Journal of Water and Climate Change (May 2023)

Evaluation of PERSIANN-CCS-CDR, ERA5, and SM2RAIN-ASCAT rainfall products for rainfall and drought assessment in a semi-arid watershed, Morocco

  • Adam Najmi,
  • Brahim Igmoullan,
  • Mustapha Namous,
  • Imane El Bouazzaoui,
  • Yassine Ait Brahim,
  • El Mahdi El Khalki,
  • Mohamed El Mehdi Saidi

DOI
https://doi.org/10.2166/wcc.2023.461
Journal volume & issue
Vol. 14, no. 5
pp. 1569 – 1584

Abstract

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Satellite-based precipitation products, with simultaneously high spatial and temporal resolutions, are mostly needed to assess climate change repercussions. Previous research used datasets neglecting either good temporal or good spatial resolution, PERSIANN-CCSCDR, ERA5, and SM2RAIN-ASCAT are some of the projects aiming to remedy these limitations. This study's goal is to evaluate the accuracy of the PERSIANN-CCS-CDR, ERA5, and SM2RAIN-ASCAT at a monthly scale and their suitability for drought assessment in a Moroccan semiarid watershed. Several statistical indices were computed, the drought SPI was calculated using PERSIANN-CCS-CDR estimates, ERA5 products, and observed records as an input in the SPI formula using Gamma distribution to simulate drought from 1983 to 2017. The preliminary comparison and evaluation results of PERSIANN-CCS-CDR estimates and ERA5 datasets showed good CC on a basin scale for monthly precipitation, with a slight overestimation of the observed precipitation shown by the PBIAS. The NSE scored 0.41 for PERSIANN-CCS-CDR and 0.72 for ERA5. The results for SM2RAIN-ASCAT showed an overestimation of the observed precipitation data. At the basin scale, the SPI3 correlation coefficients between the PERSIANN-CCS-CDR monthly estimates and observed gauge rainfall data were greater than 0.67, and the RMSE was closer to 0, outperforming ERA5 in the SPI3 evaluation. HIGHLIGHTS The use of remotely sensed precipitation data for climatological and hydrological studies.; Evaluation of one of the rarest evaluated products (PERSIANN-CCS-CDR).; Recommendation for alternative precipitation datasets for areas lacking precipitation data.;

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