1. DUAL-POLARIZATION RADAR UPGRADE Emergency Manager Workshop Feb 5 2013 Chad Entremont

2. WHAT WILL BE COVERED What is dual-pol ? Why can we see a larger variety of targets ? What is dual-pol ? Why can we see a larger variety of targets ? Benefits of detecting different targets Benefits of detecting different targets – Snow / melting snow /melting layer – Hail cores – Better heavy rain detection – Tornadic debris detection

4. DIFFERENTIAL REFLECTIVITY (ZDR) Definition: Positive values of ZDR indicate that dominant hydrometeors are larger in the horizontal than in the vertical. Negative values indicate particles are larger in the vertical than the horizontal. Values near zero indicate that hydrometeors are similar in size in the vertical and horizontal. Definition: Positive values of ZDR indicate that dominant hydrometeors are larger in the horizontal than in the vertical. Negative values indicate particles are larger in the vertical than the horizontal. Values near zero indicate that hydrometeors are similar in size in the vertical and horizontal. Uses: ZDR can be used to help identify hail shafts, detect updrafts, determine rain drop size, and identify aggregation of dry snow. Uses: ZDR can be used to help identify hail shafts, detect updrafts, determine rain drop size, and identify aggregation of dry snow.

6. CORRELATION COEFFICIENT (CC) Definition: Correlation coefficient provides a measure of the consistency of the shapes and sizes of targets within the radar beam. A higher value shows a higher consistency in the size and shape of radar targets, while a lower value indicates greater variability in shapes and sizes. Definition: Correlation coefficient provides a measure of the consistency of the shapes and sizes of targets within the radar beam. A higher value shows a higher consistency in the size and shape of radar targets, while a lower value indicates greater variability in shapes and sizes. Uses: CC can be used to help distinguish between meteorological and non- meteorological targets, find the melting layer, identify giant hail, & identify tornadic debris. Uses: CC can be used to help distinguish between meteorological and non- meteorological targets, find the melting layer, identify giant hail, & identify tornadic debris.

9. CC

12. KDP is an indication of an increase in the size and concentration of rain drops, and thus, an increase in rain rate.

13. PRECIP ESTIMATIONS Dual Pol has shown to offer better precip estimates (most of the time) Dual Pol has shown to offer better precip estimates (most of the time) Issues still exist with inaccurate estimates Issues still exist with inaccurate estimates Should improve with time Should improve with time

15. TDS Hard to detect further away from radar

16. TDS EXAMPLE 0109Z Tornado started Tornado started Tight vel couplet 105kts gtg Tight vel couplet 105kts gtg Nrot 2.0 Nrot 2.0 Potential for a strong tornado per velocity data Potential for a strong tornado per velocity data CC data not indicating any TDS yet CC data not indicating any TDS yet

17. TDS EXAMPLE 0114Z TDS! Confirmed Tornado TDS! Confirmed Tornado CC hole,.45 to.55 CC hole,.45 to.55 A few ZDR values near Zero A few ZDR values near Zero KEYS! KEYS! – Collocated with circ – 45-53 dbz values Intese vel couplet 160kts gtg !! Intese vel couplet 160kts gtg !! Nrot 2.4 Nrot 2.4 Strong Tor very likely Strong Tor very likely

18. TRAINING LINKS http://www.srh.noaa.gov/jan/?n=dualpolupgrade http://www.wdtb.noaa.gov/courses/dualpol/Outreach/ index.html