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Comparing NBM probabilistic data to similar URMA elements

JK
Jared Klein, modified 1 Year ago.

Comparing NBM probabilistic data to similar URMA elements

Youngling Posts: 3 Join Date: 4/24/15 Recent Posts

I use the Comparisons tool in WSUP Viewer to evaluate NBM and NDFD performance for select elements in recent events. But unfortunately, the comparison options are limited to deterministic elements. It would be great to also provide verification analysis for probabilistic elements too. Results can be visualized in a number of ways:

(1) Simple Percentile - Obs to compute biases.  When a user selects PQPF, for example, both the value of the selected percentile and the URMA/RTMA QPE and NDFD (or another version of NBM) for the same period would plot along with the ability to toggle the "Delta" option on/off. Note:  I think you may be able to do this in WSUP already but only for 6-h snowfall.

(2) Assessing where meaningful exceedance thresholds were realized.  Taking it one step further, when the probability of exceedance for a particular exceedance threshold (e.g., Prob of MaxT >90F) is plotted, the footprint of the same observed (forecast) threshold (e.g., the 90F contour) from URMA/RTMA (NDFD/NBM) is outlined in the comparison pop-up window.

(3) Obs Rank in NBM Percentile Space.  It would be useful to have an option to compare the gridded observations (forecast) from URMA/RTMA (NFDF/NBM) to the full NBM probabilistic distribution. For example, loading NBM v4.2 PWind and URMA winds as the comparison option would compute the obs rank (or deterministic forecast rank if the compare dataset used is NDFD/NBM) in NBM percentile space. Selecting URMA as the comparison dataset to highlight areas of low and high biases in the NBM probabilistic data could provide insight into the degree of spatial variability and the magnitude of these biases for an event. Further analysis of the meteorological setup may help identify synoptic and mesoscale features that contributed to extreme low or high biases (e.g., snowfall exceeded the 95th percentile where the ingredients for mesoscale banding aligned). Note:  We can do analysis like this for snow/rainfall using the GAZPACHO program, but it could be much more adaptable if hosted on a cloud platform. See the example for a heavy rainfall event in the SE U.S. The shading in the first graphic represents the highest NBM PQPF percentiles that were exceeded in this event at each grid point. Analysis source:  AHPS. The second graphic is similar, but the percentile or deterministic NBM forecast that produced the lowest MAE (i.e., was closest to the analysis) is plotted.