Global climate has been changing and in fact expected to change in more shocking degree. Therefore, the objective of the current study is to understand climate change signal, downscale climate change scenario for Bale highlands using CORDEX_GCM Models and identify the occurrence of climate change signal in Bale highlands. This study was aimed to make in-depth statistical analysis on past and future climatic trend, rainfall patterns and temperature trends as well as changes for various time scales over Bale highlands. Climate data recorded at meteorological station located in Bale highlands were obtained from National Meteorological Agency Bale Robe Meteorological Branch Directorate while model output of the two RCP4.5 and RCP8.5 scenarios was downloaded from CORDEX Africa Group Data library. Various statistical techniques were employed on rainfall and temperature to analyze and interpret the past and future climatic condition for rainy season over the Bale highlands. The results revealed that the climate change signal was appear over Bale Highlands. The change in temperature over Bale highlands under RCP4.5 and RCP8.5 emission scenarios shown as an increase for the period of near century, mid-century and end century. Changes of temperature under RCP8.5 was higher than the change of temperature in RCP4.5 scenario for all three periods (near, mid and end Century). Rainfall change for near, mid and end centuries under RCPs scenarios were variable. From the IPCC Fourth Assessment Report [5] and Tadege [7] there is a general consensus on the rise of the temperature. Sayed [8] has shown that the change in rainfall over the Blue Nile basin would be between +2 and +11% for 2030, while rainfall over the White Nile basin would increase between 1 and 10% for the same year.Projections of future change from different climate models can result in large ranges of future change. There is a change in annual temperature and annual precipitation relative to 1986-2005 under different greenhouse gas emissions pathways for East Africa [4]. Under RCP 8.5, the average warming across all models shows temperature increment of approximately 4°C by the end of the century. When the range of projections from individual models is examined, some showed temperature increment approaching and exceeding 6°C by the same period. Under ambitious global greenhouse gas emission reductions (represented by RCP2.6) temperatures are expected to increase by approximately 1°C by the end of the century, however, even under this ambitious scenario increases in mean annual temperature above current conditions still approach 2°C [4].Regional differences in warming are modest, with warming associated with a greater frequency of heat waves and increases in evaporation leading to moisture deficits. Elshamy et al. [9] show a temperature increase over the upper Blue Nile of between 2°C and 5°C at the end of the 21 st Century under the A1B scenario compared to the period 1961-1990.