“…A ray
in
is defined as the equivalent class of rays in the stratifications
for
. Since it is proved in [
11] that a quadratic differential
on S is Jenkins–Strebel if and only if its lifting differential
on
is Jenkins–Strebel, then the image of a Jenkins–Strebel ray r in
under the isometric embedding
is still Jenkins–Strebel in
. We call a ray in
Jenkins–Strebel if it is the equivalent class of the Jenkins—Strebel rays in the stratifications
…”