A shift in the spatial pattern of Iberian droughts during the 17th century

In this paper, series of drought occurrence and drought extension in the Iberian Peninsula are constructed for the 1600–1750 period from seven rogation series. These rogation ceremony records come from Bilbao, Catalonia, Zamora, Zaragoza, Toledo, Murcia and Seville. They are distributed across the P...

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Main Authors: F. Domínguez-Castro, R. García-Herrera, P. Ribera, M. Barriendos
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/6/553/2010/cp-6-553-2010.pdf
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spelling doaj-56cef76ea2574f639be75a9d568516d12020-11-24T23:09:42ZengCopernicus PublicationsClimate of the Past1814-93241814-93322010-09-016555356310.5194/cp-6-553-2010A shift in the spatial pattern of Iberian droughts during the 17th centuryF. Domínguez-CastroR. García-HerreraP. RiberaM. BarriendosIn this paper, series of drought occurrence and drought extension in the Iberian Peninsula are constructed for the 1600–1750 period from seven rogation series. These rogation ceremony records come from Bilbao, Catalonia, Zamora, Zaragoza, Toledo, Murcia and Seville. They are distributed across the Peninsula and include the areas with the most characteristic Iberian climate types, influenced by the Atlantic and the Mediterranean conditions, described from modern data. A seasonal division of the series shows that spring is a critical season for rogation series in most of Iberia, being Bilbao the only site were the highest number of rogations is detected for a different season. The annual analysis of the series shows a dramatic difference between the first half of the 17th century when droughts are characterized by its local character; and the rest of the period, when they affect to broader regions or even to the whole Peninsula. The analysis of spring series confirms the existence of the two periods detected in the annual analysis. Finally, secondary documentary sources are used to further characterise the two most extended droughts in the period, 1664 and 1680, and to verify the extension of the areas affected by droughts recorded through rogation series. http://www.clim-past.net/6/553/2010/cp-6-553-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author F. Domínguez-Castro
R. García-Herrera
P. Ribera
M. Barriendos
spellingShingle F. Domínguez-Castro
R. García-Herrera
P. Ribera
M. Barriendos
A shift in the spatial pattern of Iberian droughts during the 17th century
Climate of the Past
author_facet F. Domínguez-Castro
R. García-Herrera
P. Ribera
M. Barriendos
author_sort F. Domínguez-Castro
title A shift in the spatial pattern of Iberian droughts during the 17th century
title_short A shift in the spatial pattern of Iberian droughts during the 17th century
title_full A shift in the spatial pattern of Iberian droughts during the 17th century
title_fullStr A shift in the spatial pattern of Iberian droughts during the 17th century
title_full_unstemmed A shift in the spatial pattern of Iberian droughts during the 17th century
title_sort shift in the spatial pattern of iberian droughts during the 17th century
publisher Copernicus Publications
series Climate of the Past
issn 1814-9324
1814-9332
publishDate 2010-09-01
description In this paper, series of drought occurrence and drought extension in the Iberian Peninsula are constructed for the 1600–1750 period from seven rogation series. These rogation ceremony records come from Bilbao, Catalonia, Zamora, Zaragoza, Toledo, Murcia and Seville. They are distributed across the Peninsula and include the areas with the most characteristic Iberian climate types, influenced by the Atlantic and the Mediterranean conditions, described from modern data. A seasonal division of the series shows that spring is a critical season for rogation series in most of Iberia, being Bilbao the only site were the highest number of rogations is detected for a different season. The annual analysis of the series shows a dramatic difference between the first half of the 17th century when droughts are characterized by its local character; and the rest of the period, when they affect to broader regions or even to the whole Peninsula. The analysis of spring series confirms the existence of the two periods detected in the annual analysis. Finally, secondary documentary sources are used to further characterise the two most extended droughts in the period, 1664 and 1680, and to verify the extension of the areas affected by droughts recorded through rogation series.
url http://www.clim-past.net/6/553/2010/cp-6-553-2010.pdf
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