Related Experiment Video
Updated: Feb 12, 2026

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas
Published on: April 3, 2018
Development of High-Resolution Dynamic Dust Source Function -A Case Study with a Strong Dust Storm in a Regional
Dongchul Kim1, Mian Chin2, Eric M Kemp3
1USRA at GSFC, Code 614, NASA Goddard Space Flight Center, Greenbelt, MD, USA.
A new high-resolution dynamic dust source improves weather models for predicting dust storms. This enhanced NASA Unified-Weather Research and Forecasting (NU-WRF) model better captures extreme events, though challenges remain in precise timing.
Area of Science:
- Atmospheric Science
- Environmental Science
- Geospatial Analysis
Background:
- Existing dust source models in weather forecasting lack sufficient resolution.
- Accurate dust source representation is crucial for predicting dust storm events.
Purpose of the Study:
- To develop and implement a high-resolution dynamic dust source within the NASA Unified-Weather Research and Forecasting (NU-WRF) model.
- To improve the simulation of dust storms, particularly extreme events.
Main Methods:
- Incorporated 1-km resolution topographic depression data.
- Derived surface bareness using Normalized Difference Vegetation Index (NDVI) from Moderate Resolution Imaging Spectroradiometer (MODIS) data.
- Integrated the new dynamic dust source into the NU-WRF model.
Main Results:
- The new dynamic dust source provides a more accurate representation of complex topography, especially in the Western United States.
- The enhanced NU-WRF model successfully simulated an extreme dust storm event in Phoenix, Arizona, which previous models could not.
- The model demonstrated improved magnitude representation compared to the older, coarser static dust source.
Conclusions:
- The high-resolution dynamic dust source significantly enhances the NU-WRF model's capability to simulate dust storms.
- Further research is needed to refine the model's ability to reproduce the temporal dynamics of short-lived, extreme dust storm events.
Related Concept Videos
Titration Calculations: Strong Acid - Strong Base
A titration is carried out for 25.00 mL of 0.100 M HCl (strong acid) with 0.100 M of a strong base NaOH. The pH at different volumes of added base solution can be calculated as follows:
(a) Titrant volume = 0 mL. The solution pH is due to the acid ionization of HCl. Because this is a strong acid, the ionization is complete and the hydronium ion molarity is 0.100 M. The pH of the solution is then:
Fruit Development, Structure, and Function
Strong Acid and Base Solutions
Titration of a Strong Acid with a Strong Base
Titration Calculations: Weak Acid - Strong Base
For the titration of 25.00 mL of 0.100 M CH3CO2H with 0.100 M NaOH, the reaction can be represented as:
IR Frequency Region: Fingerprint Region

