Abstract

Droughts are one of the most serious threats to water availability, food security, and local livelihoods in the semi-arid areas of Tanzania. This paper adapted the participatory vulnerability assessment tools (causal effects, social mapping–resource mapping–social services–mobility–seasonality) to analyze the effects of prolonged droughts on semi-arid farming systems, community's vulnerability to drought effects, and the adopted coping strategies in six villages of Chamwino and Mwanga districts. Crop failure, loss of pasture, and drying of water sources were the common and major negative effects of droughts. Their consequences included food shortage and insecurity, water scarcity, and loss of livestock. The vulnerability to these effects was found to be driven by the social condition of households, resource ownership, and type of income sources. Those with good social conditions, relatively resourceful and deriving incomes from crop-livestock integration or non-agriculture, were less vulnerable and better placed to cope with the effects of droughts. Investments that build the productive resource base of a household and improve access to domestic and livestock water will contribute to long-term adaptive and drought-resilient systems in semi-arid areas of Tanzania.

Highlights

  • Frequent and prolonged droughts in the semi-arid areas of Tanzania are an expected phenomenon under current and future climate change and climate variability (Madaha, 2012; Mkonda and He, 2018; Haile et al, 2019)

  • The two districts are located in semi-arid areas of Tanzania which are affected by droughts

  • Crossborder labor migration during droughts was common in the three study villages of Chamwino and Kivisini in Mwanga

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Summary

Introduction

Frequent and prolonged droughts in the semi-arid areas of Tanzania are an expected phenomenon under current and future climate change and climate variability (Madaha, 2012; Mkonda and He, 2018; Haile et al, 2019). 50–70% of the semi-arid areas of Dodoma, Tanzania, are projected to experience high-temperature-induced maize and bean yield decreases due to increased evaporative demands of the land surface and reduced duration of crop growth (Thornton et al, 2009). The availability of freshwater has been predicted to drop by 50% by 2050 due to climate change, while water demand for agriculture could double during the same period (Gupta et al, 2020).

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