A simplified procedure is through its meridian (of its surface of revolution). We set $u=0$ in its parametrization ( what was there before rotation).
$$ y= \sin v, z= \cos v+\log (\tan {v/2}) $$
I prefer to linearly dimension the co-ordinates:
$$ y= a \sin v, z= a( \cos v+\log (\tan {v/2})) \tag1 $$
$$\dfrac{dy}{dz}=\dfrac{dy/dv}{dz/dv}= \dfrac
{a \cos v }{a(-\sin v + \csc v )}=-\tan v = \tan \phi $$
Thus slope of meridian is $ \; v = -\phi$
Principal curvature are $$ \quad k_2= \dfrac{\cos \phi }{y}= \dfrac{\cot v}{a} $$
$$k_1=\dfrac{d\phi}{ds} = \dfrac{-dv}{dy/\sin \phi}=\dfrac{ -\sin v \;d(\sin^{-1}y)}{dy}=\dfrac{-\sin v}{a \cos v} =\dfrac{-\tan v}{a}$$
Gauss curvature product is a negative constant
$$k_1 k_2= -1/a^2$$
where $a$ is the maximum torsion radius of pseudosphere.
From (1) $ \dfrac{y}{\sin \phi} =a $ represents constant tangent length upto axis, a property of the Tractrix.