Linear regression with multiple variables is also known as “multivariate linear regression”.
We now introduce notation for equations where we can have any number of input variables.
The multivariable form of the hypothesis function accommodating these multiple features is as follows:
hθ(x)=θ0+θ1x1+θ2x2+θ3x3+⋯+θnxn h θ ( x ) = θ 0 + θ 1 x 1 + θ 2 x 2 + θ 3 x 3 + ⋯ + θ n x n
In order to develop intuition about this function, we can think about θ0 θ 0 as the basic price of a house, θ1 θ 1 as the price per square meter, θ2 θ 2 as the price per floor, etc. x1 x 1 will be the number of square meters in the house, x2 x 2 the number of floors, etc.
Using the definition of matrix multiplication, our multivariable hypothesis function can be concisely represented as:
This is a vectorization of our hypothesis function for one training example; see the lessons on vectorization to learn more.
Remark: Note that for convenience reasons in this course we assume x(i)0=1 for (i∈1,…,m) x 0 ( i ) = 1 for ( i ∈ 1 , … , m ) . This allows us to do matrix operations with theta and x x . Hence making the two vectors ‘θ θ ’ and x(i) x ( i ) match each other element-wise (that is, have the same number of elements: n+1).]
The gradient descent equation itself is generally the same form; we just have to repeat it for our ‘n’ features:
In other words:
The following image compares gradient descent with one variable to gradient descent with multiple variables:
We can speed up gradient descent by having each of our input values in roughly the same range. This is because θ will descend quickly on small ranges and slowly on large ranges, and so will oscillate inefficiently down to the optimum when the variables are very uneven.
The way to prevent this is to modify the ranges of our input variables so that they are all roughly the same. Ideally:
−1≤x(i)≤1 − 1 ≤ x ( i ) ≤ 1 or −0.5≤x(i) − 0.5 ≤ x ( i )
These aren’t exact requirements; we are only trying to speed things up. The goal is to get all input variables into roughly one of these ranges, give or take a few.
Two techniques to help with this are feature scaling and mean normalization. Feature scaling involves dividing the input values by the range (i.e. the maximum value minus the minimum value) of the input variable, resulting in a new range of just 1. Mean normalization involves subtracting the average value for an input variable from the values for that input variable resulting in a new average value for the input variable of just zero. To implement both of these techniques, adjust your input values as shown in this formula:
xi:=xi−μisi x i := x i − μ i s i
Where μi μ i is the average of all the values for feature (i) and si s i is the range of values (max - min), or si s i is the standard deviation.
Note that dividing by the range, or dividing by the standard deviation, give different results. The quizzes in this course use range - the programming exercises use standard deviation.
For example, if xi x i represents housing prices with a range of 100 to 2000 and a mean value of 1000, then, xi:=price−10001900 x i := p r i c e − 1000 1900 .
Debugging gradient descent. Make a plot with number of iterations on the x-axis. Now plot the cost function, J(θ) over the number of iterations of gradient descent. If J(θ) ever increases, then you probably need to decrease α.
Automatic convergence test. Declare convergence if J(θ) decreases by less than E in one iteration, where E is some small value such as 10−3 10 − 3 . However in practice it’s difficult to choose this threshold value.
It has been proven that if learning rate α is sufficiently small, then J(θ) will decrease on every iteration.
To summarize:
If α α is too small: slow convergence.
If α α is too large: may not decrease on every iteration and thus may not converge.
We can improve our features and the form of our hypothesis function in a couple different ways.
We can combine multiple features into one. For example, we can combine x1 x 1 and x2 x 2 into a new feature x3 x 3 by taking x1⋅x2 x 1 ⋅ x 2 .
Polynomial Regression
Our hypothesis function need not be linear (a straight line) if that does not fit the data well.
We can change the behavior or curve of our hypothesis function by making it a quadratic, cubic or square root function (or any other form).
For example, if our hypothesis function is hθ(x)=θ0+θ1x1 h θ ( x ) = θ 0 + θ 1 x 1 then we can create additional features based on x1 x 1 , to get the quadratic function hθ(x)=θ0+θ1x1+θ2x21 h θ ( x ) = θ 0 + θ 1 x 1 + θ 2 x 1 2 or the cubic function hθ(x)=θ0+θ1x1+θ2x21+θ3x31 h θ ( x ) = θ 0 + θ 1 x 1 + θ 2 x 1 2 + θ 3 x 1 3
In the cubic version, we have created new features x2 x 2 and x3 x 3 where x2=x21 x 2 = x 1 2 and x3=x31 x 3 = x 1 3 .
To make it a square root function, we could do: hθ(x)=θ0+θ1x1+θ2x1−−√ h θ ( x ) = θ 0 + θ 1 x 1 + θ 2 x 1
One important thing to keep in mind is, if you choose your features this way then feature scaling becomes very important.
eg. if x1 x 1 has range 1 - 1000 then range of x21 x 1 2 becomes 1 - 1000000 and that of x31 x 1 3 becomes 1 - 1000000000.