In viscous withdrawal, a converging flow imposed in an upper layer of viscous liquid entrains liquid from a lower, stably stratified layer. Using the idea that a thin tendril is entrained by a local straining flow, we propose a scaling law for the volume flux of liquid entrained from miscible liquid layers. A long-wavelength model including only local information about the withdrawal flow is degenerate, with multiple tendril solutions for one withdrawal condition. Including information about the global geometry of the withdrawal flow removes the degeneracy while introducing only a logarithmic dependence on the global flow parameters into the scaling law.Recent experiments on thermal convection with two layers of miscible liquids reveal several distinct regimesan overturn regime with violent mixing of the layers, a doming regime where the interface undulates, and a stratified regime where the convection is largely stable with thin tendrils or sheets of one liquid entrained within the other [1]. Analogous steady-state entrained structures arise in drainage flows [2,3], oil extraction [4], as well as viscous withdrawal of immiscible liquid layers, which occur in microfluidics [5], fiber coating [6] and encapsulation of biological cells [7]. Recent works exploring the connections between thermodynamic phase transitions and the topology transition that takes place at the onset of entrainment have noted that, in order for the entrained structure to be completely isolated from the large-scale flow dynamics, the shape of its base must be a power-law cusp [2,8,9,10]. Intriguingly, experiments [11,12] on miscible entrainment also seem to show a robust cusp-like shape at the base of long-lived tendrils (see Fig. 1). This suggests the entrained tendrils are isolated from the fluctuating, large-scale convection by the cusp-shaped base and are therefore able to remain stable over many convection cycles. If true, this may even explain why hot-spots can persist over many convection cycles in the Earth's mantle [12,13]. Motivated by these observations, we focus on the stratified regime in thermal convection of miscible layers and present a model that tests how the large-scale flow and topography anchor a thin cylindrical tendril.Because the large-scale flow is stabilized in the stratified regime, mixing between the layers is controlled by the volume flux of liquid entrained through the tendrils, Q 0 . Existing estimates of Q 0 assume that the velocity field inside the tendril is uniformly upwards, flowing at a characteristic convection speed [11,12,14]. However, recent particle-image-velocimetry (PIV) measurements within the base of an anchored tendril reveal a stagnation-point velocity field, one more appropriately described by a characteristic strain rate E (s −1 ) instead of a characteristic velocity scale [15]. Viscous withdrawal experiments on immiscible layers suggest how an interior stagnation point can arise [8]. When the effect of the entrainment penetrates deeply into the lower layer, a broad tendril forms with the int...