A Comparison between Hurricane WRF and TWRF in Typhoon Track and Rainfall Forecast over the western North Pacific

Similar documents
Improvement and Ensemble Strategy of Heavy-Rainfall Quantitative Precipitation Forecasts using a Cloud-Resolving Model in Taiwan

Blending Analysis with Spatial Filter in TWRF: Application to Typhoon Prediction over the Western North Pacific Ocean

Impact of FORMOSAT 3/COSMIC Radio Occultation. near Taiwan

The GNSS-RO Data Impact on the Typhoon Predictions by MPAS-GSI Model

Using rainfall thresholds and ensemble precipitation forecasts to issue and improve urban inundation alerts

COSMIC GPS Radio Occultation and

The Use of GPS Radio Occultation Data for Tropical Cyclone Prediction. Bill Kuo and Hui Liu UCAR

Testing and Evaluation of GSI Hybrid Data Assimilation for Basin-scale HWRF: Lessons We Learned

Performance and Verification of HWRF/HMON Ensemble Prediction System in 2017 Real time Parallel Experiment. Zhan Zhang, Weiguo Wang

Impact of GPS RO Data on the Prediction of Tropical Cyclones

Numerical Prediction of Tropical Cyclones (PAGASA Experience)

Outline. Research Achievements

Striving Sufficient Lead Time of Flood Forecasts via Integrated Hydro-meteorological Intelligence

Typhoon Relocation in CWB WRF

Prediction of Tropical Cyclone Landfall Numbers Using a Regional Climate Model

Motivation & Goal. We investigate a way to generate PDFs from a single deterministic run

HWRF sensitivity to cumulus schemes

Comparison of Typhoon Track Forecast using Dynamical Initialization Schemeinstalled

High Resolution Ensemble Prediction of Typhoon Morakot (2009) May 11, 2011

The impact of assimilation of microwave radiance in HWRF on the forecast over the western Pacific Ocean

Performance of the 2013 Operational HWRF

An Impact Study of GPS RO Data on the Typhoon Track Forecast using the CWB Global Forecast System

Transitioning Physics Advancements into the Operational Hurricane WRF Model

Application of Mean Recentering Scheme to Improve the Typhoon Track Forecast: A Case Study of Typhoon Nanmadol (2011) Chih-Chien Chang, Shu-Chih Yang

1B-1: Verification of global and regional model forecasts for tropical cyclones affected Vietnam from

Development and research of GSI based hybrid EnKF Var data assimilation for HWRF to improve hurricane prediction

Overview of the NCEP Operational HWRF Modeling System

Preliminary evaluation of the impact of. cyclone assimilation and prediction

NCEP Operational Hurricane Modeling System. HWRF Performance Verification in 2015

Hypothesis for ESPC Demo #1: Flow-followingfinite-volume. Icosahedral

HMON (HNMMB): Development of a new Hurricane model for NWS/NCEP operations

Retrospective and near real-time tests of GSIbased EnKF-Var hybrid data assimilation system for HWRF with airborne radar data

Introduction to the HWRF-based Ensemble Prediction System

BASIN-SCALE HWRF: Evaluation of 2017 Real-Time Forecasts

Tropical cyclone track forecasts using JMA model with ECMWF and JMA initial conditions

Assessment of AHI Level-1 Data for HWRF Assimilation

Impact of assimilating the VIIRS-based CrIS cloudcleared radiances on hurricane forecasts

The Progresses of CMA Ensemble Prediction Systems and TIGGE/S2S data archive

On the assimilation of hyperspectral infrared sounder radiances in cloudy skies

NCEP Operational Hurricane Modeling System. HWRF Performance Verification in 2016

4.3.2 Configuration. 4.3 Ensemble Prediction System Introduction

Operational Hurricane Modeling at NCEP/EMC

Assimilation of Airborne Doppler Radar Observations Using the Unified GSI based Hybrid Ensemble Variational Data Assimilation System for HWRF

Numerical Weather Prediction: Data assimilation. Steven Cavallo

Curriculum Vitae A. EDUCATION

1.2 DEVELOPMENT OF THE NWS PROBABILISTIC EXTRA-TROPICAL STORM SURGE MODEL AND POST PROCESSING METHODOLOGY

Near-surface weather prediction and surface data assimilation: challenges, development, and potential data needs

Development of an Hourly- Updated NAM Forecast System

Recent Developments of JMA Operational NWP Systems and WGNE Intercomparison of Tropical Cyclone Track Forecast

Expansion of NCEP Operational Hurricane Weather Research and Forecast (HWRF) Model Forecast Guidance to all Global Tropical Cyclones

Improving Tropical Cyclone Forecasts by Assimilating Microwave Sounder Cloud-Screened Radiances and GPM precipitation measurements

School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou , China 2

Radiance Data Assimilation with an EnKF

Ting Lei, Xuguang Wang University of Oklahoma, Norman, OK, USA. Wang and Lei, MWR, Daryl Kleist (NCEP): dual resolution 4DEnsVar

The Impact of FORMOSAT-3/ COSMIC Data on Regional Weather Predictions

U.S.-Taiwan Workshop on the Advancement of Societal Responses to Mega-Disasters afflicting Mega-Cities. Introduction of Taiwan Typhoon and

Blending of Global and Regional Analyses with a Spatial Filter: Application to Typhoon Prediction over the Western North Pacific Ocean

A High-Quality Tropical Cyclone Reanalysis Dataset Using 4DVAR Data Assimilation Technique

The Impacts of GPSRO Data Assimilation and Four Ices Microphysics Scheme on Simulation of heavy rainfall Events over Taiwan during June 2012

Numerical Experiments of Tropical Cyclone Seasonality over the Western North Pacific

The EMC Mission.. In response to operational requirements:

The 2009 Hurricane Season Overview

University of Miami/RSMAS

Improvements to the NCEP Global and Regional Data Assimilation Systems

ABSTRACT 3 RADIAL VELOCITY ASSIMILATION IN BJRUC 3.1 ASSIMILATION STRATEGY OF RADIAL

COAMPS-TC 2015 Version, Performance, and Future Plans

Reduction of the Radius of Probability Circle. in Typhoon Track Forecast

Dynamical Statistical Seasonal Prediction of Atlantic Hurricane Activity at NCEP

The Impacts on Extended-Range Predictability of Midlatitude Weather Patterns due to Recurving Tropical Cyclones

Wassila Mamadou Thiaw Climate Prediction Center

Ensemble Prediction Systems

Performance and Application of CSPP/IMAPP in East China

The model simulation of the architectural micro-physical outdoors environment

HWRF Ocean: MPIPOM-TC

Precipitation Structure and Processes of Typhoon Nari (2001): A Modeling Propsective

Overview of HFIP FY10 activities and results

Current JMA ensemble-based tools for tropical cyclone forecasters

Hyperlocal Marine Weather: What s Happening?

A WRF-based rapid updating cycling forecast system of. BMB and its performance during the summer and Olympic. Games 2008

Focus on parameter variation results

Research on Climate of Typhoons Affecting China

QUANTITATIVE VERIFICATION STATISTICS OF WRF PREDICTIONS OVER THE MEDITERRANEAN REGION

HFIP ENSEMBLE PLAN. Jun Du (EMC/NCEP), presenting on behalf of the HFIP Ensemble Team:

Performance of TANC (Taiwan Auto- Nowcaster) for 2014 Warm-Season Afternoon Thunderstorm

Development Project High Resolution Numerical Prediction of Landfalling Typhoon Rainfall (tentative title)

Implementation and evaluation of a regional data assimilation system based on WRF-LETKF

GSI Data Assimilation System Support and Testing Activities: 2013 Annual Update

WGNE intercomparison of Tropical Cyclone Track forecast, 2007

AVIATION APPLICATIONS OF A NEW GENERATION OF MESOSCALE NUMERICAL WEATHER PREDICTION SYSTEM OF THE HONG KONG OBSERVATORY

Using a high-resolution ensemble modeling method to inform risk-based decision-making at Taylor Park Dam, Colorado

Assimilation of GPS RO Data for Tropical Cyclone Prediction with HWRF Chunhua Zhou1, Hui Shao1, Bill Kuo1 and Ligia Bernardet2

Comparison of Convection-permitting and Convection-parameterizing Ensembles

Statistical Characteristic of Heavy Rainfall Associated with Typhoons near Taiwan Based on the High-Density Automatic Rain Gauge Data

Observing system experiments of MTSAT-2 Rapid Scan Atmospheric Motion Vector for T-PARC 2008 using the JMA operational NWP system

The role of testbeds in NOAA for transitioning NWP research to operations

EMC Probabilistic Forecast Verification for Sub-season Scales

Section 9. Development of and studies with coupled ocean-atmosphere models

16D.4 Evaluating HWRF Forecasts of Tropical Cyclone Intensity and Structure in the North Atlantic Basin

The Model Simulation of the Architectural Micro-Physical Outdoors Environment

Recent COAMPS-TC Development and Future Plans

Transcription:

A Comparison between Hurricane WRF and TWRF in Typhoon Track and Rainfall Forecast over the western North Pacific Chin-Cheng TSAI 1, Ling-Feng HSIAO 1, Der Song CHEN 2, Jian-Wen BAO 3 1 Taiwan Typhoon and Flood Research Institute, Taiwan, 2 Central Weather Bureau, Taiwan, 3 NOAA Earth System Research Laboratory, United States 216/4

Hurricane WRF in Taiwan TTFRI and CWB collaborated with ESRL/NOAA and had successfully implemented the Hurricane WRF(HWRF) model in Taiwan since 212. In Apr. 213, TTFRI and CWB had the operational version of HWRF from EMC. TTFRI had added 2 HWRF members into Taiwan Cooperative Precipitation Ensemble Forecast Experiment (TAPEX) from 212 to 213. HWRF 215 operational version updated in Oct. 215.

Configuration of HWRF Experiment cold/warm analysis bogus Cu. M.P. PBL Note HWRF (M22) cold start NODA HWRF bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 2 way; 27/9/3km; moving; no ocean couple & no GSI; IC&BC from NCEP T574 atmospheric spectral data and include NCEP.5deg data. HWRF_T (M21) cold start NODA no bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 1 way; 45/15/5km; static; no ocean couple & no GSI; IC&BC from NCEP.5deg data. Moving domain Static domain 3

Track error(km) 213-214 TTFRI HWRF vs. EMC HWRF 2 15 213-14EMC_HWRF 213-14TTFRI_HWRF 128 125 156 155 188 188 1 11 94 5 53 28 51 26 75 72 (74) 12(65) 24(593) 36(532) 48(475) 6(417) 72(362) Forecast hour(# of cases)

Configuration of HWRF Experiment cold/warm analysis bogus Cu. M.P. PBL Note HWRF (M22) cold start NODA HWRF bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 2 way; 27/9/3km; moving; no ocean couple & no GSI; IC&BC from NCEP T574 atmospheric spectral data and include NCEP.5deg data. HWRF_T (M21) cold start NODA no bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 1 way; 45/15/5km; static; no ocean couple & no GSI; IC&BC from NCEP.5deg data. Moving domain Static domain 5

The Comparison of HWRF and TWRF in 213 Track Error 25 TS score.45 2 15 1 5 TWRF HWRF_static.4.35.3.25.2.15.1.5.4.38.21.18.33.17.17.9. 5mm 13mm 2mm 35mm 24H-accumulated 6

MSLP of HWRF_T(45/15/5km) has Bull s eye Reduce terrain resolution >> adjust ptsgm level from 2hPa to 42hPa(HWRF) 6/2 18Z +18fhr 7/11 Z +42fhr 6/24 Z +12fhr 7/12 Z +24fhr

Bull s eye of MSLP had significantly reduced when increasing the resolution(27/9/3km) 6/2 18Z +18fhr 6/24 Z +12fhr 7/11 Z +42fhr 7/12 Z +24fhr

Configuration of HWRF Experiment cold/warm analysis bogus Cu. M.P. PBL Note HWRF (M22) cold start NODA HWRF bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 2 way; 27/9/3km; moving; no ocean couple & no GSI; IC&BC from NCEP T574 atmospheric spectral data and include NCEP.5deg data. HWRF_T (M21) cold start NODA no bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 1 way; 45/15/5km 27/9/3km; static; no ocean couple & no GSI; IC&BC from NCEP.5deg data. Moving domain Static domain 9

Cases study for HWRF_T(27/9/3km) Experiments M21:45/15/5 km,e_vert=43 CTL21: 27/9/3 km, e_vert=43 Cases with warning issued by CWB,213 Soulik 7W:TRK:78-1318Z,RAN:12-1212Z Cimaron 8W:TRK:717-1812Z,RAN:18-1812Z Trami 12W:TRK:818-226Z,RAN:21-2112Z Kong-rey 14W:TRK:8266-312Z,RAN:286-2818Z Usagi 17W:TRK:91618-23Z,RAN:218Z-216Z Fitow 22W:TRK:9312-7Z,RAN:56-518Z

Track error(km) Track error of 6 warning TCs 12 cases had been finished 18 16 14 12 1 8 6 4 2 M21 CTL21 113 131 13 93 18 9 53 51 3 168 167 145 147 (12) 12(18) 24(96) 36(84) 48(73) 6(63) 72(53) Forecast hour(# of cases)

24-hour accumulated rainfall for Typhoon FITOW(213) OBS 56Z 512Z 518Z 5km CTL CTL CTL 3km

Precipitation skill score (6 TCs,18cases).6.5.4.3.2.1.52.48 TS.33.24.15.13 5mm 13mm 35mm Threshold M21 CTL21.7.6.5.4.3.2.1.61.54 BS.47.3.26.21 5mm 13mm 35mm Threshold M21 CTL21.4.35.3.25.2.15.1.35.32 ETS.24.18.14 5mm 13mm 35mm Threshold M21 CTL21.12.4.35.3.25.2.15.1.5.9.7 FAR.23.16 5mm 13mm 35mm Threshold.36.36 M21 CTL21

Track Error HWRF with static domain in 214 In typhoon season 214 horizontal resolution :27/9/3 km ; vertical resolution 43 levs But the track performance was poor after 36 forecast hour. 35 3 25 2 typhoon MATMO and FUNG-WONG(214) HWRF_static_28lev_d2 HWRF_static_d2 218 TWRF_d2 192 271 231 335 263 15 1 5 49 45 68 62 64 18 99 74 155 138 98 115 127 15 (36) 12(32) 24(28) 36(24) 48(22) 6(19) 72(12) Forecast hour(# of cases) 14

BIAS BIAS BIAS Threat Score Threat Score Threat Score Rainfall forecast skill score of typhoon FUNG-WONG&MATMO (18 cases).6.5.4.3.2.1 MATMO&FUNG-WONG(214) -24 fhr HWRF_static HWRF_static_28Lev TWRF.6.5.4.3.2.1 5 8 13 2 35 5 Threshold MATMO&FUNG-WONG(214) 24-48 fhr HWRF_static HWRF_static_28Lev TWRF 5 8 13 2 35 5 Threshold.6.5.4.3.2.1 MATMO&FUNG-WONG(214) 48-72 fhr HWRF_static HWRF_static_28Lev TWRF 5 8 13 2 35 5 Threshold 3 2.5 2 1.5 1.5 MATMO&FUNG-WONG(214) -24 fhr HWRF_static HWRF_static_28Lev TWRF 5 8 13 2 35 5 Threshold 3 2.5 2 1.5 1.5 MATMO&FUNG-WONG(214) 24-48 fhr 3 HWRF_static HWRF_static_28Lev TWRF 2.5 2 1.5 1.5 5 8 13 2 35 5 Threshold MATMO&FUNG-WONG(214) 48-72 fhr HWRF_static HWRF_static_28Lev TWRF 5 8 13 2 35 5 Threshold 15

Configuration of HWRF static Experiment cold/warm analysis bogus Cu. M.P. PBL Note HWRF static cold start NODA no bogus SAS Ferrier NCEP GFS 43levels; P_top 5hPa; 1 way; 27/9/3km; static; no ocean couple & no GSI; IC&BC from NCEP.5deg data. HWRF static cold start NODA no bogus BMJ Ferrier NCEP GFS 43levels; P_top 5hPa; 1 way; 27/9/3km; static; no ocean couple & no GSI; IC&BC from NCEP.5deg data. Warning issued by CWB,215 NOUL CHAN-HOM LINFA SOUDELOR GONI DUJUAN Static domain 16

Forecast Track Error of SAS vs BMJ 1 6 2-2 -6-1 HWRF_static_SAS_d2 HWRF_static_BMJ_d2 mean 95%- 95%+ 6 TCs in 215, warning issued by CWB (7) 6(65) 12(6) 18(58) 24(51) 3(44) 36(4) 42(37) 48(32) 54(28) 6(23) 66(19) 72(14) 35 3 25 2 15 1 5 17

95% C.I. Rainfall r.m.s.e. Rainfall forecast ability of SAS and BMJ 6 4 2 766 stations in TAIWAN, 65 initial times 9 8 7 6-2 -4 5 4 3 2 1-6 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 37 39 41 43 45 47 49 51 53 55 57 59 61 63 65 67 69 71 73 75 77 Forecast Hour SAS_rmse BMJ_rmse mean 95%- 95%+ 18

Summary & future work of Hurricane WRF We successfully implemented HWRF system in Taiwan and evaluated the track and rainfall forecast performance of HWRF over WNP from 213-214. For static domain HWRF configuration with higher vertical(43levs) and horizontal(3 km) resolution can have better capabilities in forecasting typhoon track and rainfall. But it s rainfall forecast ability still poor than TWRF. A sensitivity test of model cumulus scheme had been done to evaluate the track and rainfall forecast ability between SAS and BMJ scheme. 6 TCs cases show that BMJ performs better during 18-24H in track forecast and 25-35H in rainfall forecast. To update the 215 operational HWRF version and continue evaluating the performance over the WNP. 19

Thanks for your attention