πŸŽ“ Lesson 8 D4

Time-Varying Demand Patterns: Diurnal, Weekly, Seasonal

Time-varying demand patterns are changes in how much water people use throughout the day, week, or year β€” like higher use in the morning or during summer.

🎯 Learning Objectives

  • βœ“ Analyze diurnal demand curves to identify peak, minimum, and coincidence factors
  • βœ“ Calculate hourly demand multipliers from measured consumption data
  • βœ“ Apply seasonal adjustment factors to forecast annual demand profiles
  • βœ“ Explain how weekly patterns influence reservoir sizing and pump operation strategies
  • βœ“ Design a time-series demand input for hydraulic simulation software (e.g., EPANET)

πŸ“– Why This Matters

Imagine designing a water pipe that only meets average daily demand β€” it would fail every morning when thousands of residents shower, flush, and brew coffee simultaneously. Real-world water systems don’t experience steady flow; demand pulses hourly, dips on Sundays, and surges in summer. Ignoring these patterns leads to undersized pumps, pressure failures, wasted energy, and non-compliance with regulatory reliability standards (e.g., AWWA D100). Mastering time-varying demand isn’t just theory β€” it’s the difference between a resilient system and one that breaks at 7:15 a.m.

πŸ“˜ Core Principles

Demand variability arises from three nested temporal scales: (1) Diurnal β€” driven by human routines (e.g., morning peak ~6–9 a.m., evening peak ~5–8 p.m.), typically modeled as hourly multipliers relative to average daily demand (ADD); (2) Weekly β€” reflects workweek vs. weekend behavior, where weekend demand may be 10–25% lower than weekdays due to reduced commercial/industrial use; (3) Seasonal β€” influenced by temperature, irrigation, tourism, and school calendars, causing summer demand to exceed winter by 30–100% in arid or tourist-heavy regions. These patterns are not independent: a hot Saturday in July combines all three effects multiplicatively. Engineers must deconstruct observed metered data into base demand + time-varying components using normalization and statistical decomposition (e.g., moving averages, Fourier analysis for cyclical trends).

πŸ“ Hourly Demand Multiplier

The hourly demand multiplier (HDM) scales average daily demand to estimate flow in a given hour. It is derived from empirical data and applied in hydraulic models to simulate realistic transient loading.

Hourly Demand Multiplier (HDM)

HDM_h = Q_h / (ADD / 24)

Scales average daily demand to estimate flow in hour h.

Variables:
SymbolNameUnitDescription
HDM_h Hourly demand multiplier for hour h dimensionless Factor applied to ADD to obtain hourly demand
Q_h Measured hourly demand in hour h MG/h or L/s Actual volume consumed in that hour
ADD Average daily demand MG/day or L/s Total monthly or annual demand divided by number of days
Typical Ranges:
Residential-only system (U.S.): 0.4 – 2.2
Mixed-use system with irrigation: 0.3 – 3.5

πŸ’‘ Worked Example

Problem: A municipal utility records total monthly water use of 12.4 million gallons (MG) in June. Its service area has 8,200 residential connections. Metered data shows 6 a.m. consumption was 0.85 MG on a typical weekday. Calculate the HDM for 6 a.m. assuming uniform per-capita ADD and 30-day month.
1. Step 1: Compute average daily demand (ADD) = 12.4 MG Γ· 30 days = 0.4133 MG/day
2. Step 2: Compute hourly demand at 6 a.m. = 0.85 MG Γ· 30 days = 0.0283 MG/hour
3. Step 3: Compute HDM = (0.0283 MG/hour) Γ· (0.4133 MG/day Γ· 24 h/day) = 0.0283 Γ· 0.01722 β‰ˆ 1.64
Answer: The 6 a.m. HDM is 1.64, meaning demand at that hour is 64% above the uniform hourly average β€” consistent with typical morning peaks (range: 1.4–1.8).

πŸ—οΈ Real-World Application

In Tucson, AZ, the City Water Department uses 15-minute SCADA data from 42 pressure zones to calibrate EPANET models. During summer (June–August), they apply a composite multiplier: diurnal (e.g., 2.1 at 7 a.m.) Γ— weekly (1.05 for weekdays vs. 0.88 weekends) Γ— seasonal (1.75 vs. winter baseline). This enabled them to right-size a $12M variable-speed pump station β€” reducing energy use by 22% while maintaining >55 psi residual pressure during peak irrigation hours, per AWWA M17 requirements.

πŸ“‹ Case Connection

πŸ“‹ Calibration of Lagos Metropolitan Water Network

Persistent model–field mismatch (>25% pressure error) due to undocumented pipe replacements and unaccounted demand growt...

πŸ“‹ Water Quality Model Validation for Singapore’s Deep Tunnel Sewerage System (DTSS) Supply Branch

Disinfectant residual dropping below 0.2 mg/L at farthest nodes despite design dosing; suspected wall reaction dominance

πŸ“š References