The recovery of a signal from the intensity measurements with some entries being known in advance is termed as {\em affine phase retrieval}. In this paper, we prove that a natural least squares formulation for the affine phase retrieval is strongly convex on the entire space under some mild conditions, provided the measurements are complex Gaussian random vecotrs and the measurement number $m \gtrsim d \log d$ where $d$ is the dimension of signals. Based on the result, we prove that the simple gradient descent method for the affine phase retrieval converges linearly to the target solution with high probability from an arbitrary initial point. These results show an essential difference between the affine phase retrieval and the classical phase retrieval, where the least squares formulations for the classical phase retrieval are non-convex.
翻译:在本文中,我们证明,在某种温和条件下,从密集度测量中从某些预知的条目中恢复信号的自然最小正方形配方在一定条件下是整个空间的强烈锥体,条件是测量是复杂的高斯随机微粒体和测量编号为$m \gtrsim d\log d$,其中以美元为信号的维度。根据结果,我们证明,从一个任意的初始点看,简单梯度梯度下沉法从直线走向目标解决方案,概率很高。这些结果表明,毛线级回收和经典阶段检索之间存在根本差异,其中用于典型阶段检索的最小正方形配方是非曲线的。