Essential Mathematics for Data Analysis and Earth Geometry
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Time Series Analysis
Identifying Trends
- Upward trend: Data increases over time.
- Downward trend: Data decreases over time.
- Stationary trend: No clear increase or decrease.
Smoothing Data (Reducing Fluctuations)
- 3-point moving mean: Average of 3 consecutive values.
- 5-point moving mean: Average of 5 consecutive values.
Seasonal Indices (SI)
Formula:
Seasonal Index = Actual Value ÷ Trend Value
- SI > 1 → Above-average season.
- SI < 1 → Below-average season.
Deseasonalising Data
Formula:
Deseasonalised Value = Actual Value ÷ Seasonal Index
Regression Line (Trend Line)
Equation of the line:
y = mx + c
- m = gradient (rate of change).
- c = y-intercept (starting value).
Bivariate Data Analysis
Types of Correlation
- Positive → Both variables increase together.
- Negative → One increases, the other decreases.
- No correlation → No clear relationship.
Correlation Coefficient (Pearson’s r)
- Measures the strength & direction of correlation.
- Range:
- r > 0.7 → Strong positive.
- r ≈ 0 → Weak or no correlation.
- r < −0.7 → Strong negative.
Interpolation vs. Extrapolation
- Interpolation (✔️ reliable) → Predicting within the given data range.
- Extrapolation (⚠️ risky) → Predicting beyond the given data range.
Line of Best Fit (Linear Regression)
Equation:
y = mx + c
Residuals: Differences between actual and predicted values (lower values indicate a better fit).
Growth & Decay in Sequences
Arithmetic Sequences (Linear Growth)
Formula:
Tn = a + (n − 1)d
- a = first term.
- d = common difference.
- n = term number.
Example: 2, 5, 8, 11... (d = 3).
Geometric Sequences (Exponential Growth/Decay)
Formula:
Tn = a × r(n−1)
- a = first term.
- r = common ratio.
- n = term number.
Example: 3, 6, 12, 24... (r = 2).
Compound Interest (Exponential Growth)
Formula:
A = P(1 + r)t
- A = final amount.
- P = initial amount (principal).
- r = interest rate (decimal).
- t = time (years).
Depreciation (Exponential Decay)
Formula:
A = P(1 − r)t
- r = depreciation rate.
Earth Geometry & Time Zones
Latitude & Longitude
- Latitude (°N/°S) → Horizontal lines (equator = 0°).
- Longitude (°E/°W) → Vertical lines (Prime Meridian = 0°).
Great Circle Distance
Formula:
d = 6371 × cos−1(sin φ1 sin φ2 + cos φ1 cos φ2 cos Δλ)
- φ1, φ2 = latitudes (in degrees).
- Δλ = difference in longitudes (degrees).
- 6371 km = Earth’s radius.
Steps:
- Convert latitudes & longitudes to degrees.
- Find the difference in longitude (Δλ).
- Use the calculator’s cos−1 function.
Time Zones & GMT
- Earth rotates 360° in 24 hours → 15° = 1-hour time difference.
- East → Add time
- West → Subtract time
Time Zone Conversion Formula
Local Time = GMT ± Time Zone Offset
Example:
- Sydney (AEST) = GMT +10.
- London (GMT 0).
- If it’s 2 PM in London, the time in Sydney = 2 + 10 = 12 AM (the next day).
International Date Line (IDL)
- Crossing west → go forward a day.
- Crossing east → go back a day.