Abstract

For many regions of the world, current climate change projections are only available at coarser spatial resolution from Global Climate Models (GCMs) that cannot directly be used in impact assessment and adaptation studies at regional and local scale. Impact assessment studies require high-resolution climate data to drive impact assessment models. To overcome this data challenge, we produced a station based climate projection (precipitation and maximum and minimum temperature) for Ethiopia, Kenya, and Tanzania using observed daily data from 211 stations obtained from the National Meteorological Agency of Ethiopia and international databases. Moreover, 26 large-scale climate variables derived from the National Centers for Environmental Prediction reanalysis data (1961–2005) and second generation Canadian Earth System Model (CanESM2, 1961–2100) are used. Statistical Down-Scaling Model (SDSM) is used to produce the required high-resolution climate projection by developing a statistical relationship between the large- and local-scale climate variables. The predictors are analysed more than 16458 times and we provided 20 ensembles for the current (1961–2005) and future (2006–2100, under RCP2.6, RCP4.5, and RCP8.5) climate.

Highlights

  • Background & SummaryLarge-scale or global climate models are currently used to advance the scientific knowledge and understanding variabilities and changes in large-scale climate variables[1]

  • Evaluation of the model output for both precipitation and maximum and minimum temperature is carried out using the observed data for each station

  • The predictors derived from CanESM2 and the NCEP reanalysis data[32] are exported into Statistical Down Scaling Model (SDSM) directory for model calibration and projection

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Summary

Background & Summary

Large-scale or global climate models are currently used to advance the scientific knowledge and understanding variabilities and changes in large-scale climate variables[1]. Considering the observed changes and vulnerability of the region to variability (e.g., seasonal rainfall variability) and changes in climate and climate extremes[22,23] conducting in-depth impact assessment studies at local and regional scale is required to minimize or mitigate impacts in the future through sustainable adaptation measures. This type of information is not readily available and producing station based climate projections using SDSM requires observed data with high quality for model calibration and as input to the scenario generator, which is part of SDSM. The data can be used for impact assessment and adaptation studies in Ethiopia, Kenya, and Tanzania (Fig. 1)

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