Laboratoire des Sciences du Climat et de l'Environnement, UMR 8212 CEA-CNRS-UVSQ-UPSaclay, Gif-sur-Yvette Cedex, France.
Laboratoire de Météorologie Dynamique, UMR8539 ENS-X-UPMC, Palaiseau, France.
Sci Rep. 2018 Oct 26;8(1):15896. doi: 10.1038/s41598-018-34228-7.
The 1783-1784 Laki eruption provides a natural experiment to evaluate the performance of chemistry-transport models in predicting the health impact of air particulate pollution. There are few existing daily meteorological observations during the second part of the 18 century. Hence, creating reasonable climatological conditions for such events constitutes a major challenge. We reconstructed meteorological fields for the period 1783-1784 based on a technique of analogues described in the Methods. Using these fields and including detailed chemistry we describe the concentrations of sulphur (SO/SO) that prevail over the North Atlantic, the adjoining seas and Western Europe during these 2 years. To evaluate the model, we analyse these results through the prism of two datasets contemporary to the Laki period: • The date of the first appearance of 'dry fogs' over Europe, • The excess mortality recorded in French parishes over the period June-September 1783. The sequence of appearances of the dry fogs is reproduced with a very-high degree of agreement to the first dataset. High concentrations of SO/SO are simulated in June 1783 that coincide with a rapid rise of the number of deceased in French parishes records. We show that only a small part of the deceased of the summer of 1783 can be explained by the present-day relationships between PM2.5 and relative risk. The implication of this result is that other external factors such as the particularly warm summer of 1783, and the lack of health care at the time, must have contributed to the sharp increase in mortality over France recorded from June to September 1783.
1783-1784 年拉基火山喷发为评估化学传输模型在预测空气颗粒物污染对健康影响方面的性能提供了一个自然实验。在 18 世纪后半叶,现有的每日气象观测数据很少。因此,为这类事件创造合理的气候条件是一个主要挑战。我们根据方法中描述的类似技术,重建了 1783-1784 年期间的气象场。利用这些场,并包括详细的化学数据,我们描述了这两年间在北大西洋、毗邻海域和西欧盛行的硫(SO/SO)浓度。为了评估模型,我们通过与拉基时期同期的两个数据集来分析这些结果:• 欧洲首次出现“干雾”的日期,• 1783 年 6 月至 9 月期间法国教区记录的超额死亡率。干雾出现的顺序与第一个数据集高度一致。1783 年 6 月模拟出了 SO/SO 的高浓度,与法国教区记录的死亡人数迅速增加相吻合。我们表明,只有一小部分 1783 年夏季的死亡人数可以用当今 PM2.5 和相对风险之间的关系来解释。这一结果的含义是,其他外部因素,如 1783 年特别温暖的夏季以及当时缺乏医疗保健,必须对 1783 年 6 月至 9 月期间法国记录的死亡率急剧上升做出贡献。