One of the most important oscillations of the stratosphere is the quasi-biennial oscillation (QBO). The solar signal has a significant effect on the stratosphere and troposphere which is only revealed in climatic data by classification using QBO phases. It is thus important to investigate the mechanism of modulation of the QBO effects by the solar cycle in studying the extratropical effects of QBO in climatic data. In this study, the correlation between the 11-year solar cycle and the QBO phases is examined using JRA-55 reanalysis data from 1958 to 2018. Results show that the correlation of solar flux with temperature and geopotential height is strongest at the subtropical region. The location and amount of the correlations are different in different phases of QBO and in the easterly phase are stronger than the westerly one.