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Differential Equations
The Geometric View of ODEs
01Direction Fields and the Geometric View of ODEs02Integral Curves and the Isocline Method03Perpendicular Isoclines: The Circles of y' = -x/y04Isocline Corridors and a Trap for Solutions05Existence and Uniqueness: One Curve Through a Point06Where Existence and Uniqueness FailProblem set0/10Problem set 20/10MIT problem set0/3
Numerical Methods
01Euler's Method and Its Three Equations02Euler's Method by Hand: Building the Table03Convexity and the Sign of Euler's Error04First Order Error: Halve the Step, Halve the Error05Improved Euler (RK2): Averaging Two Slopes06Runge-Kutta 4 and the Price of Accuracy07Singular Points: Where Every Method FailsProblem set0/10Problem set 20/10MIT problem set0/1
First-Order Linear Equations
01First Order Linear: Standard Form and the Sign of p02The Conduction-Diffusion Model: Newton's Law of Cooling03The Integrating Factor and the Four-Step Method04Integrating Factors: Two Mistakes and a Trick Question05Constant Coefficients: Steady State and TransientProblem set0/10Problem set 20/10MIT problem set0/1
Substitution Methods
01Scaling a First Order ODE: The Fourth-Power Cooling Law02The Bernoulli Equation and the Substitution v = y^(1-n)03A Worked Bernoulli Example: The Substitution v = 1/y04Homogeneous Equations: The Zoom Test and y = zx05Modelling the Lighthouse Chase: A 45-Degree Heading06The Boat's Path: A Logarithmic Spiral in Polar CoordinatesProblem set0/10Problem set 20/10
Autonomous Equations
01Autonomous Equations and Time-Translation Invariance02Critical Points: Constant Solutions as Barriers03The Embezzler Model dy/dt = ry - w: One Unstable Balance04The Logistic Equation: Carrying Capacity Without Solving05Stable, Unstable and Semi-Stable Critical Points06Maximum Sustainable Harvest: Why h = a^2/4bProblem set0/10Problem set 20/10MIT problem set0/3
Complex Numbers
01Complex Division, Polar Form and the Definition of e^(iθ)02Why e^(iθ) Earns Its Name: Multiply Moduli, Add Angles03Integrating e^(-x) cos x by Complexifying04The nth Roots of Unity: Zeta on the Unit CircleProblem set0/10Problem set 20/10MIT problem set0/4
Input and Response
01Steady-State and Transient Solutions of y' + ky = q(t)02Input, Response and the Superposition Principle03Solving y' + ky = k cos ωt by Complexification04Amplitude and Phase Lag of a Sinusoidal ResponseProblem set0/10Problem set 20/10MIT problem set0/2
01Cartesian Method: Rationalise, Then Take the Real Part02The Sinusoidal Identity and Its Right Triangle03Three Proofs of the Sinusoidal Identity04The Mixing Tank: Salt Balance and k = r/V05RC Circuits, Decay Chains and Negative kProblem set0/10Problem set 20/10MIT problem set0/2
Second-Order Linear Equations
01Second-Order Linear ODEs and the Spring–Mass–Dashpot02The Characteristic Equation and Overdamped Motion03Complex Roots a ± bi and Underdamped Oscillation04Critical Damping and Reduction of Order: t e^(−at)Problem set0/10Problem set 20/10MIT problem set0/2
01One Complex Root Is Enough: Conjugates and Real Solutions02When a Damped Spring Oscillates: p Below ω₀03Damped Oscillations: Pseudo-Period and ω₁² + p² = ω₀²Problem set0/10Problem set 20/10MIT problem set0/1
01Superposition: Why Linearity Makes c₁y₁ + c₂y₂ a Solution02The Wronskian and Abel's Theorem: Fitting Any Initial Values03Normalized Solutions: Why cosh x and sinh x Solve y'' − y = 004Uniqueness: Why c₁y₁ + c₂y₂ Is Every SolutionProblem set0/10Problem set 20/10

Euler's Method and Its Three Equations

How does following one line element at a time turn a direction field into the three recursive equations a computer actually runs?


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Your summary note

    1. 1

      The initial value problem (IVP)

      Write the pair y′=f(x,y)y' = f(x,y)y′=f(x,y) and y(x0)=y0y(x_0) = y_0y(x0​)=y0​, name the two parts, and note that numerical methods are how such problems are actually solved in practice.

    2. 2

      Euler's method geometrically

      Describe starting at (x0,y0)(x_0, y_0)(x0​,y0​), following the line element of slope f(x,y)f(x,y)f(x,y) for one step of size hhh, recomputing the slope at the new point, and repeating to produce a broken-line approximation.

    3. 3

      Deriving the three Euler equations

      Complete the triangle at (xn,yn)(x_n, y_n)(xn​,yn​) with slope AnA_nAn​, horizontal side hhh and vertical side hAnh A_nhAn​, then write out xn+1=xn+hx_{n+1} = x_n + hxn+1​=xn​+h, yn+1=yn+hAny_{n+1} = y_n + h A_nyn+1​=yn​+hAn​, and An=f(xn,yn)A_n = f(x_n, y_n)An​=f(xn​,yn​).

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