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An anatomy of storm surge science at Liverpool Tidal Institute 1919-1959 : forecasting, practices of calculation and patronage

机译:利物浦潮汐研究所风暴潮科学的解剖学1919-1959:预测,计算和赞助的实践

摘要

When the effects of wind and air pressure combine with a high tide to give unusually high water levels this can lead to severe coastal flooding. This happened in England in early 1953 when 307 people died in the East Coast Flood. In Britain today such events, now called storm surges, are forecast daily using computer models from the National Oceanographic Centre in Liverpool, formerly the Liverpool Tidal Institute (TI). In 1919, when TI was established, such events were considered unpredictable. TI's researchers, Joseph Proudman (1888-1975), Arthur Doodson (1890-1968), Robert Henry Corkan (1906-1952) and Jack Rossiter (1919-1972), did much mathematical work to attempt to change this. In 1959 Rossiter published a set of statistical formulae to forecast storm surges on the East Coast and a national warning system was predicting such events using these formulae. At this point TI believed they had made surges at least as predictable as they could with their existing methods. This thesis provides a narrative of how this perceived rise in the predictability of surges happened, analysing how TI worked to achieve it between 1919 and 1959 by following two interwoven, contingent and contested threads: practices of calculation and patronage. A key aspect of this thesis is the attention I pay to material practices of calculation: the methods, technologies and management practices TI's researchers used in their mathematical work on storm surge forecasting. This is the first study by historians of oceanography or meteorology that pays this detailed level of attention to such practices in the construction of forecasting formulae. As well as using published accounts, I analyse statistical research in the making, through notes, calculations, graphs and tables produced by TI's researchers. They used particular practices of calculation to construct storm surges as calculable and predictable scientific objects of a specific kind. First they defined storm surges as the residuals derived from subtracting tidal predictions from observations. They then decided to use multiple regression, correlating their residuals with pressure gradients, to make surges predictable. By considering TI's practices of calculation the thesis adds to the literature on mathematical research as embodied and material, showing how particular practices were used to make a specific phenomenon predictable. I combine this attention to mathematical practice with analysis of why TI's researchers did this work. US historians have emphasised naval patronage of physical oceanography in this period but there is very little secondary literature for the British case. The thesis provides a British case study of patronage of physical oceanography, emphasising the influence on TI's work not only of naval patronage but also of local government, civil state and industrial patronage. Before TI's establishment Proudman argued that it should research storm surges to improve the Laplacian theory of tides. However, when the new Institute received patronage from the local shipping industry this changed and the work on forecasting surges was initially done as part of a project to improve the accuracy of tidal predictions, earning TI further patronage from the local shipping industry. After a flooding event in 1928 the reasons for the work and the patronage again shifted. Between then and 1959 TI did this work on commission from various patrons, including local government, civil state and military actors, which connected their patronage to national debates about state involvement in flood defence. To understand why TI's researchers worked on forecasting surges I analyse this complex mix of patrons and motivations. I argue that such complex patronage patterns could be fruitfully explored by other historians to further existing debates on the patronage of oceanography.
机译:当风和气压的影响与高潮共同导致异常高的水位时,可能会导致严重的沿海洪水。这发生在1953年初的英格兰,当时有307人死于东海岸洪水。今天在英国,每天都会使用利物浦国家海洋学中心(以前是利物浦潮汐研究所(TI))的计算机模型来预报此类事件,即现在所谓的风暴潮。在1919年TI成立时,此类事件被认为是不可预测的。 TI的研究人员Joseph Proudman(1888-1975),Arthur Doodson(1890-1968),Robert Henry Corkan(1906-1952)和Jack Rossiter(1919-1972)做了大量的数学工作,试图改变这一点。 1959年,罗西特(Rosseter)发布了一套统计公式来预测东海岸的风暴潮,而国家预警系统正在使用这些公式来预测此类事件。在这一点上,TI相信他们已经使现有技术中的激增至少可以预见。本文提供了关于这种可预测的电涌可预测性如何发生的叙述,分析了TI如何通过遵循两条交织的,偶然的和有争议的线程在1919年至1959年之间实现这一目标:计算和光顾实践。本论文的一个关键方面是我对计算的重要实践的关注:TI的研究人员在风暴潮预报的数学工作中使用的方法,技术和管理实践。这是海洋学或气象学史学家的第一项研究,在构建预测公式时对这种实践给予了详细的关注。除了使用已发布的帐户外,我还通过TI研究人员制作的注释,计算,图表和表格来分析统计研究。他们使用特殊的计算方法将风暴潮构建为特定种类的可计算和可预测的科学对象。首先,他们将风暴潮定义为通过从观测值中减去潮汐预测得出的残差。然后,他们决定使用多元回归,将其残差与压力梯度相关联,以使浪涌可预测。通过考虑TI的计算实践,本论文增加了关于数学研究的文献资料,包括具体化和实质性内容,显示了如何使用特定实践来预测特定现象。我将对数学实践的关注与对TI研究人员为何进行这项工作的分析相结合。在此期间,美国历史学家强调了海军对自然海洋学的赞助,但英国案例的辅助文献很少。本文提供了英国对自然海洋学惠顾的案例研究,强调了TI的工作不仅对海军惠顾,而且对地方政府,民政和工业惠顾的影响。在TI成立之前,Proudman认为应研究风暴潮来改善拉普拉斯潮汐理论。但是,当新学院获得当地航运业的支持时,情况发生了变化,并且作为提高潮汐预测准确性的项目的一部分,有关预报浪涌的工作最初已经完成,从而为TI赢得了当地航运业的进一步支持。 1928年发生水灾后,工作和光顾的原因再次转移。从那时到1959年,TI都是根据各种赞助者的委托开展这项工作的,这些赞助者包括地​​方政府,民间国家和军事行为者,他们的赞助与有关国家参与防洪的全国性辩论相关。为了理解为什么TI的研究人员致力于预测激增,我分析了顾客和动机的这种复杂组合。我认为,其他历史学家可以探索这种复杂的光顾模式,以进一步开展有关海洋学光顾的辩论。

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