Tides and Seasonal Modelling
Sinusoidal models of periodic data.
Key idea
Sinusoidal models of periodic data.
In depth
Periodic phenomena are modelled with y = A sin(B(x − h)) + k. Fit the period from observed data, the midline from the average, and the amplitude from the half range.
Worked example
High tide 4.0 m, low tide 1.0 m, 12.4 hours apart in cycle: A = 1.5, k = 2.5, B = 2π/12.4.
Real-world uses
- Predicting high and low tides for ports and sunlight hours through the year
Common mistake
Using the time between high and low tide as the period; it is only half.
How to learn this
- Read the key idea and say it in your own words.
- Work through the worked example, then try a similar problem.
- Use the interactive lesson’s visual and mini-quiz to check the pattern.
Frequently asked questions
What is Tides and Seasonal Modelling?
Sinusoidal models of periodic data. It is a topic at the advanced level in Trigonometry.
Where is Tides and Seasonal Modelling used in real life?
Real-world examples: Predicting high and low tides for ports and sunlight hours through the year.
What should I learn before Tides and Seasonal Modelling?
Make sure you are comfortable with Sound Waves and Beats, the previous topic in Trigonometry.
What is a common mistake with Tides and Seasonal Modelling?
Using the time between high and low tide as the period; it is only half.
How can I practise Tides and Seasonal Modelling?
Open the interactive lesson, play with the visual, then answer the three-question mini-quiz. Getting two right marks the topic complete.
What comes after Tides and Seasonal Modelling?
Move on to Ferris Wheel Problems next.
Related advanced topics in Trigonometry
- Graph of Tangent – Periodic with vertical asymptotes at odd multiples of π/2.
- Phase Shift – Horizontal translation of a wave.
- Vertical Shift and Midline – Moves the wave up or down.
- General Sinusoid – Combine amplitude, period, phase and shift.
- Graphs of Reciprocal Trig Functions – Secant, cosecant and cotangent graphs.
- Pythagorean Identity – The key identity from the unit circle.