Abstract

Analysis of spatial and temporal drought variability in the upper Tana River basin using Palmer Drought Severity Index (PDSI) was conducted. The drought is critical for formulation of mitigation measures in the river basin. A monthly temporal and 90-m spatial resolution was applied. This was achieved within ArcGIS environment. Climatic data for 1970 to 2010 was used for computation of the PDSI while the missing data sets were filled using Artificial Neural Networks (ANNs). The results of PDSI for dry and wet seasons at meteorological stations indicate that the time series plots for the PDSI values for dry season are generally lower than those for the wet seasons. The PDSI values for meteorological stations located at the lower elevation of the basin are lower than those located at higher elevation. On the other hand, spatially distributed drought severity based on PDSI show that the ranges of maximum and minimum drought severity values in 1970 are -0.868 to -0.804 and -0.675 to -0.610 respectively. These values of drought severity occur respectively in the north-western and south-eastern areas of the basin. PDSI values increased from the range -0.675 to -0.610 in 1970 and from -1.087 to 0.957 in 2010 for the north-eastern areas of the upper basin. The south eastern areas of the basin are more prone to drought risks than north-western parts. Use of the PDSI reflects the spatial heterogeneity and temporal variability of drought across the basin. The drought assessment offer technical approach for comprehensive understanding of drought for effective drought-induced disaster mitigation and its management, with a view to reducing adverse effects on livelihoods. Key words: Palmer Drought Severity Index (PDSI), drought severity, upper Tana River basin, monthly resolution, drought-induced disaster.

Highlights

  • Drought is a condition on land characterised by scarcity of water that falls below a defined threshold level

  • The results of spatially distributed drought severity based on Palmer Drought Severity Index (PDSI) show that the ranges of maximum and minimum drought severity values in 1970 are -0.868 to -0.804 and 0.675 to -0.610, respectively

  • From the results of spatially distributed drought magnitude, it can be seen that there is a general increase in area under the extreme and severe drought as given by PDSI from 1970 to 2010

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Summary

Introduction

Drought is a condition on land characterised by scarcity of water that falls below a defined threshold level. The term drought has been defined differently in numerous applications (UNDP, 2012). Drought may be defined differently depending on the sector involved. A hydrological-drought occurs whenever river or groundwater levels are relatively low. Water-resources drought occurs when basins experience low stream flow, reduced water reservoir volume and groundwater levels. The water resources drought is influenced by climatic and hydrological parameters within a river basin and drought management practices. The hydrological drought, mainly deals with low stream flows. This drought adversely affects various aspects of human interest such as food security, water supply and hydropower generation (Karamouz et al, 2009; Belayneh and Adamowski, 2013)

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