How does the existence of a unique geodesic in non-positive curvature follow from Cartan-Hadamard?

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Cartan-Hadamard states that a non-positively curved Riemannian manifold is covered by $\mathbb{R}^n$. How does it follow that in each homotopy class of paths from $x$ to $y$ there exists a unique geodesic?

I already know that geodesics minimise lengths locally and that the geodesics given by exp$(tv)$ are globally length minimising. Does it follow that any geodesic is of this form?