Drought analysis in Europe and in the Mediterranean basin using the standardized precipitation index

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Abstract

In this study, drought events over a large area of the Northern Hemisphere, including continental Europe, Ireland, the United Kingdom, and the Mediterranean basin, were analyzed using the Standardized Precipitation Index (SPI) at various times scales (3, 6, 12, and 24 months). To this purpose, the Global Precipitation Climatology Centre (GPCC) Full Data Monthly Product Version 2018 data set, with spatial resolutions of 0.5° longitude/latitude and for the period 1951-2016, has been used. First, the temporal evolution of the percentage of grid points, falling within the severe and extreme drought categories, has been evaluated. Then, a trend analysis has been performed at a seasonal scale, considering the autumn-winter and the spring-summer periods, and at an annual scale. The results of this paper highlight that the Mediterranean basin and North Africa are the most consistently vulnerable areas showing a general reduction in SPI values especially for the long time scale.

Figures

  • Table 1. Climate classification according to the Standardized Precipitation Index (SPI) values.
  • Figure 1. Mean annual rainfall distribution on the study area for the period 1951–2016.
  • Figure 2. Temporal evolution of the percentage of grid points which fell within severe or extreme dry conditions (Standardized Precipitation Index SPI < −1.5) for the period 1951–2016. (a) 3-month SPI; (b) 6-month SPI; (c) 12-month SPI, and (d) 24-month SPI.
  • Figure 3. Spatial distribution of the grid points presenting positive or negative rainfall trends (seasonal scale). The trend analysis has been conducted at a seasonal scale, considering the 3-month SPI values in February for winter, in May for spring, in August for summer, and in November for autumn. Colored squares indicate significant positive or negative trends while white squares refer to a non-significant trend.
  • Figure 4. Spatial distribution of the grid points presenting positive or negative rainfall trends (autumn-winter and spring-summer periods). Colored squares indicate significant positive or negative trends while white squares refer to a non-significant trend.
  • Figure 5. Spatial distribution of the grid points presenting positive or negative rainfall trends (annual scale). Colored squares indicate significant positive or negative trends while white squares refer to a non-significant trend.

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Caloiero, T., Veltri, S., Caloiero, P., & Frustaci, F. (2018). Drought analysis in Europe and in the Mediterranean basin using the standardized precipitation index. Water (Switzerland), 10(8). https://doi.org/10.3390/w10081043

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