哥伦比亚加勒比海海岸的海风

Ascario Pérez R., Juan Carlos Ortiz R., Luis F. Bejarano A., Luis Otero D., Juan C. Restrepo L., Andrés Franco H.
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引用次数: 11

摘要

海风环流是一个众所周知的重要中尺度系统,受陆地和海洋在一天内接收和储存太阳热量的不同特性的推动,它对波浪、海流和大气污染物的输送等的影响已经得到证实。这项工作的目的是描述南美洲北部哥伦比亚加勒比海三个沿海地区的海风特征:通过对哥伦比亚水文、气象和环境研究所1981-2008年数据的分析,以及对波哥大Jorge Tadeo Lozano大学观测站2010年1月1日至12月31日数据在圣玛尔塔市的详细分析,对列奥哈查、巴兰基利亚和圣玛尔塔进行了研究。Gustavsson的方法被用来确定海风的周期、持续时间、频率和每小时的模式;根据韦尔奇法修正的周期图进行波形表示和频谱分析。经证实,哥伦比亚加勒比海沿岸的海风信号在旱季(12月至3月)更为强烈,此时海风信号达到海陆温度梯度最高,且以日分量为主。在圣玛尔塔市和加勒比中部,海风比东北部的里奥哈察市和西南部的巴兰基利亚市更强,更明确,估计3月份的中值为4米s -1, 8月份的最小值为2米s -1。在巴兰基亚,海风信号达到2.5米s -1,而在里奥阿查,它达到1.5米s -1,都是在旱季(12月至3月)。结果表明,圣玛尔塔市的强信号与旱季海陆温梯度3 oC有关,巴兰基利亚为1.2 oC,列奥阿查小于1oC。尽管在列奥哈察市观测到7月海陆温梯度接近2.5 oC,但其特征不明确,信号强度不强,这可能与该地区几乎全年都存在强天气风、该地区的沙漠地貌及其地理位置有关。这是加勒比海地区第一次与海风有关的科学研究,其结果为研究这种微风对波谱、上升流、特别是污染物运输的影响奠定了重要基础,因为圣玛尔塔是哥伦比亚最重要的矿产煤炭港口之一,也是哥伦比亚北部海岸的主要旅游目的地之一。
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Sea breeze in the Colombian Caribbean coast
Circulation of sea breeze is a well-known and important mesoscale system, boosted by different properties of reception and storage of solar heat between land and sea during one day, and its effect on waves, currents, and transport of atmospheric contaminants, among others, has been proven. The aim of this work is to characterize sea breeze in three coastal zones of the Colombian Caribbean, in the north of South America: Riohacha, Barranquilla, and Santa Marta, through the analysis of data from the Instituto de Hidrologia, Meteorologia y Estudios Ambientales (Hydrology, Meteorology and Environmental Studies Institute) of Colombia during the period 1981-2008, and a detail analysis in the city of Santa Marta with data from the station of the Jorge Tadeo Lozano University of Bogota in the period January 1 st to December 31, 2010. Gustavsson´s method was used to identify the marine breeze cycle, its duration, frequency, and hourly pattern; hodograph representation and spectral analysis were performed according to the periodogram modified by the Welch method. It was established that the marine breeze signal in the Colombian Caribbean coast is stronger during the dry season (December-March), when it reaches the highest gradients of sea-land temperature and with a predominantly diurnal component. In the city of Santa Marta and central Caribbean, the sea breeze is stronger and more defined compared to those of the cities of Riohacha at the northeast, and Barranquilla at the southwest, reaching an estimated medium value of 4 m s –1 in March, and minimum values of 2 m s –1 in August. In Barranquilla, the sea breeze signal reaches 2.5 m s –1 , while in Riohacha it reaches 1.5 m s –1 , both in the dry season (December-March). According to the results, the strong signal in the city of Santa Marta is related to the gradient of 3 oC between the sea-land temperature in the dry season, while in Barranquilla is 1.2 oC, and in Riohacha it is less than 1oC. Despite having observed a sea-land temperature gradient close to 2.5 oC in July in the city of Riohacha, the hodograph is not well defined, and the signal magnitude is not strong, which could be related to the presence of strong synoptic winds almost the whole year, the desert landscape of the zone, and its geographical position. This the first scientific work related to marine breeze in this region of the Caribbean, and its results constitute an important base for studying the effect that such breezes may have on the spectrum of waves, upwelling, and especially in the transport of contaminants, given that Santa Marta is one of the most important harbors of mineral coal in Colombia, and one of the main touristic destinations in the northern Colombian coast.
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