Research Article
Precipitation variability and change in the Calabria region (Italy) from a high resolution daily dataset
Article first published online: 7 OCT 2010
DOI: 10.1002/joc.2233
Copyright © 2010 Royal Meteorological Society
Additional Information
How to Cite
Brunetti, M., Caloiero, T., Coscarelli, R., Gullà, G., Nanni, T. and Simolo, C. (2012), Precipitation variability and change in the Calabria region (Italy) from a high resolution daily dataset. Int. J. Climatol., 32: 57–73. doi: 10.1002/joc.2233
Publication History
- Issue published online: 3 JAN 2012
- Article first published online: 7 OCT 2010
- Manuscript Accepted: 31 AUG 2010
- Manuscript Revised: 5 AUG 2010
- Manuscript Received: 30 APR 2010
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Keywords:
- precipitation;
- homogenisation;
- precipitation intensity;
- Italy
Abstract
The present study aims at improving data availability and quality for the last 80–90 years for daily precipitation in the Calabria region (southern Italy). First, the original database was homogenised and the gaps filled in for 129 daily rain gauges for the 1916–2006 period. Then, precipitation variability and change were evaluated at an adequate spatial resolution. Monthly and annual total precipitation (P), number of wet days (WDs), and precipitation intensity (PI) were calculated for each series. With regard to the monthly total precipitation a general negative trend, albeit not everywhere significant, was detected, in particular for the autumn–winter period, while in summer the tendency was toward an increase in total precipitation. The monthly behaviour of WDs was not very different from that observed for P: a diffuse negative trend was detected in most months, particularly evident and significant in January, with the exception of April and the summer months, for which the tendency was toward an increase. Regarding the PI, a general negative and often significant trend was found for the entire region and for almost all the months, except summer. Attention was also focused on tendencies in the different PI categories, revealing negative trends in high-intensity categories, especially coming from the winter season.
Finally, running trend analysis revealed that the previously discussed tendencies were not persistent throughout the series length, but depended on the period examined. This important aspect should be taken into account when different results based on different time windows are compared. Copyright © 2010 Royal Meteorological Society

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