Abstract

This paper discusses the preliminary results of meteorological drought analysis over Saudi Arabia for the period 1978–2017. In conjunction with meteorological observations, datasets from the Climate Prediction Center (CPC), the Merged Analysis of Precipitation (CMAP), the Climatic Research Unit (CRU), and the Tropical Rainfall Measuring Mission (TRMM) are utilized to understand the impact of the spatial distribution of rainfall on drought events. Applying precipitation thresholds allows rainfall classifications such as deficit, scanty, and surplus. Precipitation thresholds are also used to define meteorological droughts in the country, which are categorized as usual, moderate, and severe. It is found that drought events occur in Saudi Arabia due to shortfalls in the dry season, even though there is above normal rainfall in the wet season. There is no case of a shortfall in both the wet and dry seasons causing drought. Saudi Arabian droughts of all categories occurred mostly in the dry season, with fewer in the wet season. Results show that in Saudi Arabia, the last month of the wet season (April) is less prone to drought while the first and last months of the dry season (June and September respectively) are more prone to drought. Spatial distribution of drought climatology is obtained by calculating the Standardized Precipitation Index (SPI) and the Palmer Drought Severity Index (PDSI). Further application-driven studies of projections are needed based on drought indices and climate model output.

Highlights

  • Drought is a recurrent characteristic feature of climate variability and is manifest by prolonged and continuous periods of dry weather along with an abnormal deficient of rainfall

  • We focus on meteorological drought over Saudi Arabia by analyzing the observed rainfall and its distribution patterns

  • All rainfall categories in Saudi Arabia, at annual and seasonal scales for 1978–2017, are summarized in Table 2 taking into account the distribution of the 27 stations over years, i.e., 1080 (= 27 × 40) individual station points

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Summary

Introduction

Drought is a recurrent characteristic feature of climate variability and is manifest by prolonged and continuous periods of dry weather along with an abnormal deficient of rainfall. Droughts have significant impacts on the infrastructure, socio-economic activity, and the environment. They cause drying of the earth and water shortages, dry wells, depletion of groundwater and soil moisture, stream flow reduction, crop failure, and a lack of fodder for livestock. These impacts are severe on already semi-arid and arid regions In particular on Saudi Arabia, which covers. 80% of the Peninsula (Almazroui et al 2012a, 2012b).

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