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Abdelaaziz Merabti
École Normale Supérieure
3Publications
2H-index
6Citations
Publications 3
Newest
#1Abdelaaziz Merabti ('ENS Paris': École Normale Supérieure)H-Index: 2
#2Diogo S. Martins (University of Lisbon)H-Index: 6
Last.Luis S. Pereira (Instituto Superior de Agronomia)H-Index: 51
view all 4 authors...
Abstract Due to an oversight, Figure 1 image and Figure 4 caption were incorrectly captured in the original publication.
#1Abdelaaziz Merabti ('ENS Paris': École Normale Supérieure)H-Index: 2
#2Diogo S. Martins (University of Lisbon)H-Index: 6
Last.Luis S. Pereira (University of Lisbon)H-Index: 51
view all 4 authors...
The spatial and temporal variability of droughts were studied for the Northeast Algeria using SPI and RDI computed with monthly precipitation data from 123 rainfall stations and CFSR reanalysis monthly temperature data covering the period 1979–80 to 2013–14. The gridded temperature data was interpolated to all the locations having precipitation data, thus providing to compute SPI and RDI with the time scales of 3-, 6- and 12-month with the same observed rainfall data. Spatial and temporal patter...
#1Abdelaaziz Merabti ('ENS Paris': École Normale Supérieure)H-Index: 2
#2Hind Meddi ('ENS Paris': École Normale Supérieure)H-Index: 10
Last.Luis S. Pereira (Instituto Superior de Agronomia)H-Index: 51
view all 4 authors...
Drought and wetness events were studied in the Northeast Algeria with SPI and RDI. The study area includes a variety of climatic conditions, ranging from humid in the North, close to the Mediterranean Sea, to arid in the South, near the Sahara Desert. SPI only uses precipitation data while RDI uses a ratio between precipitation and potential evapotranspiration (PET). The latter was computed with the Thornthwaite equation, thus using temperature data only. Monthly precipitation data were obtained...
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