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Air Pollution Lab

Explore how temperature inversions trap pollutants near the surface and how wind speed affects dispersion. Adjust inversion height, strength, and wind to observe real-time changes in AQI, then collect data across multiple trials.

Guided Experiment: Temperature Inversion Investigation

If you decrease the inversion height while keeping wind speed constant, what do you predict will happen to air quality (AQI)?

Write your hypothesis in the Lab Report panel, then click Next.

Air Quality Visualization

Inversion at 500 m (+5 K)AQI137Wind: 2.0 m/s0 m500 m1000 m1500 m2000 m2500 m3000 m

Controls

Surface Temperature25 °C
Inversion Height500 m
Inversion Strength+5.0 K
Wind Speed2.0 m/s
Emission Rate50 units

Results

Air Quality Index
137
Unhealthy for Sensitive Groups
C=EH×u=50.0(box model)C = \frac{E}{H \times u} \quad = \frac{50.0}{\text{(box model)}}
PM2.5
50.0 μg/m³
Mixing Height
500 m
Ventilation Coeff.
1000 m²/s
Mixing Volume
1000 m³/m
Strong inversion — pollutants trapped near surface
Temperature at Inversion
26.8 °C

AQI vs Inversion Height

Data Table

(0 rows)
#TrialConditionSurface Temp(°C)Inversion Ht(m)Wind Speed(m/s)AQIMixing Vol(m³/m)PM2.5(μg/m³)
0 / 500
0 / 500
0 / 500

Reference Guide

Temperature Inversions

Normally, air temperature decreases with altitude. A temperature inversion reverses this, creating a warm layer above cooler surface air. This warm lid prevents vertical mixing and traps pollutants below.

Tinv=TsurfaceΓh+ΔTinvT_{\mathrm{inv}} = T_{\mathrm{surface}} - \Gamma h + \Delta T_{\mathrm{inv}}

where Γ is the lapse rate (6.5 K/km), h is the inversion height, and ΔT is the inversion strength. Los Angeles experiences frequent subsidence inversions due to the Pacific high-pressure system.

Box Model

The atmospheric box model estimates pollutant concentration by treating the mixing layer as a well-mixed box. Concentration depends on the emission rate and the ventilation coefficient.

C=EH×uC = \frac{E}{H \times u}

where E is the emission rate, H is the mixing height (m), and u is the wind speed (m/s). The ventilation coefficient V = H × u determines the atmosphere's capacity to dilute pollutants.

Air Quality Index

The EPA AQI converts pollutant concentrations into a 0-500 scale using piecewise linear breakpoint interpolation.

AQI=IhiIloChiClo(CClo)+Ilo\mathrm{AQI} = \frac{I_{\mathrm{hi}} - I_{\mathrm{lo}}}{C_{\mathrm{hi}} - C_{\mathrm{lo}}} (C - C_{\mathrm{lo}}) + I_{\mathrm{lo}}
0-50Good 51-100Moderate 101-150Unhealthy for Sensitive 151-200Unhealthy 201-300Very Unhealthy 301-500Hazardous

Ventilation Coefficient

The ventilation coefficient measures the atmosphere's ability to disperse pollutants. It combines the mixing height and transport wind speed.

Vc=H×u(m2/s)V_c = H \times u \quad (\mathrm{m^2/s})

Values below 6,000 m²/s indicate poor ventilation and high pollution potential. Weather services use this metric in air quality forecasts. Stagnation events (low wind + low mixing height) produce the worst air quality episodes.