Geometry and Trigonometry

36 Angles and Triangles

Angles and triangles are fundamental building blocks in geometry. Understanding their definitions, properties, and relationships is crucial for solving a wide range of problems in mathematics, engineering, and physics.

Understanding Angles

An angle is formed by two rays (or line segments) that share a common endpoint, called the vertex. Angles are typically measured in degrees ($^\circ$) or radians (rad).

Types of Angles:

  • Acute Angle: An angle less than $90^\circ$.
  • Right Angle: An angle exactly equal to $90^\circ$.
  • Obtuse Angle: An angle greater than $90^\circ$ but less than $180^\circ$.
  • Straight Angle: An angle exactly equal to $180^\circ$ (a straight line).
  • Reflex Angle: An angle greater than $180^\circ$ but less than $360^\circ$.
  • Full Rotation/Circle: An angle exactly equal to $360^\circ$.

Angle Relationships:

  • Complementary Angles: Two angles whose sum is $90^\circ$.
  • Supplementary Angles: Two angles whose sum is $180^\circ$.
  • Angles on a Straight Line: Angles that lie on a straight line add up to $180^\circ$.
  • Angles at a Point: Angles around a central point add up to $360^\circ$.
  • Vertically Opposite Angles: When two straight lines intersect, the angles opposite each other at the intersection point are equal.
  • Corresponding Angles: Formed when a transversal line intersects two parallel lines; they are in the same relative position and are equal.
  • Alternate Interior Angles: Formed when a transversal line intersects two parallel lines; they are on opposite sides of the transversal and between the parallel lines, and are equal.
  • Consecutive Interior Angles (Co-interior): Formed when a transversal line intersects two parallel lines; they are on the same side of the transversal and between the parallel lines, and their sum is $180^\circ$.

Understanding Triangles

A triangle is a polygon with three sides and three angles. The sum of the interior angles of any triangle is always $180^\circ$.

Types of Triangles:

  • Equilateral Triangle: All three sides are equal in length, and all three angles are equal ($60^\circ$ each).
  • Isosceles Triangle: Two sides are equal in length, and the angles opposite those sides are equal.
  • Scalene Triangle: All three sides are of different lengths, and all three angles are of different measures.
  • Right-angled Triangle: One angle is a right angle ($90^\circ$). The side opposite the right angle is called the hypotenuse.
  • Acute Triangle: All three angles are acute (less than $90^\circ$).
  • Obtuse Triangle: One angle is obtuse (greater than $90^\circ$).

Properties of Triangles:

  • Angle Sum Property: The sum of the interior angles of a triangle is always $180^\circ$.
  • Exterior Angle Property: The measure of an exterior angle of a triangle is equal to the sum of the measures of its two opposite interior angles.
  • Pythagorean Theorem: For a right-angled triangle with legs $a$ and $b$ and hypotenuse $c$, $a^2 + b^2 = c^2$.

38 Introduction to Trigonometry

Trigonometry is a branch of mathematics that studies relationships between side lengths and angles of triangles. It is particularly focused on right-angled triangles and the trigonometric ratios of angles within them.

38.2 Pythagoras Theorem

The Pythagorean Theorem states that in a right-angled triangle, the square of the length of the hypotenuse (the side opposite the right angle) is equal to the sum of the squares of the lengths of the other two sides (legs).

$$ a^2 + b^2 = c^2 $$

Where $a$ and $b$ are the lengths of the legs, and $c$ is the length of the hypotenuse.

Example:

If a right triangle has legs of length $3$ and $4$, the hypotenuse $c$ would be: $$ 3^2 + 4^2 = c^2 $$ $$ 9 + 16 = c^2 $$ $$ 25 = c^2 $$ $$ c = \sqrt{25} = 5 $$

38.3 Sine, Cosine, Tangent (SOH CAH TOA)

These are the primary trigonometric ratios for acute angles in a right-angled triangle. They relate the angles to the ratio of two side lengths.

  • Sine (SOH): $$ \sin \theta = \frac{\text{Opposite}}{\text{Hypotenuse}} $$
  • Cosine (CAH): $$ \cos \theta = \frac{\text{Adjacent}}{\text{Hypotenuse}} $$
  • Tangant (TOA): $$ \tan \theta = \frac{\text{Opposite}}{\text{Adjacent}} $$

Where:

  • Opposite: The side directly across from the angle $\theta$.
  • Adjacent: The side next to the angle $\theta$, not the hypotenuse.
  • Hypotenuse: The longest side, opposite the $90^\circ$ angle.

38.4 Evaluating Trigonometric Ratios (Acute Angles)

You can evaluate trigonometric ratios for acute angles using a scientific calculator. Ensure your calculator is in the correct mode (degrees or radians) depending on the problem.

For example, to find $\sin 30^\circ$, you would input "sin(30)" into your calculator, which gives $0.5$.

Special Triangles:

Certain angles have exact trigonometric values that can be derived from special right triangles:

  • $45^\circ-45^\circ-90^\circ$ Triangle: Sides in ratio $1 : 1 : \sqrt{2}$.
  • $30^\circ-60^\circ-90^\circ$ Triangle: Sides in ratio $1 : \sqrt{3} : 2$.

38.5 Reciprocal Ratios

In addition to sine, cosine, and tangent, there are three reciprocal trigonometric ratios:

  • Cosecant (csc): Reciprocal of sine. $$ \csc \theta = \frac{1}{\sin \theta} = \frac{\text{Hypotenuse}}{\text{Opposite}} $$
  • Secant (sec): Reciprocal of cosine. $$ \sec \theta = \frac{1}{\cos \theta} = \frac{\text{Hypotenuse}}{\text{Adjacent}} $$
  • Cotangent (cot): Reciprocal of tangent. $$ \cot \theta = \frac{1}{\tan \theta} = \frac{\text{Adjacent}}{\text{Opposite}} $$

38.6 Fractional & Surd Forms

It's important to know the exact values of trigonometric ratios for common angles in fractional and surd (radical) forms, especially for non-calculator contexts.

Angle ($\theta$) $\sin \theta$ $\cos \theta$ $\tan \theta$
$0^\circ$ $0$ $1$ $0$
$30^\circ$ $\frac{1}{2}$ $\frac{\sqrt{3}}{2}$ $\frac{1}{\sqrt{3}} = \frac{\sqrt{3}}{3}$
$45^\circ$ $\frac{1}{\sqrt{2}} = \frac{\sqrt{2}}{2}$ $\frac{1}{\sqrt{2}} = \frac{\sqrt{2}}{2}$ $1$
$60^\circ$ $\frac{\sqrt{3}}{2}$ $\frac{1}{2}$ $\sqrt{3}$
$90^\circ$ $1$ $0$ Undefined

38.7 Solving Right-Angled Triangles

To solve a right-angled triangle means to find all unknown side lengths and angle measures. This is typically done using a combination of the Pythagorean Theorem and trigonometric ratios (SOH CAH TOA).

Steps to Solve:

  1. Identify the knowns (at least one side and one other angle, or two sides).
  2. Determine which unknown you need to find.
  3. Choose the appropriate formula (Pythagorean Theorem or a trig ratio) based on your knowns and the unknown you want to find.
  4. Solve the equation for the unknown.
  5. Repeat until all sides and angles are known.

38.8 Elevation & Depression Angles

  • Angle of Elevation: The angle formed by the horizontal line of sight and the line of sight looking *upwards* to an object.
  • Angle of Depression: The angle formed by the horizontal line of sight and the line of sight looking *downwards* to an object.

These angles are always measured from the horizontal. The angle of elevation from point A to point B is equal to the angle of depression from point B to point A (due to alternate interior angles with parallel horizontal lines).

38.9 Small Angle Approximations

For very small angles $\theta$ (typically less than $10^\circ$ or $0.17$ radians), measured in radians, the following approximations are often used in physics and engineering:

  • $$ \sin \theta \approx \theta $$
  • $$ \tan \theta \approx \theta $$
  • $$ \cos \theta \approx 1 - \frac{\theta^2}{2} $$

These approximations simplify calculations when dealing with small angles.

39 Trigonometric Waveforms

Trigonometric waveforms, such as sine and cosine waves, are fundamental to understanding periodic phenomena in various fields including physics, engineering, and signal processing. They describe oscillations, waves, and cyclical motions.

39.1 Trigonometric Graphs

The graphs of trigonometric functions are characterized by their repeating patterns (periodicity). The basic sine, cosine, and tangent graphs are:

  • Sine Graph ($y = \sin x$): Starts at $0$, increases to $1$, decreases to $-1$, returns to $0$. Period of $2\pi$ radians ($360^\circ$). Range: $[-1, 1]$.
  • Cosine Graph ($y = \cos x$): Starts at $1$, decreases to $-1$, increases to $1$. Period of $2\pi$ radians ($360^\circ$). Range: $[-1, 1]$. It is essentially a sine wave shifted by $\pi/2$ radians ($90^\circ$).
  • Tangent Graph ($y = \tan x$): Has vertical asymptotes where $\cos x = 0$ (e.g., at $\pm \pi/2, \pm 3\pi/2$). Period of $\pi$ radians ($180^\circ$). Range: $(-\infty, \infty)$.

39.2 Angles of Any Magnitude (CAST Diagram)

Trigonometric ratios can be extended to angles beyond $90^\circ$ by considering angles in a Cartesian coordinate system relative to the positive x-axis. The CAST diagram helps determine the sign of the trigonometric ratios in each quadrant:

QuadrantPositive RatiosAngles
I (A)All$0^\circ < \theta < 90^\circ$
II (S)Sine$90^\circ < \theta < 180^\circ$
III (T)Tangent$180^\circ < \theta < 270^\circ$
IV (C)Cosine$270^\circ < \theta < 360^\circ$

This means:

  • In Quadrant I (All), $\sin \theta, \cos \theta, \tan \theta$ are all positive.
  • In Quadrant II (Sine), only $\sin \theta$ is positive.
  • In Quadrant III (Tangent), only $\tan \theta$ is positive.
  • In Quadrant IV (Cosine), only $\cos \theta$ is positive.

39.3 Sine & Cosine Wave Production

Sine and cosine waves can be visualized as the projection of uniform circular motion onto a linear axis. As a point moves around a unit circle (radius 1), its vertical projection (y-coordinate) generates a sine wave, and its horizontal projection (x-coordinate) generates a cosine wave.

39.4 Waveform Terminology

  • Amplitude (A): The maximum displacement or distance moved by a point on a vibrating body or wave measured from its equilibrium position. For $y = A \sin(\omega t)$, the amplitude is $|A|$.
  • Period (T):: The time taken for one complete cycle of the waveform. For $y = A \sin(\omega t)$, the period is $T = \frac{2\pi}{\omega}$ (if $\omega$ is in rad/s) or $T = \frac{360^\circ}{\omega}$ (if $\omega$ is in deg/s).
  • Frequency (f): The number of complete cycles per unit time. It is the reciprocal of the period: $f = \frac{1}{T}$. Measured in Hertz (Hz).
  • Angular Frequency ($\omega$): The rate of change of the phase of a sinusoidal waveform. It is related to frequency by $\omega = 2\pi f$. Measured in radians per second (rad/s) or degrees per second (deg/s).
  • Phase Angle ($\alpha$): Represents the horizontal shift of the waveform relative to a standard sine or cosine wave. A positive $\alpha$ in $A \sin(\omega t + \alpha)$ indicates a phase lead (shift to the left), and a negative $\alpha$ indicates a phase lag (shift to the right).

39.5 Sinusoidal Form: $A \sin(\omega t \pm \alpha)$

The general equation for a sinusoidal waveform is typically given as: $$ y(t) = A \sin(\omega t \pm \alpha) \quad \text{or} \quad y(t) = A \cos(\omega t \pm \alpha) $$ Where:

  • $A$ is the Amplitude.
  • $\omega$ is the Angular Frequency.
  • $t$ is the time or independent variable.
  • $\alpha$ is the Phase Angle.
  • The sign $\pm$ indicates phase lead (+) or phase lag (-).

39.6 Complex Waveforms

Complex waveforms are those that are not purely sinusoidal but are periodic. According to Fourier's theorem, any periodic complex waveform can be represented as a sum of simple sinusoidal (sine and cosine) waves of different amplitudes, frequencies, and phase angles. This decomposition is crucial in signal analysis.

40 Cartesian & Polar Co-ordinates

In mathematics, coordinate systems are used to specify the position of points in space. Two of the most common systems are Cartesian coordinates and Polar coordinates, each offering unique advantages depending on the problem.

40.1 Introduction

The Cartesian coordinate system (also known as the rectangular coordinate system) uses two perpendicular axes (x and y) to define a point's position as an ordered pair $(x, y)$. This is the most familiar system for graphing linear and quadratic equations.

The Polar coordinate system defines a point's position by its distance from a fixed point (the pole or origin) and the angle it makes with a fixed direction (the polar axis). A point is specified by $(r, \theta)$, where $r$ is the radial distance and $\theta$ is the angular position.

40.2 Cartesian to Polar Conversion

To convert a point from Cartesian coordinates $(x, y)$ to Polar coordinates $(r, \theta)$:

  • Radius ($r$): Use the Pythagorean theorem: $$ r = \sqrt{x^2 + y^2} $$
  • Angle ($\theta$): Use the inverse tangent function, being mindful of the quadrant to get the correct angle: $$ \theta = \arctan\left(\frac{y}{x}\right) $$ You might need to add $180^\circ$ (or $\pi$ radians) if $x$ is negative, or $360^\circ$ (or $2\pi$ radians) if $\theta$ ends up negative and you want it in $[0, 360^\circ)$ range. It's often safer to use `Math.atan2(y, x)` function available in many programming languages and calculators, which automatically handles quadrants.

The angle $\theta$ is typically given in radians or degrees, often in the range $0 \le \theta < 2\pi$ or $0^\circ \le \theta < 360^\circ$.

40.3 Polar to Cartesian Conversion

To convert a point from Polar coordinates $(r, \theta)$ to Cartesian coordinates $(x, y)$:

  • X-coordinate ($x$): $$ x = r \cos \theta $$
  • Y-coordinate ($y$): $$ y = r \sin \theta $$

40.4 Calculator Pol/Rec Functions

Most scientific calculators have built-in functions for converting between Cartesian and Polar coordinates, often labeled as "Pol(" (for Cartesian to Polar) and "Rec(" (for Polar to Cartesian). These functions handle the quadrant adjustments automatically, simplifying calculations.

Example Calculator Usage:

  • To convert Cartesian $(3, 4)$ to Polar: Type `Pol(3, 4)` and press ENTER. It might return `r=5`, `theta=53.13`.
  • To convert Polar $(5, 30^\circ)$ to Cartesian: Type `Rec(5, 30)` and press ENTER. It might return `x=4.33`, `y=2.5`.

Always ensure your calculator is in the correct angle mode (DEG or RAD) before using these functions.

41 Non-Right-Angled Triangles

While basic trigonometry focuses on right-angled triangles, many real-world problems involve triangles without a $90^\circ$ angle. For these, we use the Sine Rule and Cosine Rule.

41.1 Sine & Cosine Rules

Sine Rule:

The Sine Rule relates the sides of a triangle to the sines of their opposite angles. It is used when you know:

  • Two angles and one side (AAS or ASA).
  • Two sides and a non-included angle (SSA - ambiguous case).

For any triangle ABC with sides $a, b, c$ opposite to angles $A, B, C$ respectively:

$$ \frac{a}{\sin A} = \frac{b}{\sin B} = \frac{c}{\sin C} $$

Cosine Rule:

The Cosine Rule is a generalization of the Pythagorean theorem. It is used when you know:

  • Two sides and the included angle (SAS).
  • All three sides (SSS).

For any triangle ABC:

$$ a^2 = b^2 + c^2 - 2bc \cos A $$ $$ b^2 = a^2 + c^2 - 2ac \cos B $$ $$ c^2 = a^2 + b^2 - 2ab \cos C $$

It can also be rearranged to find an angle when all three sides are known:

$$ \cos A = \frac{b^2 + c^2 - a^2}{2bc} $$ $$ \cos B = \frac{a^2 + c^2 - b^2}{2ac} $$ $$ \cos C = \frac{a^2 + b^2 - c^2}{2ab} $$

41.2 Area of Any Triangle

The area of any triangle can be calculated if you know the lengths of two sides and the measure of the angle included between them:

$$ \text{Area} = \frac{1}{2}ab \sin C $$

Or similarly:

$$ \text{Area} = \frac{1}{2}bc \sin A $$ $$ \text{Area} = \frac{1}{2}ac \sin B $$

41.3 Triangle Solution Problems

Solving non-right-angled triangles involves determining all unknown angles and side lengths given a set of initial information. The choice between the Sine Rule and Cosine Rule depends on the given information:

  • Use Sine Rule if: You have an angle-side pair (a known angle and its opposite side), and one other piece of information (another angle or another side). This covers AAS, ASA, and SSA (ambiguous case).
  • Use Cosine Rule if: You have three sides (SSS) and want to find an angle, or two sides and the included angle (SAS) and want to find the third side.

42 Trigonometric Identities & Equations

Trigonometric identities are equations that are true for all values of the variables for which the expressions are defined. Trigonometric equations are equations that involve trigonometric functions and are only true for specific values of the variable.

42.1 Trigonometric Identities

Identities are powerful tools for simplifying expressions and solving equations. Here are some of the most common categories:

Fundamental Identities:

  • Reciprocal Identities: $$ \csc \theta = \frac{1}{\sin \theta} $$ $$ \sec \theta = \frac{1}{\cos \theta} $$ $$ \cot \theta = \frac{1}{\tan \theta} $$
  • Quotient Identities: $$ \tan \theta = \frac{\sin \theta}{\cos \theta} $$ $$ \cot \theta = \frac{\cos \theta}{\sin \theta} $$
  • Pythagorean Identities: $$ \sin^2 \theta + \cos^2 \theta = 1 $$ $$ 1 + \tan^2 \theta = \sec^2 \theta $$ $$ 1 + \cot^2 \theta = \csc^2 \theta $$

Compound Angle Formulae (Addition/Subtraction Formulae):

  • $$ \sin(A \pm B) = \sin A \cos B \pm \cos A \sin B $$
  • $$ \cos(A \pm B) = \cos A \cos B \mp \sin A \sin B $$
  • $$ \tan(A \pm B) = \frac{\tan A \pm \tan B}{1 \mp \tan A \tan B} $$

Double Angle Formulae:

  • $$ \sin 2A = 2 \sin A \cos A $$
  • $$ \cos 2A = \cos^2 A - \sin^2 A = 2 \cos^2 A - 1 = 1 - 2 \sin^2 A $$
  • $$ \tan 2A = \frac{2 \tan A}{1 - \tan^2 A} $$

42.2 Identity Problems

Proving trigonometric identities involves transforming one side of the equation (usually the more complex side) into the other side using known identities and algebraic manipulation. Key strategies include:

  • Start with the more complicated side.
  • Express everything in terms of sine and cosine.
  • Look for opportunities to use Pythagorean identities.
  • Combine fractions or split single fractions.
  • Factor expressions or expand terms.
  • Multiply by a conjugate.

42.3 Trigonometric Equations

Trigonometric equations are equations that contain trigonometric functions of unknown angles. Unlike identities, these equations are only true for specific values of the angle. When solving, remember to consider:

  • The basic angle (the acute angle).
  • The quadrant(s) where the trigonometric function has the required sign (using the CAST diagram).
  • The periodicity of the function to find all possible solutions (general solution).
  • The specified range for the solutions (e.g., $0^\circ \le \theta < 360^\circ$).

The general solutions for basic equations are:

  • For $\sin \theta = k$: $$ \theta = n \cdot 360^\circ + \alpha \quad \text{or} \quad \theta = n \cdot 360^\circ + (180^\circ - \alpha) $$ where $\alpha = \sin^{-1}(k)$ and $n$ is an integer.
  • For $\cos \theta = k$: $$ \theta = n \cdot 360^\circ \pm \alpha $$ where $\alpha = \cos^{-1}(k)$ and $n$ is an integer.
  • For $\tan \theta = k$: $$ \theta = n \cdot 180^\circ + \alpha $$ where $\alpha = \tan^{-1}(k)$ and $n$ is an integer.

42.4 Equation Problems (i)

These are the simplest forms, where you directly find the basic angle and then use the CAST diagram to find solutions in the given range. For example, solving $\sin x = 0.5$ or $\cos x = -0.8$.

42.5 Equation Problems (ii)

These involve transformations of the angle, like $\sin(2x) = k$ or $\cos(x - 30^\circ) = k$. The key is to transform the range accordingly before finding solutions for the composite angle.

42.6 Equation Problems (iii)

This category includes equations that are quadratic in form (e.g., $2\sin^2 x + \sin x - 1 = 0$) or require the use of identities to simplify them into a solvable form (e.g., using $\sin^2 x + \cos^2 x = 1$ to eliminate one trigonometric function).

42.7 Equation Problems (iv)

These are more complex equations that might require multiple steps of identity application, factoring, or rearrangement to solve. They often combine concepts from previous sections, such as using double angle identities to reduce an equation to a simpler form.

43 Trigonometric & Hyperbolic Relations

Trigonometric and hyperbolic functions, while seemingly distinct, share deep mathematical connections, particularly when explored in the realm of complex numbers. They both arise from the geometry of a unit circle and a unit hyperbola, respectively, and are closely related through Euler's formula.

43.1 The Relationship (Using Euler's Formula)

The relationship between trigonometric functions (like sine and cosine) and the exponential function (which forms the basis for hyperbolic functions) is beautifully expressed by Euler's Formula:

$$ e^{ix} = \cos x + i \sin x $$

Where $i$ is the imaginary unit ($i^2 = -1$).

From Euler's formula, we can derive expressions for sine and cosine in terms of complex exponentials:

  • By replacing $x$ with $-x$ in Euler's formula: $$ e^{-ix} = \cos(-x) + i \sin(-x) = \cos x - i \sin x $$
  • Adding $e^{ix}$ and $e^{-ix}$: $$ e^{ix} + e^{-ix} = (\cos x + i \sin x) + (\cos x - i \sin x) = 2 \cos x $$ Therefore, $$ \cos x = \frac{e^{ix} + e^{-ix}}{2} $$
  • Subtracting $e^{-ix}$ from $e^{ix}$: $$ e^{ix} - e^{-ix} = (\cos x + i \sin x) - (\cos x - i \sin x) = 2i \sin x $$ Therefore, $$ \sin x = \frac{e^{ix} - e^{-ix}}{2i} $$

Now, let's look at the definitions of the hyperbolic functions:

  • Hyperbolic Cosine (cosh): $$ \cosh x = \frac{e^x + e^{-x}}{2} $$
  • Hyperbolic Sine (sinh): $$ \sinh x = \frac{e^x - e^{-x}}{2} $$

By comparing these, we can see the direct relationships:

  • $$ \cos(ix) = \frac{e^{i(ix)} + e^{-i(ix)}}{2} = \frac{e^{-x} + e^{x}}{2} = \cosh x $$
  • $$ \sin(ix) = \frac{e^{i(ix)} - e^{-i(ix)}}{2i} = \frac{e^{-x} - e^{x}}{2i} = \frac{-(e^x - e^{-x})}{2i} = \frac{-2i \sinh x}{2i} = i \sinh x $$

These fundamental relationships ($ \cos(ix) = \cosh x $ and $ \sin(ix) = i \sinh x $) reveal the deep connection between the two families of functions.

43.2 Hyperbolic Identities

Similar to trigonometric identities, hyperbolic functions also have a set of identities that can be derived from their definitions. Many of these mirror trigonometric identities, with some sign changes.

Fundamental Hyperbolic Identities:

  • $$ \cosh^2 x - \sinh^2 x = 1 $$ (This is the hyperbolic equivalent of $\sin^2 x + \cos^2 x = 1$)
  • $$ 1 - \tanh^2 x = \text{sech}^2 x $$
  • $$ \coth^2 x - 1 = \text{csch}^2 x $$

Other common hyperbolic functions:

  • Hyperbolic Tangent (tanh): $$ \tanh x = \frac{\sinh x}{\cosh x} = \frac{e^x - e^{-x}}{e^x + e^{-x}} $$
  • Hyperbolic Secant (sech): $$ \text{sech } x = \frac{1}{\cosh x} = \frac{2}{e^x + e^{-x}} $$
  • Hyperbolic Cosecant (csch): $$ \text{csch } x = \frac{1}{\sinh x} = \frac{2}{e^x - e^{-x}} $$
  • Hyperbolic Cotangent (coth): $$ \coth x = \frac{1}{\tanh x} = \frac{e^x + e^{-x}}{e^x - e^{-x}} $$

44 Compound Angles

Compound angle formulas allow us to express trigonometric functions of sums or differences of angles in terms of trigonometric functions of the individual angles. These are powerful tools for simplifying expressions, solving equations, and analyzing waveforms.

44.1 Compound Angle Formulae

These identities are fundamental for working with compound angles:

  • $$ \sin(A+B) = \sin A \cos B + \cos A \sin B $$
  • $$ \sin(A-B) = \sin A \cos B - \cos A \sin B $$
  • $$ \cos(A+B) = \cos A \cos B - \sin A \sin B $$
  • $$ \cos(A-B) = \cos A \cos B + \sin A \sin B $$
  • $$ \tan(A+B) = \frac{\tan A + \tan B}{1 - \tan A \tan B} $$
  • $$ \tan(A-B) = \frac{\tan A - \tan B}{1 + \tan A \tan B} $$

44.2 Converting $a \sin \omega t + b \cos \omega t$

Expressions of the form $a \sin \theta + b \cos \theta$ can be converted into a single trigonometric function of the form $R \sin(\theta \pm \alpha)$ or $R \cos(\theta \pm \alpha)$, where $R$ is the amplitude and $\alpha$ is the phase angle. This is particularly useful in physics and engineering for analyzing oscillating systems.

To convert $a \sin \theta + b \cos \theta$ to $R \sin(\theta + \alpha)$:

  • Find $R$: $$ R = \sqrt{a^2 + b^2} $$
  • Find $\alpha$: Compare $a \sin \theta + b \cos \theta$ with $R \sin \theta \cos \alpha + R \cos \theta \sin \alpha$. This gives $a = R \cos \alpha$ and $b = R \sin \alpha$. Therefore, $$ \tan \alpha = \frac{R \sin \alpha}{R \cos \alpha} = \frac{b}{a} $$ Be careful to find $\alpha$ in the correct quadrant based on the signs of $a$ and $b$.

Similarly, for $R \cos(\theta - \alpha)$, you would compare $a \sin \theta + b \cos \theta$ with $R \cos \theta \cos \alpha + R \sin \theta \sin \alpha$, leading to $\tan \alpha = \frac{a}{b}$.

44.3 Double Angles

Double angle identities are special cases of compound angle formulae where $A = B$.

  • $$ \sin 2A = 2 \sin A \cos A $$
  • $$ \cos 2A = \cos^2 A - \sin^2 A $$ Also: $$ \cos 2A = 2 \cos^2 A - 1 $$ And: $$ \cos 2A = 1 - 2 \sin^2 A $$
  • $$ \tan 2A = \frac{2 \tan A}{1 - \tan^2 A} $$

44.4 Products to Sums/Differences

These identities are used to transform products of sines and cosines into sums or differences, which can simplify integration or other calculations.

  • $$ 2 \sin A \cos B = \sin(A+B) + \sin(A-B) $$
  • $$ 2 \cos A \sin B = \sin(A+B) - \sin(A-B) $$
  • $$ 2 \cos A \cos B = \cos(A+B) + \cos(A-B) $$
  • $$ 2 \sin A \sin B = \cos(A-B) - \cos(A+B) $$

44.5 Sums/Differences to Products

These identities are the inverse of the product-to-sum identities and are useful for factoring trigonometric expressions or solving certain types of equations.

  • $$ \sin P + \sin Q = 2 \sin\left(\frac{P+Q}{2}\right) \cos\left(\frac{P-Q}{2}\right) $$
  • $$ \sin P - \sin Q = 2 \cos\left(\frac{P+Q}{2}\right) \sin\left(\frac{P-Q}{2}\right) $$
  • $$ \cos P + \cos Q = 2 \cos\left(\frac{P+Q}{2}\right) \cos\left(\frac{P-Q}{2}\right) $$
  • $$ \cos P - \cos Q = -2 \sin\left(\frac{P+Q}{2}\right) \sin\left(\frac{P-Q}{2}\right) $$

44.6 Power Waveforms (AC Circuits)

In AC (Alternating Current) circuits, voltage and current are often represented by sinusoidal waveforms. The power delivered in an AC circuit is the product of voltage and current. When voltage and current are out of phase, their product leads to a power waveform that can be simplified using product-to-sum identities. This helps in understanding average power, reactive power, and apparent power, which are critical concepts in electrical engineering.