[guided]Fix a direction $\theta \in S_pM$. The goal along this single geodesic is to compare the actual polar volume density $J_p(t,\theta)$ with the model density $\operatorname{sn}_k(t)^{n-1}$. The correct quantity is their quotient, because the model space form has radial Jacobian exactly $\operatorname{sn}_k(t)^{n-1}$ in each direction.
Define
\begin{align*}
q_\theta:(0,c(\theta))\cap I_k &\to (0,\infty) \\
t &\mapsto \frac{J_p(t,\theta)}{\operatorname{sn}_k(t)^{n-1}}.
\end{align*}
We prove that $q_\theta$ is nonincreasing by differentiating its logarithm.
On the interval $(0,c(\theta))$, the point $\gamma_\theta(t)$ lies before the cut time, so the radial distance from $p$ is smooth along this ray and the polar-coordinate parametrization has no cut singularity in the direction $\theta$. This is precisely the setting in which the standard [first variation formula for the polar Jacobian](/page/First%20Variation%20Formula) and the [Riccati equation for geodesic spheres](/page/Riccati%20Equation) apply.
Let
\begin{align*}
S_\theta(t):\dot{\gamma}_\theta(t)^\perp &\to \dot{\gamma}_\theta(t)^\perp
\end{align*}
be the shape operator of the geodesic sphere centered at $p$ at $\gamma_\theta(t)$, with outward unit normal $\dot{\gamma}_\theta(t)$. Define
\begin{align*}
h_\theta:(0,c(\theta)) &\to \mathbb{R} \\
t &\mapsto \operatorname{tr} S_\theta(t).
\end{align*}
The polar Jacobian changes at the rate given by the mean curvature:
\begin{align*}
\frac{\partial}{\partial t}\log J_p(t,\theta)=h_\theta(t).
\end{align*}
The shape operator satisfies the Riccati equation along the radial geodesic:
\begin{align*}
h_\theta'(t)+\operatorname{tr}(S_\theta(t)^2)+\operatorname{Ric}_g(\dot{\gamma}_\theta(t),\dot{\gamma}_\theta(t))=0.
\end{align*}
Now we use exactly the two hypotheses that allow comparison. First, $S_\theta(t)$ is symmetric on an $(n-1)$-dimensional [inner product](/page/Inner%20Product) space, so Cauchy-Schwarz applied to its eigenvalues gives
\begin{align*}
\operatorname{tr}(S_\theta(t)^2)\geq \frac{h_\theta(t)^2}{n-1}.
\end{align*}
Second, the geodesic is unit-speed, so $g(\dot{\gamma}_\theta(t),\dot{\gamma}_\theta(t))=1$, and the Ricci lower bound gives
\begin{align*}
\operatorname{Ric}_g(\dot{\gamma}_\theta(t),\dot{\gamma}_\theta(t))\geq (n-1)k.
\end{align*}
Substituting these two inequalities into the Riccati equation yields
\begin{align*}
h_\theta'(t)+\frac{h_\theta(t)^2}{n-1}+(n-1)k \leq 0.
\end{align*}
The model comparison function is
\begin{align*}
h_k:I_k &\to \mathbb{R} \\
t &\mapsto (n-1)\frac{\operatorname{sn}_k'(t)}{\operatorname{sn}_k(t)}.
\end{align*}
Since $\operatorname{sn}_k''+k\operatorname{sn}_k=0$, direct differentiation gives
\begin{align*}
h_k'(t)+\frac{h_k(t)^2}{n-1}+(n-1)k=0.
\end{align*}
Thus $h_\theta$ is a subsolution of the scalar Riccati equation solved by $h_k$.
To compare the two, define
\begin{align*}
w_\theta:(0,c(\theta))\cap I_k &\to \mathbb{R} \\
t &\mapsto h_\theta(t)-h_k(t).
\end{align*}
Subtracting the equality for $h_k$ from the inequality for $h_\theta$ gives
\begin{align*}
w_\theta'(t)+\frac{h_\theta(t)+h_k(t)}{n-1}w_\theta(t)\leq 0.
\end{align*}
The singularity at $t=0$ is harmless because both actual and model polar densities have the same Euclidean first-order behavior:
\begin{align*}
J_p(t,\theta)=t^{n-1}(1+O(t^2)),
\qquad
\operatorname{sn}_k(t)^{n-1}=t^{n-1}(1+O(t^2)).
\end{align*}
Consequently
\begin{align*}
w_\theta(t)=O(t)
\end{align*}
as $t\downarrow 0$.
For $0<\varepsilon<t<c(\theta)$ with $t\in I_k$, multiply the differential inequality for $w_\theta$ by the positive integrating factor
\begin{align*}
E_{\varepsilon,t}
:=
\exp\left(
\int_\varepsilon^t
\frac{h_\theta(s)+h_k(s)}{n-1}\,d\mathcal{L}^1(s)
\right).
\end{align*}
This gives
\begin{align*}
w_\theta(t)E_{\varepsilon,t}\leq w_\theta(\varepsilon).
\end{align*}
We still have to justify the limit as $\varepsilon\downarrow 0$, because the integrating factor depends on $\varepsilon$. The same initial asymptotics imply
\begin{align*}
\frac{h_\theta(s)+h_k(s)}{n-1}=\frac{2}{s}+O(s)
\end{align*}
as $s\downarrow 0$. Therefore, for fixed $t$, there are constants $C_t>0$ and $\varepsilon_t>0$ such that
\begin{align*}
E_{\varepsilon,t}\geq C_t\varepsilon^{-2}
\end{align*}
whenever $0<\varepsilon<\varepsilon_t$. From
\begin{align*}
w_\theta(t)E_{\varepsilon,t}\leq w_\theta(\varepsilon)
\end{align*}
we get
\begin{align*}
w_\theta(t)\leq \frac{w_\theta(\varepsilon)}{E_{\varepsilon,t}}.
\end{align*}
Since $w_\theta(\varepsilon)=O(\varepsilon)$, the right-hand side is $O(\varepsilon^3)$ and tends to $0$. Therefore
\begin{align*}
h_\theta(t)\leq h_k(t)
\end{align*}
for every $t\in(0,c(\theta))\cap I_k$.
Now differentiate the logarithm of the quotient:
\begin{align*}
\frac{\partial}{\partial t}\log q_\theta(t)
&=
\frac{\partial}{\partial t}\log J_p(t,\theta)
-
(n-1)\frac{\operatorname{sn}_k'(t)}{\operatorname{sn}_k(t)} \\
&=
h_\theta(t)-h_k(t) \\
&\leq 0.
\end{align*}
Since $q_\theta(t)>0$, the inequality for the logarithmic derivative proves that $q_\theta$ is nonincreasing along the radial geodesic before the cut time.[/guided]