Abstract

Abstract. Long time series (95 to 135 yr) of the 12-month time scale Standardized Precipitation Index (SPI) relative to 10 locations across Portugal were studied with the aim of investigating if drought frequency and severity are changing through time. Considering four drought severity classes, time series of drought class transitions were computed and later divided into several sub-periods according to the length of SPI time series. Drought class transitions were calculated to form a 2-dimensional contingency table for each sub-period, which refer to the number of transitions among drought severity classes. Two-dimensional log-linear models were fitted to these contingency tables and an ANOVA-like inference was then performed in order to investigate differences relative to drought class transitions among those sub-periods, which were considered as treatments of only one factor. The application of ANOVA-like inference to these data allowed to compare the sub-periods in terms of probabilities of transition between drought classes, which were used to detect a possible trend in droughts frequency and severity. Results for a number of locations show some similarity between alternate sub-periods and differences between consecutive ones regarding the persistency of severe/extreme and sometimes moderate droughts. In global terms, results do not support the assumption of a trend for progressive aggravation of drought occurrence during the last century, but rather suggest the existence of long duration cycles.

Highlights

  • Drought is a normal recurrent feature of climate, which occurs in all climatic zones, though with varied characteristics

  • The definition proposed by Pereira et al (2009) is assumed: drought is a natural but temporary imbalance of water availability, consisting of a persistent lower-than-average precipitation, of uncertain frequency, duration and severity, of unpredictable or difficult to predict occurrence, resulting in diminished water resources availability and reduced carrying capacity of the ecosystems, affecting socioeconomic activities and the society

  • Precipitation based drought indices are the first indicators of droughts, since hydrological droughts may emerge

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Summary

Introduction

Drought is a normal recurrent feature of climate, which occurs in all climatic zones, though with varied characteristics. There are many definitions of drought, often related with the sector perceiving or being impacted by it, leading to define meteorological, agricultural, hydrological and socioeconomic droughts (Dracup et al, 1980; Tate and Gustard, 2000; Mishra and Singh, 2010). Assessing changes in drought frequency and severity, possibly aggravating with time, is important to develop related risk management issues. There are various drought indices for assessing drought severity (Heim, 2002; Keyantash and Dracup, 2002; Mishra and Singh, 2010). Precipitation based drought indices are the first indicators of droughts, since hydrological droughts may emerge

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