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首页> 外文期刊>Environmental Research Letters >Vertical ground motion and historical sea-level records in Dakar (Senegal)
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Vertical ground motion and historical sea-level records in Dakar (Senegal)

机译:达喀尔(塞内加尔)的垂直地面运动和历史海平面记录

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With growing concerns regarding future impacts of sea-level in major coastal cities, the most accurate information is required regarding local sea-level changes with respect to the coast. Besides global and regional sea-level changes, local coastal vertical ground motions can substantially contribute to local changes in sea-level. In some cases, such ground motions can also limit the usefulness of tide-gauge records, which are a unique source of information to evaluate global sea-level changes before the altimetry era. Using satellite synthetic aperture radar interferometry, this study aims at characterizing vertical coastal ground motion in Dakar (Senegal), where a unique century-long record in Africa has been rediscovered. Given the limited number of available images, we use a stacking procedure to compute ground motion velocities in the line of sight over 1992–2010. Despite a complex geology and a rapid population growth and development, we show that the city as a whole is unaffected by differential ground motions larger than 1 mm year?1. Only the northern part of the harbor displays subsidence patterns after 2000, probably as a consequence of land reclamation works. However, these ground motions do not affect the historical tide gauge. Our results highlight the value of the historical sea-level records of Dakar, which cover a 100 year time-span in a tropical oceanic region of Africa, where little data are available for past sea-level reconstructions.
机译:随着人们对主要沿海城市海平面未来影响的担忧日益增加,需要有关沿海地区当地海平面变化的最准确信息。除了全球和区域的海平面变化外,当地沿海垂直地面运动还可以极大地促进当地的海平面变化。在某些情况下,这种地面运动还会限制潮汐仪记录的实用性,潮汐仪记录是评估测高时代之前全球海平面变化的唯一信息来源。这项研究使用卫星合成孔径雷达干涉测量法,旨在表征达喀尔(塞内加尔)的垂直沿海地面运动,那里已经重新发现了非洲一个独特的长达百年的记录。鉴于可用图像的数量有限,我们使用叠加程序来计算1992-2010年视线内的地面运动速度。尽管地质情况复杂且人口增长迅速,但我们证明了整个城市不受大于1毫米/年的地面地面运动的影响[1]。 2000年之后,只有海港北部显示出沉降模式,这可能是由于填海工程的结果。但是,这些地面运动不会影响历史潮汐仪。我们的结果凸显了达喀尔历史海平面记录的价值,该记录涵盖了非洲热带海洋地区100年的时间跨度,那里过去的海平面重建资料很少。

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