2010
DOI: 10.1029/2009wr008071
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Spatial and temporal variability of droughts in Portugal

Abstract: An analysis of droughts in mainland Portugal based on monthly precipitation data, from September 1910 to October 2004, in 144 rain gages distributed uniformly over the country is presented. The drought events were characterized by means of the Standardized Precipitation Index (SPI) applied to different time scales (1, 6, and 12 consecutive months and 6 months from April to September and 12 months from October to September). To assess spatial and temporal patterns of droughts, a principal component analysis (PC… Show more

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Cited by 257 publications
(206 citation statements)
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“…A statistical test of the hypothesis is a procedure which is used to find out whether we may "not reject" ("accept") the hypothesis, that is, act as though it is true, or whether we should "reject" it, that is, act as though it is false. This statistical test has a variety of applications for trend analysis [15], [19], [20].…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…A statistical test of the hypothesis is a procedure which is used to find out whether we may "not reject" ("accept") the hypothesis, that is, act as though it is true, or whether we should "reject" it, that is, act as though it is false. This statistical test has a variety of applications for trend analysis [15], [19], [20].…”
Section: Discussionmentioning
confidence: 99%
“…Hypothesis H0 -no trend is if (Z < Z α/2 ) and H1 -there is a trend if Z > Z α/2 . Moreover, the value of Z gives further information about any increasing or decreasing of the trend, but not its magnitude exactly [17], [20].…”
Section: Discussionmentioning
confidence: 99%
“…The slope of n pairs of data points was estimated using the Theil-Sen's estimator which is given by the equation (Santos et al 2010):…”
Section: Theil-sen's Estimatormentioning
confidence: 99%
“…The use of clustering techniques in spatial and temporal patterns in climatic and meteorological research increased in recent decades. For instance, Santos et al (2010) and Dinpashoh et al (2004) used an algorithm that combined clusters analysis and PCA for dividing the research region into climate subregions. Since time series of precipitation are dynamic, certain non-stationary or chaotic properties may be embedded in the data, requiring appropriate methods to extract the features of interest (Hsu and Li 2010).…”
Section: Introductionmentioning
confidence: 99%
“…To achieve the previous purpose one of the most common indexes, the Standardized Precipitation Index (SPI) [4], was selected due to its few data requirements, to the relatively simplicity of its computation when compared to other indices and to its comparability because it is a dimensionless index [5]- [7]. The SPI was designed to quantify the precipitation deficit at different time scales (from 1 to 24 months), which reflect the impact of droughts on the different types of reservoirs of fresh water at the watershed level -as the time scale increases, meteorological, agricultural, hydrological and the socio-economic droughts [8].…”
mentioning
confidence: 99%