This research has been carried out to investigate the dynamics of synoptic patterns associated with deep tropopause folds in the southwest Asia in 2015 using the ERA-Interim reanalysis data. The tropopause folds are detected applying the Škerlak et al. (2014) algorithm and the mean of relevant meteorological fields in each grid point are computed in a 40 ° ×40 ° horizontal domain, centered at the position of tropopause fold. The results show that in the vicinity of tropopause fold, static stability decreases in the lower layers of the troposphere and a trough with a tilted axis along northeast-southwest is formed at higher levels. Also, precipitation occurs mainly in the downstream of tropopause fold, about 100 kilometers away, which seems to be related more likely to larger-scale trough.