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- $\begingroup$ It would help folks if you wrote out the optimization problem you're solving, the gradient, as well as the error distribution (and how they're combined) contributing to the gradient in both the approx and non-approx forms. $\endgroup$Mark L. Stone– Mark L. Stone2016-09-13 18:10:50 +00:00Commented Sep 13, 2016 at 18:10
- $\begingroup$ @MarkL.Stone thanks. Are you asking me to revise the question? or giving me clues to the answer of my question. $\endgroup$HXD– HXD2016-09-13 18:13:29 +00:00Commented Sep 13, 2016 at 18:13
- $\begingroup$ Suggesting you edit question to make math clear without going through code. I have lots of hints, but am busy, so will probably leave answer to others. $\endgroup$Mark L. Stone– Mark L. Stone2016-09-13 18:15:53 +00:00Commented Sep 13, 2016 at 18:15
- $\begingroup$ @hxd1011 another thing to note is that for SGD you are updating the residual $r=Ax-b$ every time you update $x$ over the SGD epoch, so SGD explores different gradients on the curved error surface. In this way, SGD vs. BGD is reminiscent of Gauss-Seidel vs. Jacobi iteration, two basic iterative methods for linear systems. When applied to the normal equations in your linear LSQR case, this comparison may be exact ($\Delta x$ update directions for SGD=Gauss-Seidel and for BGD=Jacobi). This is discussed in sec 8.2 of this book. $\endgroup$GeoMatt22– GeoMatt222016-09-13 22:52:46 +00:00Commented Sep 13, 2016 at 22:52
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