Comparing data from radar, rain gauges and a NWP model
Marco Gabella, Gianmario Galli, Juerg Joss, Giovanni E. Perona, Locarno Monti
Abstract
Marco Gabella, Gianmario Galli, Juerg Joss, Giovanni E. Perona, Locarno Monti
Abstract
Data from rain gages, radar and a high resolu- tion Numerical Weather Prediction (NWP) model are being analyzed. The accuracy of daily, operational, radar-derived precipitation amounts is verified during heavy rain in the Alps, using in situ measurements (71 gages within 157 km from the radar). Independent data were used for the train- ing and the verification of two adjustment techniques: even a simple bulk-adjustment (based on one correction coeffi- cient, hence, space-independent) leads to a significant im- provement; a Weighted Multiple Regression (WMR) is well worth the additional effort of deriving four coefficients to replicate the influences of calibration, beam-broadening, visibility and orography. Good agreement is found between daily radar/gauges amounts during severe precipitation. This confirms previous findings: in days with strong weather signal, the WMR is able to correct several errors in one step (calibration, beam-broadening, shielding and orographic enhancement). Since it does not require full volume 3D-data, it represents an inexpensive alternative to more sophisticated methods (e.g. reflectivity profile correction). The average forecast (over a 12 000 km 2 area) was in reasonable agree- ment with the average observations while the intense cells were shifted in space (they were forecast upstream, while they occurred upslope).
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Data from rain gages, radar and a high resolu- tion Numerical Weather Prediction (NWP) model are being analyzed. The accuracy of daily, operational, radar-derived precipitation amounts is verified during heavy rain in the Alps, using in situ measurements (71 gages within 157 km from the radar). Independent data were used for the train- ing and the verification of two adjustment techniques: even a simple bulk-adjustment (based on one correction coeffi- cient, hence, space-independent) leads to a significant im- provement; a Weighted Multiple Regression (WMR) is well worth the additional effort of deriving four coefficients to replicate the influences of calibration, beam-broadening, visibility and orography. Good agreement is found between daily radar/gauges amounts during severe precipitation. This confirms previous findings: in days with strong weather signal, the WMR is able to correct several errors in one step (calibration, beam-broadening, shielding and orographic enhancement). Since it does not require full volume 3D-data, it represents an inexpensive alternative to more sophisticated methods (e.g. reflectivity profile correction). The average forecast (over a 12 000 km 2 area) was in reasonable agree- ment with the average observations while the intense cells were shifted in space (they were forecast upstream, while they occurred upslope).
Key concepts: Orography, Radar, Meteorology, Numerical weather prediction, Environmental science, Calibration, Precipitation, Quantitative precipitation estimation