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Environment Climate Meterology

Reference data and engineering information about environment climate meterology for material properties applications.

environmentclimatemeterology

Overview

Engineering reference data for Environment Climate Meterology in material science and properties.

Key Formulas

Stress

σ=FA\sigma = \frac{F}{A}

Force per unit area.

Strain

ε=ΔLL0\varepsilon = \frac{\Delta L}{L_0}

Change in length per original length.

Hooke's Law

σ=Eε\sigma = E \varepsilon

Stress proportional to strain in elastic region.

Thermal Expansion

ΔL=αL0ΔT\Delta L = \alpha L_0 \Delta T

Length change due to temperature.

Variables

SymbolDescriptionUnit
σ\sigmaStressPa
ε\varepsilonStrain
EEYoung's modulusPa
α\alphaThermal expansion coefficient1/°C
ΔT\Delta TTemperature change°C

Environmental Engineering Reference

Wind Energy Fundamentals

The kinetic energy available in wind is given by:

P=12ρAv3P = \frac{1}{2} \rho A v^3

where PP is power (W), ρ\rho is air density (kg/m³), AA is the swept area (m²), and vv is wind speed (m/s).

For a circular turbine rotor: A=πr2A = \pi r^2

Wind Chill Index

The North American Wind Chill Index (2001) formula:

Twc=13.12+0.6215Ta11.37v0.16+0.3965Tav0.16T_{wc} = 13.12 + 0.6215T_a - 11.37v^{0.16} + 0.3965T_a v^{0.16}

where TwcT_{wc} is the wind chill temperature (°C), TaT_a is the air temperature (°C), and vv is the wind speed at 10 m height (km/h).

Hydropower

The theoretical power available from hydropower:

P=ρgQHP = \rho g Q H

where PP is power (W), ρ\rho is water density (≈1000 kg/m³), gg is gravitational acceleration (9.81 m/s²), QQ is flow rate (m³/s), and HH is head (m).

Accounting for efficiency:

Pactual=ηρgQHP_{actual} = \eta \rho g Q H

where η\eta is the overall efficiency (typically 0.7–0.9).

Solar Energy

Daily solar energy on a surface:

E=0TI(t)dtE = \int_0^T I(t) \, dt

where I(t)I(t) is the solar irradiance (W/m²) as a function of time.

Solar heat gain through glazing:

Qsolar=ASHGCIQ_{solar} = A \cdot SHGC \cdot I

where SHGCSHGC is the Solar Heat Gain Coefficient (dimensionless, 0–1) and II is incident solar radiation (W/m²).

Degree-Day Calculations

Heating Degree-Days (HDD):

HDD=i=1nmax(TbaseTavg,i,0)HDD = \sum_{i=1}^{n} \max(T_{base} - T_{avg,i}, \, 0)

Cooling Degree-Days (CDD):

CDD=i=1nmax(Tavg,iTbase,0)CDD = \sum_{i=1}^{n} \max(T_{avg,i} - T_{base}, \, 0)

where TbaseT_{base} is the base temperature (commonly 18°C / 65°F) and Tavg,iT_{avg,i} is the daily average temperature.

Salinity Classifications

References