We study the instability of a laminar vortex column (in an external orthogo
nal strain field) to an axisymmetric core size perturbation, and the result
ing transition to fine-scale turbulence. The perturbation, which evolves as
a standing wave oscillation (i.e. core dynamics, CD), is inviscidly amplif
ied by the external strain. Analysis of a weakly strained Rankine vortex ex
plains the physical mechanism of instability: resonant interaction between
the perturbation - the azimuthal wavenumber m = 0 wave - and m = +/-2 waves
. The CD instability (CDI) - a type of elliptic instability - experiences t
he fastest growth when the CD oscillation frequency equals vortex column's
fluid angular velocity, such matching occurring only at specific discrete v
alues of the axial wavenumber k. At this resonant frequency, the net effect
of the swirl-induced tilting of perturbation vorticity and the CD-induced
tilting of base flow vorticity is such that perturbation vorticity is conti
nually aligned with the stretching direction of the external strain. Such s
train-vorticity locking occurs for all m; hence all waves are unstable, the
instability oscillation frequency being dependent on m. In a viscous Gauss
ian-like vortex, CDI has low-strain, low-Re and high-k cutoffs - consequenc
es of the competing effects of inviscid amplification and viscous damping.
Direct numerical simulation reveals two physical-space mechanisms of transi
tion: (i) formation of a thin annular vortex sheath surrounding a low-enstr
ophy 'bubble' (similar to axisymmetric vortex breakdown) and the sheath's s
ubsequent roll-up into smaller 'vortexlets'; and (ii) folding and reconnect
ion of core vortex filaments giving rise to additional fine-grained random
vorticity within the bubble -both mechanisms caused by CD-induced intense a
xial flow within the vortex column. The resulting finer tubular vortices (s
imilar to 'worms') have in turn their own CD, and thus this transition scen
ario suggests a physical-space cascade process in developed turbulence (as
well as a concomitant anti-cascade process during the bubble's collapse pha
se). Additionally, we show that bending waves, in spite of their faster gro
wth, effect surprisingly much slower transfer of energy into fine scales th
an CDI does, and hence are less effective than CDI in vortex transition and
in turbulence cascade.