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Reconstruction of drought episodes for central Spain from rogation ceremonies recorded at the Toledo Cathedral from 1506 to 1900: A methodological approach

机译:从1506年至1900年在托莱多大教堂记录的抄经仪式重建西班牙中部的干旱事件:一种方法学方法

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Rogation (ceremonies to ask God for rain: pro-pluvia, or to stop raining: pro-serenitate) analysis is an effective method to derive information about climate extremes from documentary data. Weighted annual sum by levels has been a widespread technique to analyze such data but this analysis is liable to be biased to spring values as these ceremonies are strongly related to farming activities. The analysis of the length of pro-pluvia periods (the time span during which rogations are carried out in relation to a drought event) and the combination of annual and seasonal information offers a more objective criterion for the analysis of the drought periods and an increase in the resolution of the study. Analysis by the pro-pluvia periods method of the rogation series from the Toledo (central Spain) Cathedral Chapter allows a good characterization of the droughts during the 1506-1900 period. Two drought maxima appear during the 1600-1675 and 1711-1775 periods, characterized by rogations during almost all the year, with a middle stage (1676-1710) when droughts were less frequent and their length shortened. Sea level pressure patterns for the instrumental and documentary periods show that droughts were mostly related to a north-eastern position of the Azores High that displaced the Atlantic low pressure systems towards a northern position. There is a weak relation with the North Atlantic Oscillation but this fact is related to the local character of the series that increases the weight of the local factors. Comparison of rainfall/drought records around Spain and the Western Mediterranean reveals the heterogeneity of their distribution in time and space as well as stresses the need of more and longer reconstructions. Better knowledge of drought variability would help to improve regional models of climate extremes and the understanding of the atmospheric patterns related to their development.
机译:轮转分析(要求上帝下雨的仪式:促成普鲁维亚,或停止下雨的仪式:促成衰老)分析是一种有效的方法,可从文献数据中得出有关极端气候的信息。按级别加权的年度总和已成为分析此类数据的一种广泛技术,但由于这些仪式与耕种活动密切相关,因此该分析易于偏向春季值。前雌蕊期的长度(与干旱事件相关的时间)的分析以及年度和季节信息的结合,为干旱期的分析和增加提供了更客观的标准。在研究的决议中。通过托卢多(西班牙中部)大教堂一章的lu级数序列分析法,可以很好地表征1506-1900年期间的干旱情况。在1600至1675年和1711-1775年出现了两次干旱最大值,其特征是几乎全年都在食,中间阶段(1676-1710)干旱较少且其长度缩短了。仪器和记录期的海平面压力模式表明,干旱主要与亚速尔群岛高东北部的位置有关,从而使大西洋低压系统向北部移动。与北大西洋涛动之间的关系较弱,但这一事实与该系列的局部特征有关,这增加了局部因素的权重。比较西班牙和西地中海周围的降雨/干旱记录,可以发现它们在时间和空间上的分布不均,并强调需要更多和更长的重建时间。更好地了解干旱的变异性将有助于改善极端气候的区域模型以及对与其发展有关的大气模式的了解。

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