Abstract

Future global warming may result in extreme precipitation events leading to crop, environment and infrastructure damage. Rainfall is a major input for the livelihood of peasant farmers in the Aswa catchment where the future rainfall variability, onset and cessation are also likely to be affected. The Aswa catchment has limited rainfall data; therefore, use of secondary datasets from Tropical Rainfall Measuring Mission (TRMM) is considered in this study, based on the close correlation of the recorded and TRMM rainfall. The latter was used to calibrate the statistical downscaling model for downscaling of two general circulation models to simulate future changes in rainfall. These data were analyzed for trends, wet and dry conditions/variability; onset and cessations of rain using the Mann–Kendall test, Standardized Precipitation Index (SPI) and the cumulative percentage mean rainfall method, respectively. Results show future rainfall is likely to increase, accompanied by increasing variability reaching as high as 118.5%. The frequency of SPI values above 2 (extreme wetness) is to increase above current level during mid and end of the century. The highest rainfall variability is expected especially during the onset and cessation months, which are generally expected to come earlier and later, by up to four and five weeks, respectively. The reliability worsens from the midterm (2036–2065) to long term (2066–2099). These likely changes in rainfall quantities, variability, onset and cessation months are some of the key rainfall dynamics that have implications for future arable agriculture, environment and water resource availability and planning over the Aswa catchment, as is increasingly the case elsewhere.

Highlights

  • Projected future global warming may result in extreme precipitation events causing drought and flooding, which in turn may result in crop yield reduction, increased soil erosion and damage to infrastructure [1,2,3,4,5]

  • Fishman [12] argues that an increase in rainfall variability amidst increased annual rainfall overrules the benefit expected from the increase on crop yields

  • We examined the future changes in rainfall patterns, trends, extreme occurrences, onset and cessation of rainfall over Aswa catchment using Standardized Precipitation Index (SPI), Mann–Kendall statistics, descriptive statistics, and cumulative percentage mean rainfall methods to provide insight into near future (2006–2035), midterm (2036–2065) and long term (2066–2100) future periods

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Summary

Introduction

Projected future global warming may result in extreme precipitation events causing drought and flooding, which in turn may result in crop yield reduction, increased soil erosion and damage to infrastructure [1,2,3,4,5]. Indicates that global warming above pre-industrial levels (1900) of 1.5 ◦ C and beyond would have adverse impacts on communities that depend on agriculture in the least developed countries. Rainfall is key to livelihoods of peasant farmers who depend on rain fed agriculture [7,8,9,10,11]. Fishman [12] argues that an increase in rainfall variability amidst increased annual rainfall overrules the benefit expected from the increase on crop yields.

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