Grand Bahama Post-Hurricane Dorian

Kristen Welsh-Unwala, Anne Imig, Isabella Listl, Arno Rein
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Abstract

Freshwater lenses, a layer of fresh water that floats atop saline groundwater, are vulnerable sources of drinking water for small islands. The threats to freshwater lenses, and their recovery following catastrophic events, is not well documented. Due to storm surge and flooding during the Category 5 Hurricane Dorian in September 2019, the freshwater lenses of Grand Bahama were inundated with salt water, removing the freshwater source of drinking water for the island. This study builds on previous work to monitor the recovery of the freshwater lenses three years after the hurricane by assessing tidal lag, as well as stable isotopes in water (δ2H and δ18O), to understand the hydrologic characteristics of the FWL in Grand Bahama. Results from electrical conductivity revealed that the tidal lag, or the time it takes for the tidal effect to be observed in groundwater, was approximately 2.5 hours on average. Through stable isotope analysis of precipitation samples, we determined a local meteoric water line of δ2H = 8.2 * δ18O + 12.2, which is close to the global meteoric water line. Groundwater samples did not show evidence of significant evaporation from precipitation. These results serve as baseline data for additional monitoring and recovery efforts on Grand Bahama.
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多里安飓风过后的大巴哈马群岛
淡水透镜是浮在含盐地下水之上的一层淡水,是小岛上脆弱的饮用水来源。淡水透镜体面临的威胁,以及它们在灾难性事件后的恢复,并没有得到很好的记录。由于2019年9月5级飓风多里安期间的风暴潮和洪水,大巴哈马的淡水镜头被盐水淹没,消除了该岛饮用水的淡水来源。这项研究建立在之前的工作基础上,通过评估潮汐滞后以及水中的稳定同位素(δ2H和δ18O)来监测飓风发生三年后淡水透镜体的恢复情况,以了解大巴哈马FWL的水文特征。电导率的结果表明,潮汐滞后,即在地下水中观察到潮汐效应所需的时间,平均约为2.5小时。通过对降水样品的稳定同位素分析,我们确定了当地的大气水线δ2H = 8.2 * δ18O + 12.2,接近全球大气水线。地下水样本没有显示降水蒸发的显著证据。这些结果可作为大巴哈马进一步监测和恢复工作的基线数据。
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