Improved high-impact weather HRRR/RAP forecast accuracy from assimilation of satellite-based cloud, lightning, convection, AMVs, fire, and radiance data.

Slides:



Advertisements
Similar presentations
Numerical Weather Prediction Readiness for NPP And JPSS Data Assimilation Experiments for CrIS and ATMS Kevin Garrett 1, Sid Boukabara 2, James Jung 3,
Advertisements

© The Aerospace Corporation 2014 Observation Impact on WRF Model Forecast Accuracy over Southwest Asia Michael D. McAtee Environmental Satellite Systems.
Adaptation of the Gridpoint Statistical Interpolation (GSI) for hourly cycled application within the Rapid Refresh Ming Hu 1,2, Stan Benjamin 1, Steve.
Rapid Refresh and RTMA. RUC: AKA-Rapid Refresh A major issue is how to assimilate and use the rapidly increasing array of off-time or continuous observations.
Transitioning unique NASA data and research technologies to the NWS 1 Radiance Assimilation Activities at SPoRT Will McCarty SPoRT SAC Wednesday June 13,
The 2014 Warn-on-Forecast and High-Impact Weather Workshop
Improved Simulations of Clouds and Precipitation Using WRF-GSI Zhengqing Ye and Zhijin Li NASA-JPL/UCLA June, 2011.
Rapid Update Cycle Model William Sachman and Steven Earle ESC452 - Spring 2006.
Global Forecast System (GFS) Model Previous called the Aviation (AVN) and Medium Range Forecast (MRF) models. Global model and 64 levels Relatively primitive.
Recent Progress on High Impact Weather Forecast with GOES ‐ R and Advanced IR Soundings Jun Li 1, Jinlong Li 1, Jing Zheng 1, Tim Schmit 2, and Hui Liu.
NOAA ESRL GSD Assimilation and Modeling Branch WoF / Hi-Impact Wx Workshop 1 April 2014 – Norman, OK From RAPv3/HRRR-2014 to the NARRE/HRRRE era Stan Benjamin.
Weather Model Development for Aviation Stan Benjamin and Steve Weygandt: Assimilation and Modeling Branch, Chief/Deputy NOAA Earth System Research Laboratory,
Warn on Forecast Briefing September 2014 Warn on Forecast Brief for NCEP planning NSSL and GSD September 2014.
Assimilation of GOES Hourly and Meteosat winds in the NCEP Global Forecast System (GFS) Assimilation of GOES Hourly and Meteosat winds in the NCEP Global.
Ensemble Numerical Prediction of the 4 May 2007 Greensburg, Kansas Tornadic Supercell using EnKF Radar Data Assimilation Dr. Daniel T. Dawson II NRC Postdoc,
Verification Summit AMB verification: rapid feedback to guide model development decisions Patrick Hofmann, Bill Moninger, Steve Weygandt, Curtis Alexander,
Assimilation of AIRS Radiance Data within the Rapid Refresh Rapid Refresh domain Haidao Lin Steve Weygandt Ming Hu Stan Benjamin Patrick Hofmann Curtis.
GSI EXPERIMENTS FOR RUA REFLECTIVITY/CLOUD AND CONVENTIONAL OBSERVATIONS Ming Hu, Stan Benjamin, Steve Weygandt, David Dowell, Terra Ladwig, and Curtis.
COSMO General Meeting, Offenbach, 7 – 11 Sept Dependance of bias on initial time of forecasts 1 WG1 Overview
Evaluation of satellite data assimilation impacts on mesoscale environment fields within the hourly cycled Rapid Refresh Haidao Lin Steve Weygandt Ming.
IMPROVING VERY-SHORT-TERM STORM PREDICTIONS BY ASSIMILATING RADAR AND SATELLITE DATA INTO A MESOSCALE NWP MODEL Allen Zhao 1, John Cook 1, Qin Xu 2, and.
Development of an EnKF/Hybrid Data Assimilation System for Mesoscale Application with the Rapid Refresh Ming Hu 1,2, Yujie Pan 3, Kefeng Zhu 3, Xuguang.
The NOAA Rapid Update Cycle (RUC) 1-h assimilation cycle WWRP Symposium -- Nowcasting & Very Short Range Forecasting – 8 Sept 2005 – Toulouse, France Stan.
AMB Verification and Quality Control monitoring Efforts involving RAOB, Profiler, Mesonets, Aircraft Bill Moninger, Xue Wei, Susan Sahm, Brian Jamison.
Outline Background Highlights of NCAR’s R&D efforts A proposed 5-year plan for CWB Final remarks.
WSN05 6 Sep 2005 Toulouse, France Efficient Assimilation of Radar Data at High Resolution for Short-Range Numerical Weather Prediction Keith Brewster,
NOAA/OAR report on recent JCSDA/satellite assimilation efforts 13 May 2015 Stan Benjamin - NOAA/ESRL Contributions from - ESRL/GSD – Haidao Lin (poster.
Development and Testing of a Regional GSI-Based EnKF-Hybrid System for the Rapid Refresh Configuration Yujie Pan 1, Kefeng Zhu 1, Ming Xue 1,2, Xuguang.
2006(-07)TAMDAR aircraft impact experiments for RUC humidity, temperature and wind forecasts Stan Benjamin, Bill Moninger, Tracy Lorraine Smith, Brian.
Evaluation of impact of satellite radiance data within the hybrid variational/EnKF Rapid Refresh data assimilation system Haidao Lin Steve Weygandt Ming.
Edward Mansell National Severe Storms Laboratory Donald MacGorman and Conrad Ziegler National Severe Storms Laboratory, Norman, OK Funding sources in the.
Evaluation of radiance data assimilation impact on Rapid Refresh forecast skill for retrospective and real-time experiments Haidao Lin Steve Weygandt Stan.
GSI applications within the Rapid Refresh and High Resolution Rapid Refresh 17 th IOAS-AOLS Conference 93 rd AMS Annual Meeting 9 January 2013 Patrick.
DRAFT – Page 1 – January 14, 2016 Development of a Convective Scale Ensemble Kalman Filter at Environment Canada Luc Fillion 1, Kao-Shen Chung 1, Monique.
NOAA/OAR report on recent JCSDA/satellite assimilation efforts 21 May 2014 Stan Benjamin - NOAA/ESRL ESRL/GSD talks Lidia Cucurull, Mariusz Pagowski, Haidao.
NOAA ESRL GSD Earth Modeling Branch Boulder, CO USA 6 th Conf on Weather/Climate/New Energy Economy January 2015 HRRR/RAP assimilation/model improvements.
The use of WSR-88D radar data at NCEP Shun Liu 1 David Parrish 2, John Derber 2, Geoff DiMego 2, Wan-shu Wu 2 Matthew Pyle 2, Brad Ferrier 1 1 IMSG/ National.
NCEP Production Suite Review
16th Annual WRF Users’ Workshop
Recent and Future Advancements in Convective-Scale Storm Prediction with the High- Resolution Rapid Refresh (HRRR) Forecast System NOAA/ESRL/GSD/AMB Curtis.
Assimilation of AIRS SFOV Profiles in the Rapid Refresh Rapid Refresh domain Haidao Lin Ming Hu Steve Weygandt Stan Benjamin Assimilation and Modeling.
A. FY12-13 GIMPAP Project Proposal Title Page version 04 August 2011 Title: Fusing Goes Observations and RUC/RR Model Output for Improved Cloud Remote.
Rapid Update Cycle-RUC. RUC A major issue is how to assimilate and use the rapidly increasing array of offtime or continuous observations (not a 00.
Lightning data assimilation in the Rapid Refresh and evaluation of lightning diagnostics from HRRR runs Steve Weygandt, Ming Hu, Curtis Alexander, Stan.
Satellite Data Assimilation Activities at CIMSS for FY2003 Robert M. Aune Advanced Satellite Products Team NOAA/NESDIS/ORA/ARAD Cooperative Institute for.
Towards Assimilation of GOES Hourly winds in the NCEP Global Forecast System (GFS) Xiujuan Su, Jaime Daniels, John Derber, Yangrong Lin, Andy Bailey, Wayne.
Land-Surface evolution forced by predicted precipitation corrected by high-frequency radar/satellite assimilation – the RUC Coupled Data Assimilation System.
Weather Model Development for Aviation Stan Benjamin and Steve Weygandt: Assimilation and Modeling Branch, Chief/Deputy NOAA Earth System Research Laboratory,
2004 Developments in Aviation Forecast Guidance from the RUC Stan Benjamin Steve Weygandt NOAA / Forecast Systems Lab NY Courtesy:
Global vs mesoscale ATOVS assimilation at the Met Office Global Large obs error (4 K) NESDIS 1B radiances NOAA-15 & 16 HIRS and AMSU thinned to 154 km.
WARN ON FORECAST AND HIGH IMPACT WEATHER WORKSHOP 09 February 2012 Use of Rapid Updating Meso‐ and Storm‐scale Data Assimilation to Improve Forecasts of.
HRRR Primary FAA-CoSPA NCEPESRL/GSD/AMB RAP Dev1 RAPv2 Primary HRRR Dev1 RAPv1 NCO RAP Dev2 RAP Retro HRRR Retro Retrospective Real-Time HRRR (and RAP)
RUC Convective Probability Forecasts using Ensembles and Hourly Assimilation Steve Weygandt Stan Benjamin Forecast Systems Laboratory NOAA.
GLFE Real-time TAMDAR Impact Experiments with the 20km RUC Stan Benjamin,Tracy Lorraine Smith, Bill Moninger, Brian Jamison NOAA Forecast Systems Laboratory.
June 20, 2005Workshop on Chemical data assimilation and data needs Data Assimilation Methods Experience from operational meteorological assimilation John.
NOAA Capabilities Relevant to DOE Solar Forecasting FOA (DE-FOA ) Webinar May 30, 2012.
Assimilation of AIRS SFOV retrievals in the Rapid Refresh model system Rapid Refresh domain Steve Weygandt Haidao Lin Ming Hu Stan Benjamin P Hofmann Jun.
Multi-scale Analysis and Prediction of the 8 May 2003 Oklahoma City Tornadic Supercell Storm Assimilating Radar and Surface Network Data using EnKF Ting.
Indirect impact of ozone assimilation using Gridpoint Statistical Interpolation (GSI) data assimilation system for regional applications Kathryn Newman1,2,
Rapid Update Cycle-RUC
Tadashi Fujita (NPD JMA)
High-Resolution Rapid Refresh (HRRR): WRF Enhancements and Challenges
Center for Analysis and Prediction of Storms (CAPS) Briefing by Ming Xue, Director CAPS is one of the 1st NSF Science and Technology Centers established.
Aircraft weather observations: Impacts for regional NWP models
Development of convective-scale data assimilation techniques for 0-12h high impact weather forecasting JuanzhenSun NCAR, Boulder, Colorado Oct 25, 2011.
Winter storm forecast at 1-12 h range
Aircraft-based Observations:
Rapid Update Cycle-RUC Rapid Refresh-RR High Resolution Rapid Refresh-HRRR RTMA.
WMO NWP Wokshop: Blending Breakout
New Developments in Aviation Forecast Guidance from the RUC
Presentation transcript:

Improved high-impact weather HRRR/RAP forecast accuracy from assimilation of satellite-based cloud, lightning, convection, AMVs, fire, and radiance data NOAA Satellite Science Week – 24 Feb 2015 Stan Benjamin, Steve Weygandt, Haidao Lin, Curtis Alexander, Ming Hu, Tracy Lorraine Smith NOAA/ESRL/GSD, Boulder, CO Outline HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high-impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite- based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Results from RAP OSEs (obs sensitivity experiments) from radiances and observations Rapid Refresh reflectivity - 0h valid 02z 26 Jan 2012 With lightning assim No lightning assim

Rapid Refresh and HRRR NOAA hourly updated models (situational awareness for energy, aviation, severe weather, etc.) Sat Science WeekFebruary 2015 HRRR/RAP sat assim – high-impact wx 2 13km Rapid Refresh (RAP) (mesoscale) 3km High Resolution Rapid Refresh (HRRR) (storm-scale) RAP HRRR Version 2 -- NCEP implement 25 Feb 2014 Version 3 – GSD Planned NCEP –June 2015 Initial -- NCEP implement 30 Sept 2014 Version 2 – GSD Planned NCEP –June 2015

Data assimilation for RAP and HRRR 3 RAP Data Assimilation cycle Observations Hourly cycling model HRRR EnKF- hybrid, Radar and Cloud anx

Hourly Observation TypeVariables ObservedObservation Count RawinsondeTemperature, Humidity, Wind, Pressure120 Profiler – 915 MHzWind, Virtual Temperature20-30 Radar – VADWind125 RadarRadial Velocity125 radars Radar reflectivity – CONUS3-d refl  Rain, Snow, Graupel1,500,000 Lightning(proxy reflectivity) GOEGOES-R, ground Aircraft Wind, Temperature2, ,000 Aircraft - WVSSHumidity Surface/METAR Temperature, Moisture, Wind, Pressure, Clouds, Visibility, Weather Surface/MesonetTemperature, Moisture, Wind~5K-12K Buoys/shipsWind, Pressure GOES AMVsWind AMSU/HIRS/MHS (RARS) Radiances1K-10K GOESRadianceslarge GOES cloud-top press/tempCloud Top Height100,000 GPS – Precipitable waterHumidity260 WindSat ScatterometerWinds2,000 – 10,000 RAPv3: Observations used (Sat-based) 4 HRRRv2 – all except radiances into 3km GSI assimilation

Hourly Observation TypeVariables ObservedObservation Count RawinsondeTemperature, Humidity, Wind, Pressure120 Profiler – 915 MHzWind, Virtual Temperature20-30 Radar – VADWind125 RadarRadial Velocity125 radars Radar reflectivity – CONUS3-d refl  Rain, Snow, Graupel1,500,000 Lightning(proxy reflectivity)NLDN Aircraft Wind, Temperature2, ,000 Aircraft - WVSSHumidity Surface/METAR Temperature, Moisture, Wind, Pressure, Clouds, Visibility, Weather Surface/MesonetTemperature, Moisture, Wind~5K-12K Buoys/shipsWind, Pressure GOES AMVsWind AMSU/HIRS/MHS (RARS) Radiances1K-10K GOESRadianceslarge GOES cloud-top press/tempCloud Top Height100,000 GPS – Precipitable waterHumidity260 WindSat ScatterometerWinds2,000 – 10,000 RAPv3: Observations used (new 2015) 5 HRRRv2 – all except radiances into 3km GSI assimilation

Arkansas tornadoes – Sunday 27 April 2014 ✖ ✖ 3 fatalities 8 fatalities HRRR (and RAP) Future MilestonesHRRR Milestones Arkansas Tornadoes Background Sat Science Week HRRR/RAP sat assim – high-impact wx 6

HRRR 6-hr fcst made at 2 PM for 8 PM 27 April Actual tornado path HRRR forecast rotation track Tornadic thunderstorm ✖ ✖ ✖ Fatalities Observed radar HRRR (and RAP) Future MilestonesHRRR Milestones HRRR Supercell Forecast Arkansas

HRRR 10-hr fcst made at 10 AM for 8 PM 27 April Observed radar HRRR forecast rotation track ✖ ✖ HRRR (and RAP) Future MilestonesHRRR Milestones HRRR Supercell Forecast Arkansas Actual tornado path Tornadic thunderstorm ✖ Fatalities HRRR

July 2, 2013 Yarnell, AZ Wildfire Perimeter Radar Reflectivity 4 PM MST June 30, 2013 Yarnell, AZ Yarnell, AZ Wildfire Background Last contact with fire crew ~ 4:30 PM MST (2330 UTC) Sun. 30 June, 2013 Wildfire Driven by thunderstorm outflow, 30 June 2013

Observed Radar (dBZ) HRRR Fcst Radar (dBZ) Yarnell HRRR Fcst 80m Wind (kts) Yarnell HRRR run at 12 pm MST Available by 2 pm MST HRRR (and RAP) Future MilestonesHRRR Milestones HRRR Wind Forecast Yarnell, AZ

z HRRR 0-h fcst 1200 PM MST Yarnell Observed Radar 0-h HRRR forecast 80 m AGL wind speed (kts) and direction (barbs) 0-h fcst HRRR forecast radar reflectivity HRRR forecast from 1900 UTC (noon MST) model run, which is available by 2 PM MST

HRRR 1-h fcst 2000 z 100 PM MST Yarnell Observed Radar HRRR 1-h HRRR forecast for 1 PM 80 m AGL wind speed (kts) and direction (barbs) 1-h fcst HRRR forecast radar reflectivity HRRR forecast from 1900 UTC (noon MST) model run, which is available by 2 PM MST

HRRR 2-h fcst 2100 z 200 PM MST Yarnell Observed Radar HRRR 2-h HRRR forecast for 2 PM 80 m AGL wind speed (kts) and direction (barbs) 2-h fcst HRRR forecast radar reflectivity Gust Front Edge HRRR forecast from 1900 UTC (noon MST) model run, which is available by 2 PM MST

HRRR 3-h fcst 2200 z 300 PM MST Yarnell Observed Radar HRRR 3-h HRRR forecast for 3 PM 80 m AGL wind speed (kts) and direction (barbs) 3-h fcst HRRR forecast radar reflectivity SW winds Gust Front Edge HRRR forecast from 1900 UTC (noon MST) model run, which is available by 2 PM MST

HRRR 4-h fcst 2300 z 400 PM MST Yarnell Observed Radar HRRR 4-h HRRR forecast for 4 PM 80 m AGL wind speed (kts) and direction (barbs) 4-h fcst HRRR forecast radar reflectivity Gust Front Edge HRRR forecast from 1900 UTC (noon MST) model run, which is available by 2 PM MST

HRRR 5-h fcst 0000 z 500 PM MST Yarnell Observed Radar HRRR 5-h HRRR forecast for 5 PM 80 m AGL wind speed (kts) and direction (barbs) 5-h fcst HRRR forecast radar reflectivity NE winds Gust Front Edge HRRR forecast from 1900 UTC (noon MST) model run, which is available by 2 PM MST

17 Outline HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high- impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite-based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Results from RAP OSEs (obs sensitivity experiments) from radiances and observations (including AMVs) Sat Science Week HRRR/RAP sat assim – high-impact wx 17

 Includes new sensors/data  GOES sounding data from GOES-15  AMSUA/MHS from NOAA-19 and METOP-B ;  Includes the direct readout (RARS) data  Removes some high-peaking channels to fit the model top of RAP, removes O 3 channels  Implemented the enhanced variational bias correction scheme with cycling Radiance DA updates for RAPv3 (mid NCEP implementation)

Radiance channels selected for RAP V2 AMSU-A (remove high-peaking channels) NOAA-15: channels 1-10, 15; NOAA-18: channels 1-8, 10,15; METOP-A: channels 1-6, 8-10,15 (removed channel 8 on 26 Sep per NCEP note) ; HIRS4 (remove high-peaking and O 3 channels) METOP-A: channels: 4-8, 10-15; MHS NOAA-18, METOP-A : channels 1-5;

Radiance channels selected for RAPv3 (2015) AMSU-A (remove high-peaking channels) NOAA-15: channels 1-10, 15; NOAA-18: channels 1-8, 10,15; NOAA-19: channels 1-7, 9-10, 15; METOP-A: channels 1-6, 8-10,15 (removed channel 8 on 26 Sep per NCEP note) ; METOP-B: channels 1-10, 15; HIRS4 (remove high-peaking and O 3 channels) METOP-A: channels: 4-8, 10-15; MHS NOAA-18/19, METOP-A/B : channels 1-5; GOES (remove high-peaking and ozone channels) GOES-15 (sndrD1,sndrD2,sndrD3,sndrD4): channels 3- 8, RARS - NOAA-15/18/19, METOP-A/B

Retrospective Experiments (RAPv2) Extensive retro run for bias coefficients spin up Control run (CNTL) – (conventional data only) 1-h cycling run, 8-day retro run (May 28 – June ) RAP Hybrid EnKF system (RAP V2) Real-time radiance (limited availability) CNTL + RAP real time radiance data (amsua/mhs/hirs4/goes) Use updated bias coefficients from the extensive retro run RARS + Real-time radiance (better availability) (RARS = Regional ATOVS Retransmission Services) Full coverage radiance (perfect availability) Using full data for AMSUA/MHS/HIRS4 (no data latency)

Impact from no/RARS/full data sets May28-June retro runs RARS included Real-time data hPa RMS mean Full data T emperature Relative Humidity Wind +2.5% +1.5% +3.5% Normalize Errors E N = (CNTL – EXP) CNTL 18 Hr Fcst Full data helps, esp. with wind fcsts, but also T and RH (over RARS)

6-h Forecast RMS Error improvements - Observation impact: radiance vs. raob Retro run (05/15/ /22/2013) upper-air verification Radiance impact raob impact Pairwise comparison Temperature Worse Better Relative Humidity Worse Better Wind Worse Better

RAP-radiance assimilation summary Direct-readout data especially important to hourly RAP Reduces data latency (necessary for RAP/HRRR) RAP system will get much more real-time radiance data by using RARS data Could still double radiance impact with zero latency 4-month data-impact RAP experiments with and without RARS direct readout data, 1-4% positive impact has been seen for temperature, moisture, and wind Much less than aircraft, slightly less than raob impact Direct readout will likely have more impact on 1h-12h forecasts with Global Rapid Refresh

RAP 2013 obs impact -20% Normalize: 6h Fcst – 0h Anx V – 1.8 m/s, RH – 6%, T – 0.5K Temperature RMS (K) [ hPa] Relative Humidity RMS (%) [ hPa] Wind RMS (m/s) [ hPa] Airc Raob Sfc GPS AMV +3h +6h +9h +12h Aircraft – largest impact wind/RH/temp – all have up to 20% reduction forecast error, especially 6h-9h fcsts Following in importance: Raob, Surface, GPS-Met, AMVs +3h +6h +9h +12h RAP data impact -- North America -- GSI/ensemble/hybrid DA -- May 2013 experiments -- 12z and 00z combined -20% 25

26 Outline HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high- impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite-based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Results from RAP OSEs (obs sensitivity experiments) from radiances and observations (including AMVs) Sat Science Week HRRR/RAP sat assim – high-impact wx 26

What is the cloud and precipitation hydrometeor (HM) analysis? Observations Merge HM field Update hydrometeors in the model state based on the cloud field. Map to HM field No cloud Cloud Unknown ceilometeors

WSR-88D Reflectivity ceilometeors What is the cloud and precipitation hydrometeor (HM) analysis? GOES cloud top pressure The 3 km model hydrometeors are updated based on cloud and precipitation observations to provide a high-resolution 3-d cloud (qr, qi) analysis.

3-d variables updated Add HM to 3-d model grid? Remove from 3-d model? Which observations are used? cloud water, cloud ice, temperature, water vapor Yes, below 1.2 km AGL Yes. Cloud trimming at night to ground added in 2015 Sat (GOES) cloud- top pressure/temp, METAR ceilometers Rain water, snow water Yes, for Zr < 28 dBZ for all temperatures. If 2m T < 5°C: add to full column, Else: add at observed maximum reflectivity level YesRadar reflectivity More details about the cloud and precipitation hydrometeor (HM) analysis Sat Science Week HRRR/RAP sat assim – high-impact wx 29

30 Outline HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high- impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite-based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Results from RAP OSEs (obs sensitivity experiments) from radiances and observations Sat Science Week HRRR/RAP sat assim – high-impact wx 30

Digital filter-based assimilation initializes ongoing / developing convection / precipitation regions Forward integration,full physics with obs-based latent heating -20 min -10 min Initial +10 min + 20 min RAP / HRRR model forecast Backwards integration, no physics Initial fields with improved balance, storm-scale circulation Reflectivity HRRR (and RAP) Future MilestonesHRRR Milestones Radar/lightning digital filter assimilation 31  Radar reflectivity  Lightning (GOES-R or ground)  Satellite cloud-top cooling rate Use for following obs types:

32 Outline HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high- impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite-based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Results from RAP OSEs (obs sensitivity experiments) from radiances and observations

Cloud-top cooling (CTC) assimilation NOAA/ESRL/GSD and UAH Tracy Lorraine Smith, Steve Weygandt // John Mecikalski RAP experiment: Analysis For 00h 25dBz 19z 19 June Improved CSI, POD, FAR with CTC RAP1h Forecast valid 20z 19 June 2014 CSI, POD same with CTC. Cloud-top cooling data from U.Alabama-Huntsville. Assimilation of larger cooling than -3K/15min. Next step: CTC assimilation at 3km in HRRR.

34 Outline HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high- impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite-based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Results from RAP OSEs (obs sensitivity experiments) from radiances and observations Sat Science Week HRRR/RAP sat assim – high-impact wx 34

35 HRRR-chem – assimilation of WFABBA HRRR-chem-3km PM25- surface 11h fcst valid 17z 24 Feb 2015

Example: RAP cold-start tests without/with aerosol-aware cloud microphysics. More small-scale cloud with more CCN over land. NCEP RAPv3/HRRRv Changes Use of forecast aerosol fields to have prognostic cloud- condensation nuclei (CCN). 36

ESRL – experimental version RAPv3 – GSD testing in 2014 Final RAP-primary impl - 1/1/2015 – Will initialize 2014 ESRL-HRRR(v2) – Improved PBL, LSM, cu-parm, DA – WRFv3.6.1 w/ Thompson/NCAR aerosol-aware microphysics HRRRv2 – GSD testing in 2014 – Final HRRR-primary impl - 1/1/2015 – Initialized by 2014 RAP (v3) – Improved radar assimilation, hybrid assimilation, PBL/cloud physics RAPv4 – GSD testing in 2015 – Hourly RAP ensemble data assimilation HRRRv3 – GSD testing in 2015 – Target: Improved 3km physics + improved data assimilation. NWS-NCEP - operational – Planned dates Implement June 2015 (domain expansion to NAM domain) Implement June 2015 (extension to 24h) Implement 2016 HRRR (and RAP) Future MilestonesHRRR Milestones RAP/HRRR Implementation Map 37

Improved high-impact weather HRRR/RAP forecast accuracy from assimilation of satellite-based cloud, lightning, convection, AMVs, fire, and radiance data HRRR (3km)/ RAP (13km) are the hourly updated models for NOAA. Focus – situational awareness, decision making for severe weather, transportation, energy, all-season high-impact weather. HRRR/RAP are only NOAA models that currently assimilate satellite- based cloud and radar reflectivity data HRRR/RAP additions at NCEP: lightning, radial wind, mesonet HRRR/RAP assimilation at ESRL – : Cloud-top cooling from GOES Fire data from ABBA, MODIS for HRRR-chem-smoke, RAPchem Direct readout radiance data from JPSS Initial testing of global cloud analysis (in progress) Rapid Refresh reflectivity - 0h valid 02z 26 Jan 2012 With lightning assim No lightning assim – storm-scale ens assimilation – GSI – 4dEnVar HRRR ensemble, toward 15-min update cycle (5 min) Satellite data – GOES-R+, JPSS/SNPP – critical to improve HRRR as primary short-range prediction of high-impact wx

Future work–RAP/GRR - direct-readout Include more direct readout data in real-time RAP and continue to test and evaluate their impact in real-time RAP Plan to include the AIRS direct readout data in RAP if available Plan to include direct readout data in RAP from SNPP and possible future JPSS Include the direct readout radiance data from NPP/JPSS for future hourly GSD Global Rapid Refresh