: 0
Evaluación de la aptitud natural de los paisajes físico-geográficos en la cuenca del río Grande, Oaxaca, México 墨西哥瓦哈卡州里约热内卢Grande盆地物理地理景观的自然适宜性评估
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.49203
Marco Antonio Pablo Pablo , José Ramón Hernández Santana

Environmental conservation depends largely on the appropriate management and rational use of natural resources. The assessment of natural landscapes and their suitability for human occupation is key to ensure optimal resource use. The criteria for establishing land-use potentials vary according to the type of activity concerned. For example, in determining the most suitable areas for growing grapes in Cuyo, Argentina, Valpreda (2005) focused on topography, soil quality and water availability, whereas in their study on the oil-producing region of northern Chiapas, Mexico, Bollo et al. (2010) applied markedly different criteria. Soil components and their variability were key to the multi-purpose study of Ovalles and Núñez (1994), while morphometric criteria have been used by Bocco et al. (2010) on farming; for cattle raising, Travieso-Bello et al. (2013) added soil quality and moisture, similar to Rodríguez-Gallego, et al. (2012). In the state of Oaxaca, scientific studies on the feasibility of human activity in different natural landscapes are yet to be undertaken. This study assesses the natural landscapes and resources of the Río Grande drainage basin aimed at establishing optimal locations for agriculture, livestock farming, forestry, wildlife conservation and their combinations. Following the FAO studies (1976, 1993), geomorphological and morphoclimatic systems have been considered as landscape units for analysis. The methodology was adapted from the following studies: The Revised Universal Soil Loss Equation (Ouyang, 2002); an estimate of soil pH based on Landsat imagery (López-Granados et al., 2005); a calculation of potential livestock carrying capacity (lcc) (Semarnat, 2003; Vergara and Ortiz-Espinoza, 2010); and a land use and vegetation cover analysis for forestry suitability and the potential distribution of two cat species (Lynx rufus and Panthera onca) (Chávez y Ceballos, 2006; Medellín-Legorreta and Bárcenas, 2009; Semarnat 2010; Semarnat-Conanp, 2010). Our analysis shows that 15.6% of the total area (152 km2) has optimal conditions for agriculture; 12.5% (122 km2) for livestock farming; 6.5% (64 km2) for conservational agricultural activities; 11% (108 km2) for conservational livestock production; 11.7% (114 km2) for conservational forestry activities; and 167 km2 (17.1%) for conservation alone. Finally, 25.6% of the territory (250 km2) is suitable (but not optimal) for agriculture, conservational livestock activities and conservation. This methodology based on physical-geographical landscapes allows to identify vocational land-use patterns across the Río Grande drainage basin as a means to optimize the management of the various economic activities. The identification and evaluation of productive and conse

环境保护在很大程度上取决于对自然资源的适当管理和合理利用。自然景观的评价及其对人类活动的适宜性是确保资源优化利用的关键。确定土地利用潜力的标准因有关活动的类型而异。例如,Valpreda(2005)在确定阿根廷Cuyo最适合种植葡萄的地区时,侧重于地形、土壤质量和水分供应,而Bollo等人(2010)在对墨西哥恰帕斯北部产油区的研究中采用了明显不同的标准。土壤成分及其变异是Ovalles和Núñez(1994)多用途研究的关键,而Bocco等人(2010)在农业方面使用了形态计量学标准;对于养牛,Travieso-Bello等人(2013)添加了土壤质量和水分,类似于Rodríguez-Gallego等人(2012)。在瓦哈卡州,关于人类活动在不同自然景观中的可行性的科学研究尚未开展。本研究评估了Río大流域的自然景观和资源,旨在建立农业、畜牧业、林业、野生动物保护及其组合的最佳位置。根据粮农组织的研究(1976年、1993年),地貌和形态气候系统已被视为分析的景观单位。该方法改编自以下研究:修订的通用土壤流失方程(欧阳,2002);根据陆地卫星图像估算土壤pH值(López-Granados等人,2005年);牲畜潜在承载能力(lcc)的计算(Semarnat, 2003年;Vergara and ortizs - espinoza, 2010);对两种猫科动物(猞猁和美洲豹)的森林适宜性和潜在分布进行了土地利用和植被覆盖分析(Chávez y Ceballos, 2006;Medellín-Legorreta和Bárcenas, 2009;Semarnat 2010;Semarnat-Conanp, 2010)。分析表明,该区15.6%的面积(152 km2)具有最佳农业发展条件;12.5%(122平方公里)用于畜牧业;6.5%(64平方公里)用于保护性农业活动;11%(108平方公里)用于保护性畜牧业生产;11.7%(114平方公里)用于保护性林业活动;仅保护区面积167平方公里(17.1%)。最后,25.6%的领土(250平方公里)适合(但不是最佳的)农业,保护性畜牧业活动和保护。这种基于自然地理景观的方法可以识别整个Río大流域的职业土地利用模式,作为优化各种经济活动管理的一种手段。确定和评价河流流域各种地貌和形态气候系统的生产和保护潜力是由两个基本的地理原则支配的:用整体方法对自然和地理限制进行空间分析,以及将自然资源绘制成地图,作为领土分析和制定最佳管理战略的投入。这两个原则都允许在自然倾向和最佳土地利用的放大镜下建立部门规划。同样的工作也可以进行,以使其他瓦哈坎地区以及其他区域和国家项目受益。
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引用次数: 1
Estructura territorial de la actividad pesquera en Guaymas, Sonora 索诺拉瓜伊马斯渔业活动的领土结构
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.49937
Gonzalo Yurkievich , Álvaro Sánchez Crispín

The aim of this paper is to ascertain the territorial dimension of the fishing economy in Guaymas, Mexico. The geographical studies addressing this economic activity in Mexico and published in the last decades are scarce. For this reason, this research work is particularly important, as it outlines the fishery activities in one of the most active sea-ports of northwest Mexico, from a territorial perspective. The first part of this article explains why and how Economic Geography addresses fishery activities and which methodology we pursued to carry out this investigation, based on studies carried out by geographers, particularly in France and Argentina. Then the paper describes the natural conditions prevailing in the Gulf of California (also known as Sea of Cortez), a large inlet of the eastern Pacific Ocean that is rich in marine resources and where most of the main national fisheries are located. Guaymas is one of the most important sea ports located along the Gulf of California for its long fishing history and the variety of fishing species captured. This port, located in the southern coast of the state of Sonora, is a mediumsized city with a little over 100 thousand inhabitants; a considerable proportion of the local labor force works in the fishery sector and associated industries. Today, the fishery sector in Guaymas is characterized by a large number of artisan fishermen, a prominent fleet preciand the regular practise of illegal catching. This port is the seat of large enterprises, such as Ocean Garden, involved in the industrialization of catches (basically fish oil and fish meal) and their further commercialization within and outside Mexico. Two commercially important species have played a key role in the evolution and outline of the current territorial structure of fisheries in Guaymas. One is shrimp, with a fishery that recorded a boom during 1970-1990, bringing along a number of benefits for local fishermen in Sonora. This fishery declined in subsequent years, mostly due to the overexploitation of shrimp banks and the incorporation of private capital investors to the local shrimp economy; the downward trend of this fishery in Guaymas is still evident. For its part, sardine, particularly Monterey sardine, is the other important species in the economy in this sea port. It is captured to meet the demand for oil and fish meal. Since the 1960s, Guaymas has become Mexico's sardine port, as this species is at the core of the territorial structure of fisheries in this city. A significant volume of sardine biomass has been captured in the last 50 years in Guaymas, resulting in the overexploitation of the resource which, along with water pollution, has led to the collapse of sardine populations. Nonetheless, stakeholders and authorities involved this fishery have obtained the international certification of local sardine catches. There are several enterprises located in Guaymas dedicated to the industrial processing of sard

本文的目的是确定在瓜伊马斯,墨西哥渔业经济的领土尺度。在过去的几十年里,关于墨西哥这一经济活动的地理研究很少发表。因此,这项研究工作特别重要,因为它从领土的角度概述了墨西哥西北部最活跃的海港之一的渔业活动。本文的第一部分解释了经济地理学研究渔业活动的原因和方式,以及基于地理学家(特别是法国和阿根廷的地理学家)的研究,我们采用了哪种方法来开展这项调查。然后,论文描述了加利福尼亚湾(也被称为科尔特斯海)的自然条件,这是东太平洋的一个大入口,海洋资源丰富,也是大多数主要国家渔业的所在地。瓜伊马斯是加利福尼亚湾沿岸最重要的海港之一,因其悠久的渔业历史和捕获的各种鱼类。这个港口位于索诺拉州的南部海岸,是一个拥有10多万居民的中型城市;相当大比例的当地劳动力在渔业部门和相关工业工作。今天,瓜伊马斯渔业部门的特点是大批手工渔民、一支重要的船队和经常进行非法捕捞。该港口是大型企业的所在地,如海洋花园,参与捕捞产业化(主要是鱼油和鱼粉)及其在墨西哥国内外的进一步商业化。两个具有重要商业价值的物种在瓜伊马斯目前渔业领土结构的演变和轮廓中发挥了关键作用。其中之一是虾,在1970-1990年期间,虾的捕鱼业出现了繁荣,为索诺拉当地渔民带来了许多好处。这一渔业在随后几年有所下降,主要是由于对虾库的过度捕捞和私人资本投资者加入当地对虾经济;瓜伊马斯这种渔业的下降趋势仍然很明显。就沙丁鱼而言,尤其是蒙特利沙丁鱼,是这个海港经济的另一个重要物种。捕鲸是为了满足对鱼油和鱼粉的需求。自20世纪60年代以来,瓜伊马斯已经成为墨西哥的沙丁鱼港口,因为这个物种是这个城市渔业领土结构的核心。在过去的50年里,瓜伊马斯捕获了大量的沙丁鱼生物量,导致资源的过度开发,再加上水污染,导致了沙丁鱼种群的崩溃。尽管如此,参与该渔业的利益相关者和当局已经获得了当地沙丁鱼捕捞的国际认证。在瓜伊马斯有几家企业专门从事沙丁鱼的工业加工。这些公司是垂直整合的,因此他们可以很容易地在墨西哥和国外购买渔获物,加工并销售制成品。这些和其他渔业产品的市场位于离瓜伊马斯相当远的地方,包括墨西哥城、瓜达拉哈拉、墨西卡利和奇瓦瓦市,以及美国加利福尼亚州的几个地方。墨西哥这一地区渔业经济的地域结构被安排在一个由大量和多样化的年捕鱼量构成的空间平台上,这是一个综合海港,不仅满足了这一经济的需求,还服务于索诺拉强大的工业和农业部门。造船厂、从事渔业的大型企业(本国和外国)、银行、学术研究中心和政府办公室都可以加入当地渔业基础设施。渔业产品(加工或不加工)商业化的地理范围,包括远离该港口的几个市场,是瓜伊马斯在索诺拉州和加利福尼亚湾渔业经济中发挥中心作用的另一个因素。
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引用次数: 8
Morfodinámica costera en la playa Bailén, costa sur del occidente de Cuba, entre los años 2003-2013 2003-2013年古巴西部南海岸bailen海滩的海岸形态动力学
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.47086
Alexis Ordaz Hernández , José Ramón Hernández Santana , Elmidio Estévez Cruz , Carlos Díaz Guanche , Ana Patricia Méndez Linares

Due to their geological nature, beaches are susceptible to changes over a relatively short period of time. Composed mainly of recently formed rocks, the scarcely consolidated structure of the substrate makes beaches vulnerable to the action of waves, tides, currents, wind, changes in sea level and human activity. Beach dynamics is marked by different degrees of fragility. In tropical regions, especially in the Caribbean, extreme hydro-meteorological phenomena such as hurricanes and cold fronts associated with extra-tropical storms significantly accelerate the erosion and accretion processes along the coast. The geographical location of the Cuban archipelago, at the margins of the Tropic of Cancer (its northernmost latitude is 27°17’ N), makes it susceptible to the combined action of hurricanes (between June and November) and cold fronts (between November and March). This very fact makes the study of coastal morphodynamic changes a subject of the utmost importance in sustainable-development projects and environmental planning, including the preservation of coastal natural resources. In Cuba, several authors have reported a coastal retreat of 1 to 3 m per year in western beaches, as well as an average loss of sand of about 50 000 m3 per year in the famous Varadero beach. The latter case is mainly due to the extraction of sand from the underwater platform between 1968 and 1978 for construction purposes. This paper addresses the morphodynamic processes taking place at Bailén beach, on the southwestern Cuban coast, as observed during a 10-year period, from 2003 to 2013. Transversal topographic measurements were taken at the beachfront and coastline at 15 observation stations along 2 140 m of beach in 2007, 2010 and 2013. These measurements were then compared to the data available for 2003. Estimated volumes of accreted and eroded sand for the period 2003-2007 indicate remarkable changes in beach morphology and evidence the vulnerability of coastal systems to extreme events, such as those unleashed by hurricane Ivan in 2004. The most important morphological changes observed included an increase of 0.20 to 0.50 m in dune height in some cases, and a decrease in others in the order of 0.15 to 0.40 m. Finally, granulometric tests were conducted to establish the spatial and temporal variations in the diameter of sand grains. To the north side of the beach, the maximum recession rate was 2.0 m per year, and sand grains were larger. Both measurements are indicative of the impact of buildings constructed at the front side of dunes and the beach berm on beach morphology. In the southern sector, on the other hand, the maximum accretion reached 8.0 m per year, whereas the average value was 2.3 m per year. During the 10 years of analysis, beach recovery has been characterized by a low resilience to the impact of hurricanes and other meteorological events. There is a clear spatial correlation between the inadequate location of buildings less than

由于其地质性质,海滩在相对较短的时间内容易发生变化。主要由新近形成的岩石组成,基材的结构几乎没有固结,这使得海滩容易受到波浪、潮汐、海流、风、海平面变化和人类活动的影响。海滩动态的特点是不同程度的脆弱性。在热带地区,特别是加勒比地区,与热带外风暴有关的飓风和冷锋等极端水文气象现象显著加速了沿海的侵蚀和增积过程。古巴群岛的地理位置位于北回归线的边缘(其最北纬为27°17′N),使其容易受到飓风(6月至11月)和冷锋(11月至3月)的共同作用。这一事实使得对沿海形态动力学变化的研究成为可持续发展项目和环境规划(包括保护沿海自然资源)中最重要的课题。在古巴,几位作者报告说,西部海滩每年后退1至3米,著名的巴拉德罗海滩每年平均损失约5万立方米的沙子。后一种情况主要是由于1968年至1978年期间为建设目的从水下平台提取沙子。本文讨论了2003年至2013年10年期间在古巴西南海岸的bail海滩上观察到的形态动力学过程。分别于2007年、2010年和2013年在海滨和海岸线2 140 m的15个观测站进行了横向地形测量。然后将这些测量结果与2003年的可用数据进行比较。据估计,2003-2007年期间的泥沙淤积量和侵蚀量表明了海滩形态的显著变化,并证明了海岸系统对极端事件的脆弱性,例如2004年“伊万”飓风引发的那些事件。观察到的最重要的形态变化是,有的沙丘高度增加了0.20 ~ 0.50 m,有的沙丘高度减少了0.15 ~ 0.40 m。最后,通过粒度试验确定了沙粒直径的时空变化规律。海滩北侧最大退缩速率为2.0 m /年,沙粒较大。这两项测量都表明了在沙丘正面建造的建筑物和海滩护堤对海滩形态的影响。南段最大增积量为8.0 m /年,平均为2.3 m /年。在10年的分析中,海滩恢复的特点是对飓风和其他气象事件影响的复原力较低。在距离海岸不到30米的沙丘和护堤上,海滩动态最强烈的地方,建筑物的位置不适当,与强烈侵蚀过程的发展之间存在明显的空间相关性,如在bail n海滩北部所观察到的那样。初始海岸线位置的缓慢恢复转化为沉积物平均直径的稳步增加。当水文气象事件发生时,这些海滩的低恢复能力变得更加明显。为了使通过重新安置当地沙子的海滩恢复项目取得成功,必须密切监测海滩,记录沉积物动态以及风和水对横向剖面的影响。此外,为了确保这种自然资源的有效再生,必须确定每线性米海滩的平均沙子体积。最后,拆除位于护堤和沙丘正面的旧建筑,并禁止在这些地点进行进一步的建设,应有助于恢复该海滩的形态动力平衡,提高旅游服务质量。
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引用次数: 0
Índice de vulnerabilidad costera del litoral tabasqueño, México 墨西哥塔巴斯科海岸脆弱性指数
Q3 Social Sciences Pub Date : 2016-12-01 DOI: 10.14350/rig.50172
Juan Carlos Núñez Gómez , Rodimiro Ramos Reyes , Everardo Barba Macías , Alejandro Espinoza Tenorio , Lilia María Gama Campillo

Sea level rise is one of the most serious events that will impact low-lying lands, as is the case of most of Tabasco State. Historically, the State of Tabasco has been repeatedly impacted by extreme floods, the most recent one occurring in 2007. However, recent studies have shown that coastal erosion is the effect that most directly has impacted the Tabasco's coastline, as this has even modified soil strata; this is also related to extreme hydrometeorological events associated with environmental changes and changes in the salinity gradient off the coast. In such a situation, future changes in the coastline are almost certain. Tabasco's coastline has been recognized as one of the most vulnerable zones in the country since Mexico's first national communication to the unfccc in 1997. Therefore, it is important to evaluate the vulnerability of this zone. The purpose of this study was to estimate the vulnerability of the Tabasco's coastline by applying the coastal vulnerability index method (ivm) using a geographic information system (gis). This method has been successfully applied in several different places around the world including Canada, the United State, Spain and Indonesia. This model is suitable for the local conditions of Tabasco coast, as the input variables it requires (including waves, tides, sea level, coastal slope, erosion rates and geomorphology) are available for the study area, thus allowing the possibility of estimating the coast's vulnerability based on local data. Results from map algebra operations showed that the zones of very high or high vulnerability encompass a six-kilometer stretch around the Sánchez Magallanes community, near the del Carmen lagoon in the municipality of H. Cárdenas, Tabasco. This is due to the high-waves regime and other conditions associated to the coastal dune geomorphology as well as the unconsolidated fine sediments prevailing therein. Other high vulnerability zones are found just in front of the major lagoon system in the State of Tabasco, the Carmen-Pajonal-Machona and Mecoacan lagoons; being the last one the most vulnerable of all. It is worth pointing out that this zone is located within the influence zone of the Dos Bocas port where an intense anthropogenic activity occurs. It is also important to point out that this study is one of the first approaches to the estimation of coastal vulnerability in Mexico. The implementation and application of this model of coastal vulnerability evaluation are significant given the spatial scale of the study and that this is the first time that these variables have been collected for the state of Tabasco. Our results might inform decision-making processes on the proper management of the Tabasco coastline, thus benefiting the local communities.

海平面上升是影响低洼地区的最严重事件之一,塔巴斯科州的大部分地区也是如此。从历史上看,塔巴斯科州多次受到极端洪水的影响,最近一次发生在2007年。然而,最近的研究表明,海岸侵蚀是最直接影响塔巴斯科海岸线的因素,因为它甚至改变了土壤层;这也与与环境变化和沿海盐度梯度变化有关的极端水文气象事件有关。在这种情况下,海岸线未来的变化几乎是肯定的。自1997年墨西哥首次向联合国气候变化框架公约提交国家通报以来,塔巴斯科的海岸线一直被认为是该国最脆弱的地区之一。因此,对该区域的脆弱性进行评估具有重要意义。本研究的目的是利用地理信息系统(gis),采用海岸脆弱性指数法(ivm)对塔巴斯科州海岸线的脆弱性进行评估。这种方法已经在世界上几个不同的地方成功应用,包括加拿大、美国、西班牙和印度尼西亚。该模型适用于塔巴斯科海岸的当地情况,因为它需要的输入变量(包括波浪、潮汐、海平面、海岸坡度、侵蚀速率和地貌)在研究区域是可用的,从而可以根据当地数据估计海岸的脆弱性。地图代数运算的结果显示,极高或高脆弱性区域包括在塔巴斯科州Cárdenas市del Carmen泻湖附近Sánchez Magallanes社区周围6公里长的区域。这是由于高浪状态和其他与海岸沙丘地貌有关的条件,以及其中普遍存在的未固结的细沉积物。其他高脆弱性区域位于塔巴斯科州主要泻湖系统的前面,卡门-帕约纳-马乔纳和梅科阿坎泻湖;作为最后一个最脆弱的人。值得指出的是,该区域位于发生强烈人为活动的多斯博卡斯港影响区内。同样重要的是要指出,这项研究是估计墨西哥沿海脆弱性的首批方法之一。考虑到研究的空间尺度,这是首次在塔巴斯科州收集这些变量,该沿海脆弱性评估模型的实施和应用具有重要意义。我们的结果可能会为塔巴斯科海岸线的适当管理决策过程提供信息,从而使当地社区受益。
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引用次数: 10
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Investigaciones Geograficas
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