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UPOS Terrestrial Weather Products

Dust Transport Application
DTA

Purpose:
CARMA-Dust (Community Aerosol Research Model from Ames/NASA) is a model for the forecast of dust storms and the prediction of dust concentration in the atmosphere. The model makes 72 hour forecasts of dust including the effects of winds, dust particle size and surface moisture using MM5 weather forecast data. The model includes the effects of atmospheric stability, winds and particle size in the forecast of dust aerosol concentrations.

The dust model was originally developed by Dr. Owen Toon and Pete Colarco at The University of Colorado, Boulder. The model has been modified by the Space Department at the Johns Hopkins APL to be use AFWA MM5 weather data to make world-wide daily dust forecasts.

The model uses a newly developed dust source database developed by Dr. Paul Ginoux at GIT/NASA GSFC. The Ginoux source model is a global dust data set developed using TOMS satellite data.

The CARMA-Dust model uses 10 particle sizes for dust ranging in size from 0.5 µm to 10 µm. Since larger dust particles have short airborne lifetimes on the order of several hours, larger particles have not been included.

The model uses 72 hour MM5 forecast data, with meteorological variables given on sigma pressure levels. Initial dust conditions are estimated in CARMA using a 48 hour model "spin-up". The spin-up uses the preceding 2 days of MM5 forecast data. The model then uses the initialized conditions and continues the run cycle through the 72 hour forecast time making dust concentration predictions every 3 hours.

Input:
MM5 forecast data.

Output:
The output of the CARMA model is a set of colored maps showing the total dust concentration at user selected heights above ground. The dust concentration maps use a log scale to cover concentrations from 10 µg/m3 (log(10)=1) to >10,000 µg/m3 (log(10,000)=4).

Dust concentrations in the atmosphere vary from less than 50 µg/m3 (normal atmosphere), >100 µg/m3 under hazy conditions, 1000 µg/m3 (reduced visibility, very hazy), to 5000 µg/m3 and higher in dust storm conditions. Note that severe dust storm conditions have been reported with concentrations exceeding 100,000 µg/m3. Satellite and airborne visibility are affected by dust concentration and particle size distribution with altitude.

Documents: (Adobe Acrobat PDF)
Quickstart
User's Guide
Requirements Document
Design Document
Test Plan
Support Plan
Version Description
The Application:
Dust Transport Application

For comments, questions, contact B. Barnum, JHU/APL


http://sd-www.jhuapl.edu/UPOS/CARMA/ © 2000 JHUAPL All rights reserved.