A Story of the PSU Hurricane System

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Presentation transcript:

A Story of the PSU Hurricane System Group-meeting @ 20131212

The track of PSU EnKF system 2003, Snyder & Zhang, 1st time EnKF + radar (OSSE); 294 cites; 2004, Zhang et al., relaxing method in EnKF. 216 cites; 2004, Dowell & Zhang et al., 1st time real radar data EnKF assimilation; 166 cites; 2006, Zhang, Meng and Aksoy, MM5-EnKF; 73 cites; 2007, Meng & Zhang, multi-physics EnKF; 80 cites; 2008, Meng & Zhang, WRF-EnKF; 65 cites; 2008, Meng & Zhang, month-long experiment; 38 cites; 2009, Zhang et al., WRF+parallel-EnKF; real ground-based radar; cloud-resolving hurricane; Super-Observing (SO) method; SCL; 96 cites; 2012, Weng & Zhang, Airborne radar EnKF; airborne radar SO method; 18 cites; 2011, Zhang et al., real-time performance with large cases for airborne radar; 25 cites; 2014, cycling WRF-EnKF with all recon observations;

Ground-base Radar for Hurricane Humberto (2007): radars Reflectivity Mosaic

Ground-base Radar for Hurricane Humberto (2007) : intensity forecasts NoDA Operational Forecasts WRF-EnKF with Vr Zhang et al., 2009

Airborne Radar for Katrina The NOAA P3 flight track of the 050825I1 mission during August 25 2005 and KAMX composite reflectivity at 2000 UTC 25 Aug 2005, the middle point of time of the last leg over the 4.5 km horizontal resolution model domain. The colored lines with label are the tracks of flight leg – a line across the storm center. P3 LF composite reflectivity of the 1st leg at Aug 25, 2005.

Airborne Radar for Katrina Hurricane track (a), minimum sea level pressure (b) and maximum 10m wind speed (c) forecasts. (Weng&Zhang, 2012)

1st time real-time forecast for hurricane Ike (2008) 120h rain obs. Tracks Intensity Swatch 孟子曰:"天时不如地利,地利不如人和..." Mencius said, Opportunities of time vouchsafed by Heaven are not equal to advantages of situation afforded by the Earth, and advantages of situation afforded by the Earth are not equal to the union arising from the accord of Men. Vmax 120h rain prediction

Performance over 5-year cases NHC yearly intensity forecast error NHC yearly track forecast error PSU 5-year track forecast error PSU 5-year intensity forecast error Figure 1: NHC (a) track error, (b) intensity error. Zhang&Weng, 2014

PSU WRF-EnKF Cycling System ARW V3.4.1 Cumulus Grell-Devenyi ensemble (27 km domain only) Microphysics WSM 6-class graupel PBL YSU Surface Layer Monin-Obukov Land Surface thermal diffusion Radiation Rrtm / Dudhia Air-sea flux Green and Zhang Ocean 1-D 60-member ensemble Gaspairi & Cohn 99' covariance localization with varying RoI IC & BC: GFS using 3DVAR background uncertainty Hourly assimilation with TDR over all 3 domains D1: 379x244x27kmx44sigma D2: 304x304x9km D3: 304x304x3km There are 2 streams for PSU in 2012. Stream 1.5 named ATCF ID APSU is ARW deterministic forecast initialized with TDR data assimilation, while stream 2.0 ANPS is ARW deterministic forecast initialized with operational GFS analysis. Both of them have the same WRF model configuration. They have 3 domains with 27,9,3 km resolution, the out domain is fixed, the 2 inner domains are centered by the TCVital data. For TDR data assimilation, there are 60 members initialized with operational GFS and perturbed by WRFDA. ATCF IDs: APSU: stream 1.5, ARW 3-km deterministic forecast; PS01-10: stream 2.0, ARW 3-km ensemble forecasts.

PSU Cycling System Workflow WPS & real.exe 1(job)* 32(cores)*4 minnutes WRFDA perturb 16J*16* 14m (256 coers) BC perturb 3J *8c *2m 3-h WRF 61J*32* 20m 2928c Replace environment 3J *16c *8m EnKF 3J *128c *8~65m 3-h WRF 61J*32* 20m 2928c EnKF 3J *128c *8~65m (depend on the number of obs) 4 epochs: 00,06,12,18Z @+3:45h WRF Init 6J * 32 *8m 192c Replace mean 3J *16c *7m Replace environment 3J *16c *8m 14:36 15:46 16:04 14:28 Low Priority (submit after APSU and AP?? running) e.g. for 06Z, Starts @ 09:45 09:49 10:03 10:11 10:18 10:26 11:31 APSU: 1J *512c *130m 13:41 AP01~10: 10J *240c *180m 14:31 WPP & GFDL Tracker: 11J *16c *24m NCL plotting: 11J * 16c * 30m WPS & real.exe 1J *32c *24m BC perturb 10J *8c *2m Initial: arwenkf_step1_icbcs.sh 10:55 Assimilation: arwenkf_step2_anacycle.sh 11:20 11:22 Forecast: arwenkf_step3_forecast.sh WPS & real.exe 1(job)* 32(cores)*4 minnutes WRFDA perturb 16J*16* 14m (256 coers) BC perturb 3J *8c *2m EnKF 3J *128c *8~65m (depend on the number of obs) 12Z, Starts @ 15:45 /lfs2/projects/hfip-psu/yweng/D2013/APSU_Shell/run_APSU.sh WRF Init 6J * 32 *8m 192c Replace mean 3J *16c *7m Replace environment 3J *16c *8m 15:49 16:03 16:11 16:18 16:26

PSU Cycling System: retrospective cases over 2008-2012 Track errors Intensity errors PSU NoDA vs. PSU Cycling with conventional obs. PSU Cycling with con. obs. Vs. con.+recon obs. PSU NoDA vs. NHC

PSU 2013 real-time performance track (km) Vmax (kt) Bias-corrected Vmax (kt) Vmax (kt) without homo Mean absolute forecast errors homogeneously averaged for 2013 stream 1.5 APSU (red), operational OFCL (cyan), GFS (purple), HWRF (blue) and GFDL (green). Only include the cases in ATCF a-deck files.

Benefited from Recon inner-core obs. 00Z 4 Oct PSU IC HWRF IC NOAA dropsondes for tropical storm Karen. 06Z 4 Oct MSLP (mb, contour), 10m winds (bar) and its wind speed (shaded) derived from the initial fields of APSU (left column) and HWRF (right column) at 00Z (top row) and 06Z (bottom row), respectively. These figures are produced by David Zelinsky.

Benefited from Recon inner-core obs. Track Track errors Intensity errors Intensity Track (top-left) and intensity (top-right) forecasts and their mean absolute forecast errors of track (bottom-left, unit: km) and intensity in the term of maximum surface wind speed (bottom-right, unit: knots) homogeneously averaged for 2013 stream 1.5 APSU (red), operational OFCL (cyan), GFS (pink), HWRF (blue) and GFDL (green) for tropical storm Karen.

Worse forecasts without inner-core obs. Intensity Track Track errors Intensity errors Operational forecast for Humberto

Summary EnKF had being developed over 13 years in our group. Real-time performance is a key step for EnKF. Where will we go? Real operation E4DVar Satellite Other convective systems