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Modeling Tips

  • May 15, 2020

AERMOD View: AERSURFACE 20060 in AERMET View

AERSURFACE is a tool developed by the U.S. Environmental Protection Agency (USEPA) which uses digital land cover data to objectively calculate numeric values of surface characteristics (i.e. albedo, Bowen ratio, and surface roughness) required by AERMET, the meteorological preprocessor for the AERMOD air dispersion model.

  • April 15, 2020

Met Data: Importing Hourly Surface Meteorological Data from Excel

Most users are aware of Lakes Environmental Software’s Import from Excel utility which reads hourly meteorological data from an Excel spreadsheet and generates a text-based data file in SAMSON format. The generated file can be used in a variety of air modeling applications.

  • March 16, 2020

CALPUFF View – Customizing Land Use Properties

A major step in any CALPUFF modeling study is to calculate geophysical properties of the modeling domain. The CALPUFF modeling system contains several preprocessors to perform these calculations.

  • February 17, 2020

CALPUFF View: Mapping Land Use Data in Shapefile Format

Land use data is vital to air quality modeling because the types of land cover encountered within the modeling domain play a big role in calculating atmospheric stability. Turbulence parameterization will be very different in a heavily populated urban area compared to a flat, grassy field or a large body of water. Digital land use data is available in a wide variety of formats, and the new CALPUFF View Version 9.0 now allows users to import land use data in shapefile format.

  • January 15, 2020

CALPUFF View: Modeling Sub-Hourly Time Steps

In past modeling tips, we have discussed how to estimate sub-hourly pollutant concentrations using AERMOD, a Gaussian plume dispersion model with an hourly minimum time step. Now we look at how a similar concept can be modeled using a different modeling system – CALPUFF.

  • December 16, 2019

AERMOD View: Modeling Urban Sources

Dispersion within urban environments has different characteristics than that occurring in a rural environment. The urban boundary layer will behave in a more convective, turbulent manner during the hours just after sunset due to the urban heat island effect. AERMOD has capabilities to model this boundary layer by enabling the urban dispersion coefficient.