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High resolution radar data and products over the Continental United States Valliappa.Lakshmanan@noaa.gov National Severe Storms Laboratory Norman OK, USA.

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Presentation on theme: "High resolution radar data and products over the Continental United States Valliappa.Lakshmanan@noaa.gov National Severe Storms Laboratory Norman OK, USA."— Presentation transcript:

1 High resolution radar data and products over the Continental United States
National Severe Storms Laboratory Norman OK, USA

2 Evolution of WDSS 1993-1998 1995-2000 2003 2005 Single-radar
SCIT, MDA, TDA Now part of RPG Single-radar with multi-sensor input NSE inputs Scheduled for ORPG-8 2003 Multi-radar multi-sensor over regional domain (1000km x 1000 km) Gridded products Shipped to select WFOs Used in Storm Pred. Center Product gen. for AWIPS? 2005 Multi-radar multi-sensor over CONUS CONUS 1km grids Available on the Internet Used in SPC 18 September 2018

3 What products? How often?
Gridded hail products Reflectivity at constant temperature levels and layer averages Low-level and mid-level shear and rotation tracks Short-term forecast fields Lightning Density More … Spatial Resolution: 0.01 deg x 0.01 deg [x 1km] resolution Approximately 1km x 1km throughout Continental United States. 1km in height Temporal resolution: 2D reflectivity mosaics every 2 minutes 3D and derived products every 5 minutes 18 September 2018

4 How does it work? The process for creating 2D composites:
Ingest Level-II radar data tilt by tilt QC reflectivity data (Lak06, JAM, review) Create virtual volume composites Merge composites from all the CONUS radars (Lak06, WF, accepted) 2nd level of QC -- using satellite and surface temperature data. 18 September 2018

5 Virtual volume composite
In a traditional composite, Process volume-by-volume. Take maximum of all tilts. Need to wait for end of volume. In a virtual volume composite: Process tilt-by-tilt. Keep a running volume. Replace older data each time. Take maximum of most current tilts. No need to wait for end of volume scan. A virtual volume provides more timely data. at19.5 at0.5 18 September 2018

6 Why do QC? On a single-radar product, users may:
want to see clear-air returns. tolerate more clutter tolerate test patterns, etc. On a multi-radar product, clutter and clear-air returns are distracting. 18 September 2018

7 Impact of QC raw With QC’ed composites Left: What we would get if directly combined raw (virtual volume) reflectivity composite data Clear-air return, sun strobes, test patterns Right: combining QCed virtual volume reflectivity composite The QC is performed radar-by-radar Takes into account terrain, texture and vertical structure. 18 September 2018

8 Second level of QC The radar QC is conservative
Doesn’t always remove non-precipitation echo Especially if it is biological i.e. moving. A second level of QC looks at satellite and surface temperature and retains echo where there is likely to be clouds. Bad data (bloom) No clouds 18 September 2018

9 What do we do with the composite?
The 2D radar mosaic is created every 2 minutes at 1km resolution. Converted to Grib2 and sent to the SPC. Put on the Internet: Snapshots with map background Converted to Geotiff Loadable with Google Earth or any GIS software. Google Earth does real-time loading Talk in IIPS on Tuesday Not 24x7 The software is licensed by some private companies They run it on their own machines. They take care of 24x7 reliability. 18 September 2018

10 2D vs 3D The 2D composite is cheap to create Need to compute in 3D
5 dual-Xeon machines with 6 GB RAM But always provides an underestimate of true values. Need to compute in 3D Height of dBZ value important! Can incorporate NSE information by height A lot more products! The 3D products need: 5 dual-Xeon with 6 GB RAM 2 dual-Xeon with 16 GB RAM 64-bit architecture composite from 2D: dBZ composite from 3D: dBZ 18 September 2018

11 The 3D flow Not just reflectivity.
Compute shear (Smith05) and low-level shear. Process lightning 18 September 2018

12 3D processing Combine QC’ed reflectivity in 3D Combine AzShear in 3D
Compute hail diagnosis and layer averages. Compute storm motion from composite. Use it to advect storms for short-term forecast. 18 September 2018

13 Example products Extracted from the real-time generation on Jan. 11, 2006 The day I created this presentation! We haven’t run the CONUS system in Spring yet, so the severe weather products may be underwhelming. 18 September 2018

14 Reflectivity products
Composite from 2D Composite from 3D Height of Max Ref Which radars? 18 September 2018

15 Azimuthal shear products
30 minute rotation tracks Azimuthal shear 0-3km MSL 18 September 2018

16 Severe weather diagnosis
Also: Probability of Severe Hail Maximum Expected Hail Size VIL_Density VIL_of_the_day Other echo top dBZ levels Reflectivity at temp. levels VIL Convection Echo top (18 dBZ) 18 September 2018

17 Short-term forecast Reflectivity at T=0 Clusters
Reflectivity at T=30 (forecast) Southward motion 18 September 2018

18 Precipitation estimates
Instantaneous precip rate Ref closest to ground Just the 88D algorithm on CONUS Uses hybrid scan reflectivity Convective/stratiform segregration based on presence of hail 88D Z/R relationships. Not multi-sensor QPESUMS-II under development at NSSL. 2hr precip accum 18 September 2018

19 What do we do with these products?
The 3D products are created every 5 minutes 1km resolution (0.01deg x 0.01deg x 1km) Converted to Grib2 and sent to the SPC. Put on the Internet (not all of them): Snapshots with map background Converted to Geotiff Loadable with Google Earth or any GIS software. Google Earth does real-time loading Talk in IIPS on Tuesday Looking for the NWS to pick this up! 18 September 2018


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