I apologize in advance if this is a silly question, or if it is well-known to people studying Riemannian geometry.
In the context of Riemannian submersions, it is possible to relate the scalar curvature of the two manifolds (in particular, I refer to corollary 9.37 of Besse's book "Einstein manifolds").
I would like to know if something similar also holds for Riemannian immersions. For instance, is it possible to relate the scalar curvature of the 2-sphere with the (vanishing) scalar curvature of the ambient space (for instance using something like the second fundamental form or something similar)?
EDIT
I realize it is better if a give some other details.
The case I am interested in is the following: $N=P\times SU(n)$ where $P=\{\mathbf{x}\in\mathbb{R}^{n}:x^{1}>x^{2}>....>x^{n}>0\}$ with $(x^{1},...,x^{n})$ is the natural Cartesian coordinate system in $\mathbb{R}^{n}$, and $M=f^{-1}(1)\cap N$ where $f(\mathbf{x},U)=\sum_{j}x^{j}$.
On the manifold $N$ there is the Riemannian metric $$ g=\sum_{j}\frac{\mathrm{d}x^{j}\otimes\mathrm{d}x^{j}}{x^{j}} + \sum_{k}G_{k}(\mathbf{x})\theta^{k}\otimes\theta^{k}, $$ where $\{\theta^{k}\}$ is a preferred system of left-invariant one forms on $SU(n)$ (or better, their pullback to $N$ with respect to the obvious projection map), and we endow $M$ with the Riemannian metric $h$ which is the pull-back of $g$ with respect to the canonical immersion $i: M\rightarrow N$.
There is a basis of globally-defined vector fields $\{\partial_{x^{j}},X_{k}\}$ on $N$, where the $X_{k}$'s are tangent to $SU(n)$ and are dual to the $\theta^{k}$'s, and there is a basis of globally-defined differential forms $\{\mathrm{d}x^{j},\theta^{k}\}$.
Clearly, using the pullback with respect to the inclusion map, we can still use $\{\mathrm{d}x^{j},\theta^{k}\}$ as an overcomplete basis of differential forms on $M$, and it is clear that $h$ "looks" exactly the same using this basis. Regarding vector fields, by setting $Y_{j}=\partial_{x^{j}} - \sum_{l}x^{l}\partial_{x^{l}}$, we obtain an overcomplete basis $\{Y_{j},X_{k}\}$ of vector fields.
The situation is similar to that of the unit 2-sphere in $\mathbb{R}^{3}$ where the overcomplete basis of globally-defined vector fields is obtained by considering the restriction to the 2-sphere of the fundamental vector fields of the standard action of $SO(3)$ on $\mathbb{R}^{3}$ having the unit 2-sphere as an orbit, while the overcomplete basis of globally-defined differential forms is obtained considering the pull-back of the $\mathrm{d}x^{j}$ to the sphere, with $(x^{1},x^{2},x^{3})$ a Cartesian coordinate system on $\mathbb{R}^{3}$.
I want to compute the scalar curvature of $(M,h)$. It can be computed in terms of an orthogonal basis of tangent vectors at each point of $M$, but I am not able to do it because I was not able to quickly find such a basis. Therefore, I thought I could do it using the overcomplete basis introduced before, but up to now I failed. I realized that the difficulty I face boils down, essentially, to the fact that for computing the Ricci tensor and the scalar curvature I need to take the trace of something, and taking a trace requires choosing a basis, and can not be done using an overcomplete basis.
This made me wonder if, for a Riemannian immersion as the one described above, it is possible to define the Ricci tensor and the scalar curvature using an overcomplete basis of vector fields defined in terms of vector fields on the ambient manifold.
If you have read up to now, I thank you for the patience, and I welcome any hint.