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UNIVERSITY OF CALIFORNIA RIVERSIDE

WRAP Regional Modeling Center

Section 308 Results   -   Supported by: Western Regional Air Partnership

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2002 CMAQ Performance Evaluation Appraoch

Evaluation by Model Sub-region

For continental scale modeling of regional haze we expect considerable variation in model performance by geographical region, for example, coastal versus mountainous sites and the eastern US (high sulfur) versus the western US (low sulfur) sites. Therefore, it is useful to divide the model domain into different georgraphical regions when compiling model performance metrics.

Listed below are several proposals for grouping IMPROVE sites into model performance evaluation zones:
We seek input on the draft perfomanace zones so that we can revise the UCR model evaluation software to genrerate performance metrics for appropriately defined sub-regions. Important issues to consider include:

Stratification by Site Type

We also expect variation in model performance either by type of site, i.e., urban versus rural versus remote environements. Thus it might also be useful to stratify the ambient monitoring data according to site type. To some extent the design of the monitoring networks themselves address the issue of site type for example,the IMPROVE sites are only located at remote sites. For other networks such as the AQS, for example, the sites are not stratified by type, and additional effort will be needed to stratify these data for mdoel performance evaluations. One possible stratification scheme of AQS sites is:

Evaluation by Meteorological Conditions

Currently we evaluate model performance by season: Winter, Spring, Summer and Fall. We expect model performance within a season to vary depending on episodic meteorology conditions. We need to determine how best to stratify by episode: (e.g., by temperature, PBL Height, passage of frontal zones, etc.) Therefore, it would be more useful to stratify model performance results according to meteorology conditions. As in the case of greater sub-regional resolution, meteorology stratification will result in increased evaluation results, and new tools or methods will be needed to summarize model performance.


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