I've actually been struggling against this for like 2 months now. What is it that makes these different?
hypotheses= X * theta
temp=(hypotheses-y)'
temp=X(:,1) * temp
temp=temp * (1 / m)
temp=temp * alpha
theta(1)=theta(1)-temp
hypotheses= X * theta
temp=(hypotheses-y)'
temp=temp * (1 / m)
temp=temp * alpha
theta(2)=theta(2)-temp
theta(1) = theta(1) - alpha * (1/m) * ((X * theta) - y)' * X(:, 1);
theta(2) = theta(2) - alpha * (1/m) * ((X * theta) - y)' * X(:, 2);
The latter works. I'm just not sure why..I struggle to understand the need for the matrix inverse .
Basically you add a vector of ones to x to vectorize the intercept. You can update a 2x1 matrix of thetas in one line of code. With x concatenate a vector of ones making it a nx2 matrix then you can calculate h(x) by multiplying by the theta vector (2x1), this is (X * theta) bit.
How to calculate Gradient Descent? In order to find the gradient of the function with respect to x dimension, take the derivative of the function with respect to x , then substitute the x-coordinate of the point of interest in for the x values in the derivative.
Gradient descent is an optimization algorithm which is commonly-used to train machine learning models and neural networks. Training data helps these models learn over time, and the cost function within gradient descent specifically acts as a barometer, gauging its accuracy with each iteration of parameter updates.
What you're doing in the first example in the second block you've missed out a step haven't you? I am assuming you concatenated X with a vector of ones.
temp=X(:,2) * temp
The last example will work but can be vectorized even more to be more simple and efficient.
I've assumed you only have 1 feature. it will work the same with multiple features since all that happens is you add an extra column to your X matrix for each feature. Basically you add a vector of ones to x to vectorize the intercept.
You can update a 2x1 matrix of thetas in one line of code. With x concatenate a vector of ones making it a nx2 matrix then you can calculate h(x) by multiplying by the theta vector (2x1), this is (X * theta) bit.
The second part of the vectorization is to transpose (X * theta) - y) which gives you a 1*n matrix which when multiplied by X (an n*2 matrix) will basically aggregate both (h(x)-y)x0 and (h(x)-y)x1. By definition both thetas are done at the same time. This results in a 1*2 matrix of my new theta's which I just transpose again to flip around the vector to be the same dimensions as the theta vector. I can then do a simple scalar multiplication by alpha and vector subtraction with theta.
X = data(:, 1); y = data(:, 2); m = length(y); X = [ones(m, 1), data(:,1)]; theta = zeros(2, 1); iterations = 2000; alpha = 0.001; for iter = 1:iterations theta = theta -((1/m) * ((X * theta) - y)' * X)' * alpha; end
In the first one, if X were a 3x2 matrix and theta were a 2x1 matrix, then "hypotheses" would be a 3x1 matrix.
Assuming y is a 3x1 matrix, then you can perform (hypotheses - y) and get a 3x1 matrix, then the transpose of that 3x1 is a 1x3 matrix assigned to temp.
Then the 1x3 matrix is set to theta(2), but this should not be a matrix.
The last two lines of your code works because, using my mxn examples above,
(X * theta)
would be a 3x1 matrix.
Then that 3x1 matrix is subtracted by y (a 3x1 matrix) and the result is a 3x1 matrix.
(X * theta) - y
So the transpose of the 3x1 matrix is a 1x3 matrix.
((X * theta) - y)'
Finally, a 1x3 matrix times a 3x1 matrix will equal a scalar or 1x1 matrix, which is what you are looking for. I'm sure you knew already, but just to be thorough, the X(:,2) is the second column of the 3x2 matrix, making it a 3x1 matrix.
function [theta, J_history] = gradientDescent(X, y, theta, alpha, num_iters)
% Performs gradient descent to learn theta. Updates theta by taking num_iters
% gradient steps with learning rate alpha.
% Number of training examples
m = length(y);
% Save the cost J in every iteration in order to plot J vs. num_iters and check for convergence
J_history = zeros(num_iters, 1);
for iter = 1:num_iters
h = X * theta;
stderr = h - y;
theta = theta - (alpha/m) * (stderr' * X)';
J_history(iter) = computeCost(X, y, theta);
end
end
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