The second fundamental form (which I usually write II and pronounce “two”, but here will write $Q$) is defined for an immersed hypersurface in a Riemannian manifold; frequently the case of interest is a geodesic sphere. If $\nu$ denotes the (outward) unit normal to immersed hypersurface $M^{n-1} \subset (N^n, g)$ and $eta$ denotes its metric dual, then $$Q(X,Y) := g(\nabla_X \nu, Y).$$ Complete $\nu$ to a frame $e_1, \ldots, e_{n-1}, e_n := \nu$ around a point of $M$ with coframe $\omega^1, \ldots, \omega^n := \eta$. Then $\nabla_{e_i} \nu = h_{ij} \omega^j$ for some $h_{ij}$ and we accordingly define on forms that $$Q(\alpha) = h_{ij} e(\omega^i)e^*(\omega^j) \alpha.$$ The second fundamental form is symmetric, hence diagonalizable; frequently we like to write it in this diagonal form $$Q(\alpha) = \sum_{i=1}^{n-1} \lambda_i e(\omega^i) e^*(\omega^i) \alpha.$$

The mean curvature is a scalar-valued function on $M$ defined as $H = \sum h_{ii}$; that is, $H$ is the trace of $Q$. One important place where the trace arises is in $$Q \mathrm{vol} = H \mathrm{vol},$$ used in the (Stern–di Cerbo) global computation of Price monotonicity, for example.