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Published byAnnabel Parsons Modified over 9 years ago
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Chapter 3 Graphing Trigonometric Functions 3.1 Basic Graphics 3.2 Graphing y = k + A sin Bx and y = k +A cos Bx 3.3 Graphing y = k + A sin (Bx + C) and y = k +A cos (Bx + C) 3.4 Additional Applications 3.5 Graphing Combined Forms 3.6 Tangent, Cotangent, Secant, and Cosecant Functions Revisited
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3.1 Basic Graphs Graphs of y = sin x and y = cos x Graphs of y = tan x and y = cot x Graphs of y = csc x and y = sec x Graphing with a graphing calculator
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y = sin x
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y = cos x
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y = tan x
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Other Graphs
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3.2 Graphing y= k + A sin Bx and y = k + A cos Bx Graphing y = A sin x and y = A cos x Graphing y = sin Bx and y = cos Bx Graphing y = A sin Bx and y = A cos Bx Graphing y= k + A sin Bx and y = k + A cos Bx Applications
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Comparing Amplitudes Compare the graphs of y = 1/3 sin x and y = 3 sin x The effect of A in y = A sin x is to increase or decrease the y values without affecting the x values.
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Comparing Periods Compare the graphs of y = sin 2x and y = sin ½ x The graph shows the change in the period.
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Amplitude and Period For both y = A sin Bx and y = A cos Bx: Amplitude = |A|Period = 2 /B
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Vertical Shift y = -2 + 3 cos 2x, - x 2 Find the period, amplitude, and phase shift and then graph
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Period and Frequency For any periodic phenomenon, if P is the period and f is the frequency, P = 1/f.
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3.3 Graphing y = k + A sin (Bx + C) and y = k + A cos (Bx + C) Graphing y = A sin (Bx + C) and y = A cos (Bx + C) Graphing y = k + A sin (Bx + C) and y = k + A cos (Bx + C) Finding the equation for the graph of a simple harmonic motion
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Finding Period and Phase Shift y = A sin (Bx + C) and y = A cos (Bx + C) These have the same general shape as y = A sin Bx and y = A cos Bx translated horizontally. To find the translation: x = -C/B (phase shift) and x = -C/B + 2 /B
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Phase shift and Period Find the period and phase shift of y = sin(2x + /2) The period is . The phase shift is – /4.
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Steps for Graphing
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3.4 Additional Applications Modeling electric current Modeling light and other electromagnetic waves Modeling water waves Simple and damped harmonic motion: resonance
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Alternating Current Generator I = 35 sin (40 t – 10 ) (current) Amplitude = 35 Phase shift: 40 t = 10 t = ¼ Frequency = 1/Period = 20 Hz Period = 1/20
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Electromagnetic Waves E = A sin 2 (vt – r/ ) t = time, r = distance from the source, is the wavelength, v is the frequency
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Water Waves y = A sin 2p(f 1 t – r/ ) t = time, r = distance from the source, is the wavelength, f 1 is the frequency
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Damped Harmonic Motion Y = (1/t)sin ( /2)t, 1 t 8 First, graph y = 1/t. Then, graph y = sin( t/2) keeping high and low points within the envelope.
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3.6 Tangent, Cotangent, Secant, and Cosecant Functions Revisited Graphing y = A tan (Bx + C) and y = cot (Bx + c) Graphing y = A sec (Bx + C) and y = csc (Bx + c)
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y = tan x
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y = cot x
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y = csc x
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Y = sec x
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Graphing y = A tan (Bx + C) Y = 3 tan ( /2(x) + /4), -7/2 x 5/2 Phase shift = -1/2 Period = 2 Asymptotes at -7/2, -3/2, ½, and 5/2
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Graph of y = sec x Graph y = 5 sec (1/2(x) + for -7 x 3 .
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Graphing y = A csc(Bx + C) Graph y = 2 csc ( /2(x) = ) for -2 < x < 10
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