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L.R. Schuurman
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In Ethiopia, rainfall variability and changes in rainfall patterns, induced by climate change, could increase the frequency and occurrence of floods and droughts. Due to smallholder farmers in the Gumera sub-basin, Ethiopia, mostly relying on rainfed agriculture, climatic changes highly influence the agricultural production with corresponding negative effects on food security and their economic well-being. To reduce their vulnerability to climate variability, the majority of smallholder farmers take up adaptation strategies, whereas a small group of farmers does not have the capacity to adapt. However, the understanding of what factors drive the climate adaptive capacity of farmers and how climate adaptive behaviour influences a farmer’s economic well-being is limited. Therefore, via a bottom-up approach, this study aims to determine what factors drive the climate adaptive capacity of smallholder farmers in the Gumera sub-basin and how they adapt to climate variability. Focus Group Discussions are conducted prior to an individual household survey to obtain local-level knowledge and data on the characteristics of smallholder farmers. Subsequently, this data is used to develop a methodology to incorporate the climate adaptive behaviour of smallholder farmers in socio-hydrological modelling. By implementing a logit model, the (dynamic) adaptive capacity of smallholder farmers is implemented, which provides the opportunity to create a better understanding of why farmers adapt to climate variability and its impact on their economic well-being. From the Focus Group Discussions and the individual household survey it is observed that the majority of farmers adapt to climate variability in case of a bad year, defined as a drought, by changing to a short cycle crop, mostly potato, and adjusting the planting and harvesting dates. The drivers that are found to mainly influence the uptake of these adaptation strategies are farm size, altitude, level of education, the number of livestock owned, capital, experience, access to a weather forecast, and labour availability. A small group of farmers does not take up adaptation strategies instead. First of all, their adaptive capacity is constrained by a lack of land, labour, and a weather forecast. Secondly, the rather optimistic perception of non-adapting farmers towards climate change seems to limit their adaptive capacity. Thirdly, especially the limited use of the onset of rains by non-adapting farmers was observed to negatively influence their climate adaptive capacity. Incorporating the climate adaptive behaviour of smallholder farmers in socio-hydrological modelling by enabling a logit model showed to be a successful approach. Based on the main drivers for the climate adaptive capacity, the model is able to simulate the agricultural practices with respect to climate variability. As such, the model has shown to be able to simulate agricultural practices that better coincide with what is observed during both the Focus Group Discussions and the household survey. In addition, the methodology used to evaluate the long-term effect of climate adaptation on the economic well-being of a farmer has the potential to help in creating a better understanding of why farmers adapt to climate variability.
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In Ethiopia, rainfall variability and changes in rainfall patterns, induced by climate change, could increase the frequency and occurrence of floods and droughts. Due to smallholder farmers in the Gumera sub-basin, Ethiopia, mostly relying on rainfed agriculture, climatic changes highly influence the agricultural production with corresponding negative effects on food security and their economic well-being. To reduce their vulnerability to climate variability, the majority of smallholder farmers take up adaptation strategies, whereas a small group of farmers does not have the capacity to adapt. However, the understanding of what factors drive the climate adaptive capacity of farmers and how climate adaptive behaviour influences a farmer’s economic well-being is limited. Therefore, via a bottom-up approach, this study aims to determine what factors drive the climate adaptive capacity of smallholder farmers in the Gumera sub-basin and how they adapt to climate variability. Focus Group Discussions are conducted prior to an individual household survey to obtain local-level knowledge and data on the characteristics of smallholder farmers. Subsequently, this data is used to develop a methodology to incorporate the climate adaptive behaviour of smallholder farmers in socio-hydrological modelling. By implementing a logit model, the (dynamic) adaptive capacity of smallholder farmers is implemented, which provides the opportunity to create a better understanding of why farmers adapt to climate variability and its impact on their economic well-being. From the Focus Group Discussions and the individual household survey it is observed that the majority of farmers adapt to climate variability in case of a bad year, defined as a drought, by changing to a short cycle crop, mostly potato, and adjusting the planting and harvesting dates. The drivers that are found to mainly influence the uptake of these adaptation strategies are farm size, altitude, level of education, the number of livestock owned, capital, experience, access to a weather forecast, and labour availability. A small group of farmers does not take up adaptation strategies instead. First of all, their adaptive capacity is constrained by a lack of land, labour, and a weather forecast. Secondly, the rather optimistic perception of non-adapting farmers towards climate change seems to limit their adaptive capacity. Thirdly, especially the limited use of the onset of rains by non-adapting farmers was observed to negatively influence their climate adaptive capacity. Incorporating the climate adaptive behaviour of smallholder farmers in socio-hydrological modelling by enabling a logit model showed to be a successful approach. Based on the main drivers for the climate adaptive capacity, the model is able to simulate the agricultural practices with respect to climate variability. As such, the model has shown to be able to simulate agricultural practices that better coincide with what is observed during both the Focus Group Discussions and the household survey. In addition, the methodology used to evaluate the long-term effect of climate adaptation on the economic well-being of a farmer has the potential to help in creating a better understanding of why farmers adapt to climate variability.
Student report
(2019)
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Ruben van Dijk, Ileen Streefkerk, Ludo Schuurman, Floris van 't Klooster, Julia Mc Gregor, Willem Luxemburg, Jules van Lier
This study investigates the many dynamics of the Manyame Catchment and comes up with recommendations on how to adapt or become more resilient to the risks at hand. The bad politics and forthcoming economic situation of Zimbabwe has led to instability and dramatic inflation over the last decade. This has resulted in a terrible investment climate, limited aid received from foreign countries and an outflow of educated population. Exploitation of water resources by industries, mines and urban centres located close to the rivers resulted in a decline in the quality and quantity of the environment. Especially the Manyame River Catchment, that supplies the capital Harare and flows north into the Zambezi, has been greatly affected. The catchment suffers from several pollution sources such as agriculture, mining, industrial dumps and wastewater inflow. Poor management and the deterioration of the drinking water supply and sanitation infrastructure has led to the recent outbreak of cholera. Although the Manyame Catchment has enough water, another main issue is the spatial distribution of its water resources. In some areas there are dams, but no farmers to utilize the water. In other areas farmers are desperate for water, but don’t receive any. The increasing dry spells due to climatic changes, has had disastrous effects for the non-irrigating smallholder farmers dependent on their maize production for survival, while floods created by the backwater curve from the Cahora Bassa Dam in the Lower Manyame sub-catchment have washed away the livestock, crops and infrastructure on the fertile areas in the flood plains. The situation stresses for better awareness, monitoring and guardance of the water resources. This will provide information for improvements in the planning, policy and management of water resources. Although the history of Zimbabwean governance would suggest it is purely acting on crisis management, proactive planning would be preferable to the alternative; to wait for the aquifers to dry up only for people to realize the real value of water.
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This study investigates the many dynamics of the Manyame Catchment and comes up with recommendations on how to adapt or become more resilient to the risks at hand. The bad politics and forthcoming economic situation of Zimbabwe has led to instability and dramatic inflation over the last decade. This has resulted in a terrible investment climate, limited aid received from foreign countries and an outflow of educated population. Exploitation of water resources by industries, mines and urban centres located close to the rivers resulted in a decline in the quality and quantity of the environment. Especially the Manyame River Catchment, that supplies the capital Harare and flows north into the Zambezi, has been greatly affected. The catchment suffers from several pollution sources such as agriculture, mining, industrial dumps and wastewater inflow. Poor management and the deterioration of the drinking water supply and sanitation infrastructure has led to the recent outbreak of cholera. Although the Manyame Catchment has enough water, another main issue is the spatial distribution of its water resources. In some areas there are dams, but no farmers to utilize the water. In other areas farmers are desperate for water, but don’t receive any. The increasing dry spells due to climatic changes, has had disastrous effects for the non-irrigating smallholder farmers dependent on their maize production for survival, while floods created by the backwater curve from the Cahora Bassa Dam in the Lower Manyame sub-catchment have washed away the livestock, crops and infrastructure on the fertile areas in the flood plains. The situation stresses for better awareness, monitoring and guardance of the water resources. This will provide information for improvements in the planning, policy and management of water resources. Although the history of Zimbabwean governance would suggest it is purely acting on crisis management, proactive planning would be preferable to the alternative; to wait for the aquifers to dry up only for people to realize the real value of water.