04_Linear_Regression_with_multiple

Linear regression with multiple features

New version of linear regression with multiple features

Multiple variables = multiple features
In original version we had
- X = house size, use this to predict
- y = house price
If in a new scheme we have more variables (such as number of bedrooms, number floors, age of the home)
- x₁, x₂, x₃,x₄are the four features
  - x₁ - size (feet squared)
  - x₂ - Number of bedrooms
  - x₃ - Number of floors
  - x₄ - Age of home (years)
- y is the output variable (price)
More notation
- n
  - number of features (n = 4)
- m
  - number of examples (i.e. number of rows in a table)
- xⁱ
  - vector of the input for an example (so a vector of the four parameters for the i^thinput example)
  - i is an index into the training set
  - So
    - x is an n-dimensional feature vector
    - x³ is, for example, the 3rd house, and contains the four features associated with that house
- x_jⁱ
  - The value of feature j in the ith training example
  - So
    - x₂³is, for example, the number of bedrooms in the third house
Now we have multiple features
- What is the form of our hypothesis?
- Previously our hypothesis took the form;
  - h_θ(x) = θ₀ + θ₁x
    - Here we have two parameters (theta 1 and theta 2) determined by our cost function
    - One variable x
- Now we have multiple features
  - h_θ(x) = θ₀ + θ₁x₁ + θ₂x₂ + θ₃x₃ + θ₄x₄
- For example
  - h_θ(x) = 80 + 0.1x₁ + 0.01x₂ + 3x₃ - 2x₄
    - An example of a hypothesis which is trying to predict the price of a house
    - Parameters are still determined through a cost function
- For convenience of notation, x₀ = 1
  - For every example i you have an additional 0th feature for each example
  - So now your feature vector is n + 1 dimensional feature vector indexed from 0
    - This is a column vector called x
    - Each example has a column vector associated with it
    - So let's say we have a new example called "X"
  - Parameters are also in a 0 indexed n+1 dimensional vector
    - This is also a column vector called θ
    - This vector is the same for each example
- Considering this, hypothesis can be written
  - h_θ(x) = θ₀x₀ + θ₁x₁ + θ₂x₂ + θ₃x₃ + θ₄x₄
- If we do
  - h_θ(x) =θ^T X
    - θ^Tis an [1 x n+1] matrix
    - In other words, because θis a column vector, the transposition operation transforms it into a row vector
    - So before
      - θwas a matrix [n + 1 x 1]
    - Now
      - θ^Tis a matrix [1 x n+1]
    - Which means the inner dimensions of θ^T and X match, so they can be multiplied together as
      - [1 x n+1] * [n+1 x 1]
      - = h_θ(x)
      - So, in other words, the transpose of our parameter vector * an input example X gives you a predicted hypothesis which is [1 x 1] dimensions (i.e. a single value)
  - This x₀ = 1 lets us write this like this
- This is an example of multivariate linear regression

Gradient descent for multiple variables

Fitting parameters for the hypothesis with gradient descent
- Parameters are θ₀ to θ_n
- Instead of thinking about this as n separate values, think about the parameters as a single vector (θ)
  - Where θ is n+1 dimensional
Our cost function is

Similarly, instead of thinking of J as a function of the n+1 numbers, J() is just a function of the parameter vector
- J(θ)
Gradient descent

Once again, this is
- θ_j = θ_j - learning rate (α) times the partial derivative of J(θ) with respect to θ_J(...)
- We do this through a simultaneous update of every θ_j value
Implementing this algorithm
- When n = 1

Above, we have slightly different update rules for θ₀ and θ₁
- Actually they're the same, except the end has a previously undefined x₀⁽ⁱ⁾ as 1, so wasn't shown
We now have an almost identical rule for multivariate gradient descent

What's going on here?
- We're doing this for each j (0 until n) as a simultaneous update (like when n = 1)
- So, we re-set θ_j to
  - θ_j minus the learning rate (α) times the partial derivative of of the θ vector with respect to θ_j
  - In non-calculus words, this means that we do
    - Learning rate
    - Times 1/m (makes the maths easier)
    - Times the sum of
      - The hypothesis taking in the variable vector, minus the actual value, times the j-th value in that variable vector for EACH example
- It's important to remember that
These algorithm are highly similar

Gradient Decent in practice: 1 Feature Scaling

Having covered the theory, we now move on to learn about some of the practical tricks
Feature scaling
- If you have a problem with multiple features
- You should make sure those features have a similar scale
  - Means gradient descent will converge more quickly
- e.g.
  - x1 = size (0 - 2000 feet)
  - x2 = number of bedrooms (1-5)
  - Means the contours generated if we plot θ₁ vs. θ₂ give a very tall and thin shape due to the huge range difference
- Running gradient descent on this kind of cost function can take a long time to find the global minimum

Pathological input to gradient descent
- So we need to rescale this input so it's more effective
- So, if you define each value from x1 and x2 by dividing by the max for each feature
- Contours become more like circles (as scaled between 0 and 1)
May want to get everything into -1 to +1 range (approximately)
- Want to avoid large ranges, small ranges or very different ranges from one another
- Rule a thumb regarding acceptable ranges
  - -3 to +3 is generally fine - any bigger bad
  - -1/3 to +1/3 is ok - any smaller bad
Can do mean normalization
- Take a feature x_i
- - Replace it by (x_i - mean)/max
  - So your values all have an average of about 0

Instead of max can also use standard deviation

Learning Rate α

Focus on the learning rate (α)
Topics
- Update rule
- Debugging
- How to chose α

Make sure gradient descent is working

Plot min J(θ) vs. no of iterations
- (i.e. plotting J(θ) over the course of gradient descent
If gradient descent is working then J(θ) should decrease after every iteration
Can also show if you're not making huge gains after a certain number
- Can apply heuristics to reduce number of iterations if need be
- If, for example, after 1000 iterations you reduce the parameters by nearly nothing you could chose to only run 1000 iterations in the future
- Make sure you don't accidentally hard-code thresholds like this in and then forget about why they're their though!

- Number of iterations varies a lot
  - 30 iterations
  - 3000 iterations
  - 3000 000 iterations
  - Very hard to tel in advance how many iterations will be needed
  - Can often make a guess based a plot like this after the first 100 or so iterations
- Automatic convergence tests
  - Check if J(θ) changes by a small threshold or less
    - Choosing this threshold is hard
    - So often easier to check for a straight line
      - Why? - Because we're seeing the straightness in the context of the whole algorithm
      - Could you design an automatic checker which calculates a threshold based on the systems preceding progress?
- Checking its working
  - If you plot J(θ) vs iterations and see the value is increasing - means you probably need a smaller α
    - Cause is because your minimizing a function which looks like this
- But you overshoot, so reduce learning rate so you actually reach the minimum (green line)
- So, use a smaller α
Another problem might be if J(θ) looks like a series of waves
- Here again, you need a smaller α
However
- If α is small enough, J(θ) will decrease on every iteration
- BUT, if α is too small then rate is too slow
  - A less steep incline is indicative of a slow convergence, because we're decreasing by less on each iteration than a steeper slope
Typically
- Try a range of alpha values
- Plot J(θ) vs number of iterations for each version of alpha
- Go for roughly threefold increases
- - 0.001, 0.003, 0.01, 0.03. 0.1, 0.3

Features and polynomial regression

Choice of features and how you can get different learning algorithms by choosing appropriate features
Polynomial regression for non-linear function

Example
- House price prediction
  - Two features
    - Frontage - width of the plot of land along road (x₁)
    - Depth - depth away from road (x₂)
- You don't have to use just two features
  - Can create new features
- Might decide that an important feature is the land area
  - So, create a new feature = frontage * depth (x₃)
  - h(x) = θ₀ + θ₁x₃
    - Area is a better indicator
- Often, by defining new features you may get a better model
Polynomial regression
- May fit the data better
- θ₀ + θ₁x + θ₂x² e.g. here we have a quadratic function
- For housing data could use a quadratic function
- - But may not fit the data so well - inflection point means housing prices decrease when size gets really big
  - So instead must use a cubic function

How do we fit the model to this data
- To map our old linear hypothesis and cost functions to these polynomial descriptions the easy thing to do is set
  - x₁ = x
  - x₂ = x²
  - x₃ = x³
- By selecting the features like this and applying the linear regression algorithms you can do polynomial linear regression
- Remember, feature scaling becomes even more important here
Instead of a conventional polynomial you could do variable ^(1/something) - i.e. square root, cubed root etc
Lots of features - later look at developing an algorithm to chose the best features

Normal equation

For some linear regression problems the normal equation provides a better solution
So far we've been using gradient descent
- Iterative algorithm which takes steps to converse
Normal equation solves θ analytically
- Solve for the optimum value of theta
Has some advantages and disadvantages

How does it work?

Simplified cost function
- J(θ) = aθ²+ bθ + c
  - θ is just a real number, not a vector
- Cost function is a quadratic function
- How do you minimize this?
  - Do
    - - Take derivative of J(θ) with respect to θ
      - Set that derivative equal to 0
      - Allows you to solve for the value of θ which minimizes J(θ)
In our more complex problems;
- Here θ is an n+1 dimensional vector of real numbers
- Cost function is a function of the vector value
  - How do we minimize this function
    - Take the partial derivative of J(θ) with respect θ_jand set to 0 for every j
    - Do that and solve for θ₀ to θ_n
    - This would give the values of θ which minimize J(θ)
- If you work through the calculus and the solution, the derivation is pretty complex
- - Not going to go through here
  - Instead, what do you need to know to implement this process

Example of normal equation

Here
- m = 4
- n = 4
To implement the normal equation
- Take examples
- Add an extra column (x₀ feature)
- Construct a matrix (X - the design matrix) which contains all the training data features in an [m x n+1] matrix
- Do something similar for y
  - Construct a column vector y vector [m x 1] matrix
- Using the following equation (X transpose * X) inverse times X transpose y

If you compute this, you get the value of theta which minimize the cost function

General case

Have m training examples and n features
- The design matrix (X)
- - Each training example is a n+1 dimensional feature column vector
  - X is constructed by taking each training example, determining its transpose (i.e. column -> row) and using it for a row in the design A
  - This creates an [m x (n+1)] matrix
- Vector y
- - Used by taking all the y values into a column vector

What is this equation?!
- (X^T * X)^-1
- - What is this --> the inverse of the matrix (X^T* X)
    - i.e. A = X^TX
    - A^-1= (X^TX)^-1
In octave and MATLAB you could do;

pinv(X'*x)*x'*y
- - X' is the notation for X transpose
  - pinv is a function for the inverse of a matrix
In a previous lecture discussed feature scaling
- If you're using the normal equation then no need for feature scaling

When should you use gradient descent and when should you use feature scaling?

- Gradient descent
  - Need to chose learning rate
  - Needs many iterations - could make it slower
  - Works well even when n is massive (millions)
    - Better suited to big data
    - What is a big n though
      - 100 or even a 1000 is still (relativity) small
      - If n is 10 000 then look at using gradient descent
- Normal equation
- - No need to chose a learning rate
  - No need to iterate, check for convergence etc.
  - Normal equation needs to compute (X^TX)^-1
    - This is the inverse of an n x n matrix
    - With most implementations computing a matrix inverse grows by O(n³)
      - So not great
  - Slow of n is large
  - - Can be much slower

Normal equation and non-invertibility

Advanced concept
- Often asked about, but quite advanced, perhaps optional material
- Phenomenon worth understanding, but not probably necessary
When computing (X^TX)^-1 * X^T* y)
- What if (X^TX) is non-invertible (singular/degenerate)
  - Only some matrices are invertible
  - This should be quite a rare problem
    - Octave can invert matrices using
      - pinv (pseudo inverse)
        This gets the right value even if (X^TX) is non-invertible
      - inv (inverse)
- What does it mean for (X^TX) to be non-invertible
  - Normally two common causes
    - Redundant features in learning model
      - e.g.
        x₁ = size in feet
        x₂ = size in meters squared
    - Too many features
      - e.g. m <= n (m is much larger than n)
        m = 10
        n = 100
      - Trying to fit 101 parameters from 10 training examples
      - Sometimes work, but not always a good idea
      - Not enough data
      - Later look at why this may be too little data
      - To solve this we
        Delete features
        Use regularization (let's you use lots of features for a small training set)
- If you find (X^TX) to be non-invertible
  - Look at features --> are features linearly dependent?
    - So just delete one, will solve problem

04: Linear Regression with Multiple Variables