Transition of Radar Refractivity to Operational Radars OS&T Briefing, 6 April 2004 Interested...
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Transcript of Transition of Radar Refractivity to Operational Radars OS&T Briefing, 6 April 2004 Interested...
Transition of Radar Refractivity to Operational Radars
OS&T Briefing, 6 April 2004
Interested parties: NCAR, McGill University, NEXRAD Office of Science and Technology, Federal Aviation Administration, and University participants??
Convergence boundaries
22:57 UTC
Moisture gradients and convergence boundaries associated with thunderstorm development, June 12, 2002
Convergence boundaries
22:57 UTC
Moisture gradient
Moisture gradient
23:27 UTC23:27 UTC 00:01 UTC00:01 UTC 00:31 UTC00:31 UTC 00:40 UTC00:40 UTC
Forecasting Challenge: Tracking the “pockets” of boundary layer moisture so critical for convection initiation and growth.
Why REFRACTT
• Demonstrate feasibility on operational radars and motivate NWS and FAA to install refractivity on WSR-88D and TDWR
• Demonstrate forecast improvement in models and very short period forecasting techniques over a larger domain
• Improve basic understanding of the role of water vapor in convective storm initiation and storm evolution
• This is technology transfer of IHOP results to the operational community
100 km
-100 km
0 km
-100 km 0 km 100 km
S-Pol Radar
Boundary
WSR-88D’s
TDWR Radars
Satellite Derived Products: CAPE, CINLI, Precipitable Water,Soundings
Satellite FOV
Surface Mesonets
NWS/ResearchSoundingsAERI: ARM/CART
TV Radar (Local Station)
Spring 2006
REFRACTT
Refractivity Experiment For H20 Research And Collaborative operational Technology Transfer
Install refractivity on the national network of radars
Oklahoma
Future: Install refractivity on all available operational radars
ASR-9s
ASR-9s
λ = 5 cmPT = 250 kw0.5° pencil beam
λ = 10 cmPT = 1000 kw1.4° x 5° fan beam
TDWRs
TDWRs
FAA Radar Networks
Cost Function
Old t
orz
orv ZqGvwvuFJ
,
))(()),,((
VDRAS Boundary Layer Winds
• Test technique using IHOP data to produce stability fields (CAPE, CIN, and moisture)
• Test use of VDRAS stability fields in the Auto-Nowcaster
Assimilation of Refractivity into VDRAS
New equation t
ovN
orz
orv NqTpHZqGvwvuFJ
,
),,(())(()),,((
Juanzhen Sun
Refractivity Hourly HRLDAS Evaporation (mm)
18:00
Refractivity
16:00
Refractivity Soil Moisture
16:00
Soil Moisture
18:00
High Resolution Land Data Assimilation System (HRLDAS) Comparison of Refractivity Observations with
IHOP25 May 2002
Collaborative studies with Fei Chen
Data Processing: IHOP “Climatology”
Broad WNW-ESE refractivity and daily N gradient observed.Mimics (reflects?) climatological moisture gradient in the area.
Small-Scale Structure of N
Lesser variability in along-wind direction than across:• More mixing in along-wind direction via surface friction?• More advection-driven E-W gradients (across wind).
Timeline
2003 2004 2005 2006 2007
Prototype DevelopmentRefractivity on S-Pol’s RVP8
Prototype development on TDWR and ASR-9
ORDA (RVP8) installation
Prototype installation and testing on NSSL’s KOUN
Prototype installation and testing on ROC’s KCRI
Operational Radar Refractivity Test
Where are we currently ?
•Received the support of the NEXRAD TAC at the 28 October 2003 meeting.
•Coordinating with Bob Saffle on writing documentation for NWS Stage 1 and Stage 2 documents
•Weber and Parker (MIT/LL) have received high level (verbal not monetary) support for testing the refractivity technique on the TDWR testbed radar in OKC.
•Submitted a preliminary letter of intent to NCAR/ATD to request the SPol radar for REFRACT 2006
NCAR SPol Ground Clutter Map Oklahoma Panhandle – IHOP2002
Would like to see similar by-pass filter maps for selected NEXRAD radar sites. Cheryl Stephenson and Dave Zittel at ROC have been contacted.