We investigated pressure-induced changes in pyrochlore iridates ( \(A_2\hbox {Ir}_2\hbox {O}_7\) , \(A=\) Pr, Gd, Dy and Er) using Raman spectroscopy and X-ray diffraction. All four compounds exhibited a pressure-driven isostructural transition associated with the rearrangement of \(\hbox {IrO}_6\) octahedra in the pyrochlore lattice. Interestingly, the critical pressure ( \(P_\textrm{c}\) ) for this transition correlates inversely with the A-site cation radius, \(P_\textrm{c}\) decreased from \(\sim \) 10.8 GPa (Er, smallest cation) to \(\sim \) 7.5 GPa (Pr, largest cation). Additionally, the bulk modulus systematically decreases with increasing ionic radius of A-site across the \(A_2\hbox {Ir}_2\hbox {O}_7\) series. High-pressure Raman spectroscopy revealed anomalous decrease of the linewidth with increasing pressure for Ir–O ( \(T_{2g}^{4}\) ) and Ir–O–Ir ( \(A_{1g}\) and \(E_g\) ) vibrational modes, suggesting a suppression of electron–phonon coupling due to enhanced electronic bandwidth under pressure.