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Long-term drought variability and trends in Barcelona (1787-2014) - imarina:5130245

Autor/s de la URV:Aguilar Anfrons, Enrique Modesto / COLL BENAGES, JOAN RAMON / Sigro Rodríguez, Francisco Javier
Autor segons l'article:Coll, J. R. Aguilar, E. Prohom, M. Sigro, J.
Adreça de correu electrònic de l'autor:enric.aguilar@urv.cat
javier.sigro@urv.cat
javier.sigro@urv.cat
Identificador de l'autor:0000-0002-8384-377X
0000-0003-0969-0338
0000-0003-0969-0338
Any de publicació de la revista:2016
Tipus de publicació:Journal Publications
ISSN:02116820
Referència de l'ítem segons les normes APA:Coll, J. R. Aguilar, E. Prohom, M. Sigro, J. (2016). Long-term drought variability and trends in Barcelona (1787-2014). Cuadernos De Investigacion Geografica, 42(1), 29-48. DOI: 10.18172/cig.2927
Referència a l'article segons font original:Cuadernos De Investigacion Geografica. 42 (1): 29-48
Resum:Long-term drought variability and trends were assessed in Barcelona at annual and seasonal scale for the period 1787-2014 and sub-periods 1851-2014, 1901-2014 and 1951-2014 to identify changes in drought patterns across time. High quality and adjusted monthly temperature and precipitation series were required for this purpose. The Standardized Precipitation Index (SPI), based on precipitation, and the Standardized Precipitation Evapotranspiration Index (SPEI), based on the difference between precipitation and reference evapotranspiration (ET0), were calculated to describe temporal drought fluctuations. Therefore, major droughts and wet events were identified and an accurate analysis of drought severity, magnitude and duration were also carried out. Both drought indices provided similar results related to drought variability and trends in Barcelona across time, although the SPEI showed larger drought severity than SPI especially during the second half of the 20th century. Trends analysis revealed a significant drying trend at annual scale according to the SPEI since mid-19th century while the SPI did not show changes in drought patterns. At seasonal scale, both the SPI and SPEI found a clear drying trend only for summer (JJA) during the current period (1951-2014), although the SPEI was indicating the trend towards drier conditions for the whole period (1787-2014). Drought severity in SPEI series increased 13% during the second half of the 20th century compared with the whole period under study while drought magnitude and duration did not present significant changes in both the SPI and SPEI series. The increasing atmospheric evaporative demand associated to the large temperature rising experienced in Barcelona during the last decades could have played a substantial role in explaining the increase of drought severity and trends found in the SPEI series.
DOI de l'article:10.18172/cig.2927
Enllaç font original:https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/2927
Versió de l'article dipositat:info:eu-repo/semantics/publishedVersion
Accès a la llicència d'ús:https://creativecommons.org/licenses/by/3.0/es/
Departament:Geografia
Grup de recerca:Centre en Canvi Climàtic (C3)
URL Document de llicència:https://repositori.urv.cat/ca/proteccio-de-dades/
Àrees temàtiques:Revistas de historia y filosofía
Human geography and urban studies
Geography, planning and development
Geography, physical
Geografia i urbanisme
Geografía
Environmental studies
Environmental science (miscellaneous)
Earth and planetary sciences (miscellaneous)
Ciencias sociales
Paraules clau:Spi
Spei
Drought
Climate change
Barcelona
Entitat:Universitat Rovira i Virgili
Data d'alta del registre:2024-03-23
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