The two-dimensional erosion of a vortex subjected to an external, adve
rse shear is studied experimentally. The flow takes place in a thin st
ratified layer; the vortex is produced by electromagnetic forcing, whe
reas the shear is driven mechanically. The system thus allows the vort
ex strength and the external shear to be controled independently. We o
bserve the so-called 'erosion' process, i.e. the progressive decrease
of the vortex area, leaving the vortex core unaffected. This process i
s controlled by the ratio gamma = S/omega(max), where omega(max) and S
are respectively the maximum vorticity of the vortex and the external
shear. At small gamma, the erosion is weak and the vortex survives ov
er the duration of the experiment. At large gamma, the vortex is first
eroded, and then, after a critical time, becomes stretched and eventu
ally breaks up into filaments. During the first period of time, the co
mpensated maximum vorticity (with friction decay removed) is constant
and the vortex area decreases, while beyond the critical time, both qu
antities decrease with time. A critical value for gamma, defining the
transition between these two regimes, is determined experimentally: ga
mma(c) = 0.051+/-0.017. The breaking process itself, during which the
vorticity of the vortex core decreases, is investigated. All the quali
tative aspects of the erosion process, the onset of breaking and the b
reaking process itself are found to be in excellent agreement with the
theoretical and numerical description. The experimental value of gamm
a(c) and the properties of the filamentation process are consistent wi
th the numerical estimates.