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Recent observations over the Arabian Peninsula reveal an apparent paradox: while the frequency of synoptically forced dust storms has declined since the late 1990s, mean near-surface dust concentrations, poor-visibility events, and chronic air-quality degradation have increased. This contrast is often attributed to changes in emissions or land use. Here, we propose instead that the paradox reflects an abrupt dynamical regime shift in large-scale circulation and boundary-layer ventilation. The Arabian Peninsula is strongly influenced by baroclinic disturbances generated by short-wavelength Rossby waves radiated from the subtropical jet stream (STJ). These disturbances drive deep vertical coupling, strong surface winds, and efficient ventilation of the boundary layer. Multiple independent diagnostics indicate that the regional circulation underwent an abrupt transition in the late 1990s, marked by increased static stability, increased pressure depth of the troposphere, a reduction in the squared meridional temperature gradient, and a corresponding decline in mean available potential energy. These changes are consistent with weakened Rossby wave radiation and reduced baroclinic activity downstream of the STJ.The consequences of this transition are twofold. First, reduced baroclinic activity suppresses deep convection, strong downdrafts, and synoptically driven high-wind events, leading to a decline in dust storm frequency. Second, and critically, weakened ageostrophic flow at the top of the boundary layer reduces shear-driven turbulence generation, particularly under stable boundary-layer conditions. The resulting collapse of vertical mixing limits ventilation and increases the residence time of dust near the surface, leading to higher mean surface concentrations despite fewer extreme dust events.This framework extends a dynamical theory previously developed to explain abrupt increases in fog under weakened baroclinic forcing to mineral dust and air quality. The results demonstrate that reduced ventilation alone is sufficient to reconcile declining dust storm frequency with increasing surface dust loading, highlighting the nonlinear sensitivity of boundary-layer processes to large-scale circulation changes. The findings underscore the importance of regime shifts in atmospheric dynamics for understanding long-term changes in dust, pollution, and visibility in arid regions.