Report on EN6 DTC Ensemble Task 2014: Preliminary Configuration of North American Rapid Refresh Ensemble (NARRE)

Similar documents
Report on EN2 DTC Ensemble Task 2015: Testing of Stochastic Physics for use in NARRE

NCEP Short Range Ensemble Forecast (SREF) System: what we have and what we need? Jun Du. NOAA/NWS/NCEP Environmental Modeling Center

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

Development of an Hourly- Updated NAM Forecast System

HPC Winter Weather Desk Operations and 2011 Winter Weather Experiment Dan Petersen Winter weather focal point

AMPS Update June 2016

National Centers for Environmental Prediction: Building a Weather-Ready Nation

Introduction to NCEP's time lagged North American Rapid Refresh Ensemble Forecast System (NARRE-TL)

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

The National Weather Service of the Future: Building a Weather-Ready Nation

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

Toward improved initial conditions for NCAR s real-time convection-allowing ensemble. Ryan Sobash, Glen Romine, Craig Schwartz, and Kate Fossell

Verification as Diagnosis: Performance Diagrams for Numerical Forecasts of Severe Precipitation in California during the HMT Winter Exercises

Implementation and Evaluation of a Mesoscale Short-Range Ensemble Forecasting System Over the Pacific Northwest

Canadian Meteorological and Oceanographic Society and American Meteorological Society 21 st Conference on Numerical Weather Prediction 31 May 2012

New 16km NCEP Short-Range Ensemble Forecast (SREF) system: what we have and what we need? (SREF.v6.0.0, implementation date: Aug. 21.

Amy Harless. Jason Levit, David Bright, Clinton Wallace, Bob Maxson. Aviation Weather Center Kansas City, MO

Current and future configurations of MOGREPS-UK. Susanna Hagelin EWGLAM/SRNWP, Rome, 4 Oct 2016

SPC Ensemble Applications: Current Status and Future Plans

3.6 NCEP s Global Icing Ensemble Prediction and Evaluation

Plans for NOAA s regional ensemble systems: NARRE, HRRRE, and a regional hybrid assimilation

operational status and developments

Implementation and Evaluation of a Mesoscale Short-Range Ensemble Forecasting System Over the Pacific Northwest

Development of High-Resolution Rapid Refresh (HRRR) Ensemble Data Assimilation, Forecast and Post-Processing

CAPS Storm-Scale Ensemble Forecasting (SSEF) System

Unifying the NCEP Production Suite

Weather Hazard Modeling Research and development: Recent Advances and Plans

5.3 TESTING AND EVALUATION OF THE GSI DATA ASSIMILATION SYSTEM

Performance of the ocean wave ensemble forecast system at NCEP 1

Panel Session 8: Current Capabilities and Future Plans for Surface Transportation Weather Support

Aircraft-based Observations: Impact on weather forecast model performance

Convection-Resolving NWP with WRF. Section coordinator Ming Xue University of Oklahoma

HPC Ensemble Uses and Needs

Welcome to the 5 th NCEP Ensemble Users Workshop William. M. Lapenta Acting Director Environmental Modeling Center NOAA/NWS/NCEP

NOAA s Severe Weather Forecasting System: HRRR to WoF to FACETS

2012 and changes to the Rapid Refresh and HRRR weather forecast models

Linking the Hydrologic and Atmospheric Communities Through Probabilistic Flash Flood Forecasting

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

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

A study on the spread/error relationship of the COSMO-LEPS ensemble

Dynamic Ensemble Model Evaluation of Elevated Thunderstorms sampled by PRECIP

An Integrated Approach to the Prediction of Weather, Renewable Energy Generation and Energy Demand in Vermont

Development of High-Resolution Rapid Refresh (HRRR) Ensemble Data Assimilation, Forecasts and Post Processing

The EMC Mission.. In response to operational requirements:

Denver International Airport MDSS Demonstration Verification Report for the Season

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

CONDUIT Update Cooperative Opportunity for NCEP Data using IDD Technology Rebecca Cosgrove NCEP/NCO/Production Management Branch September 15, 2014

Ensemble Prediction Systems

Evaluation of Ensemble Icing Probability Forecasts in NCEP s SREF, VSREF and NARRE-TL Systems

Update on the KENDA project

WxChallenge Model Output Page Tutorial

Improvements to the NCEP Global and Regional Data Assimilation Systems

GSI DATA ASSIMILATION SYSTEM: COMMUNITY SUPPORT AND PRELIMINARY TESTING RESULTS

J11.5 HYDROLOGIC APPLICATIONS OF SHORT AND MEDIUM RANGE ENSEMBLE FORECASTS IN THE NWS ADVANCED HYDROLOGIC PREDICTION SERVICES (AHPS)

Unidata Policy Meeting Key Program Status

Transitioning NCAR s Aviation Algorithms into NCEP s Operations

Stochastic methods for representing atmospheric model uncertainties in ECMWF's IFS model

NDIA System Engineering Conference 26 October Benjie Spencer Chief Engineer, NOAA/National Weather Service

How ECMWF has addressed requests from the data users

weather forecast Improving NOAA models for energy Stan Benjamin, Boulder, CO USA Joseph Olson, Curtis Alexander, Eric James,

5.2 PRE-PROCESSING OF ATMOSPHERIC FORCING FOR ENSEMBLE STREAMFLOW PREDICTION

Potential Operational Capability for S2S Prediction

Assessment of Ensemble Forecasts

Focus on parameter variation results

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

ICON. Limited-area mode (ICON-LAM) and updated verification results. Günther Zängl, on behalf of the ICON development team

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

Hybrid variational-ensemble data assimilation. Daryl T. Kleist. Kayo Ide, Dave Parrish, John Derber, Jeff Whitaker

Jordan G. Powers Kevin W. Manning. Mesoscale and Microscale Meteorology Laboratory National Center for Atmospheric Research Boulder, CO

The Impact of Horizontal Resolution and Ensemble Size on Probabilistic Forecasts of Precipitation by the ECMWF EPS

A GSI-based convection-allowing EnKF and ensemble forecast system for PECAN

EMC Probabilistic Forecast Verification for Sub-season Scales

The WRF Developmental Testbed Center (DTC)

The benefits and developments in ensemble wind forecasting

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

The Role of Diagnostics in Numerical Weather Prediction

Moving to a simpler NCEP production suite

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

Application and verification of the ECMWF products Report 2007

Assessment of the Noah LSM with Multi-parameterization Options (Noah-MP) within WRF

AMDAR Global Status, Benefits and Development Plans*

Preliminary results. Leonardo Calvetti, Rafael Toshio, Flávio Deppe and Cesar Beneti. Technological Institute SIMEPAR, Curitiba, Paraná, Brazil

Ensemble forecast and verification of low level wind shear by the NCEP SREF system

COntinuous Mesoscale Ensemble Prediction DMI. Henrik Feddersen, Xiaohua Yang, Kai Sattler, Bent Hansen Sass

Hyperlocal Marine Weather: What s Happening?

Recent Data Assimilation Activities at Environment Canada

Numerical Weather Prediction. Meteorology 311 Fall 2016

Five years of limited-area ensemble activities at ARPA-SIM: the COSMO-LEPS system

Verification of ensemble and probability forecasts

The NOAA Operational Numerical Guidance System: Recent Changes and Moving Forward. William. M. Lapenta Acting Director Environmental Modeling Center

Concepts of Forecast Verification FROST-14

A Cycled GSI+EnKF and Storm-Scale Ensemble Forecasting (SSEF) Experiment

Upgrade of JMA s Typhoon Ensemble Prediction System

An Investigation of Reforecasting Applications for NGGPS Aviation Weather Prediction: An Initial Study of Ceiling and Visibility Prediction

COSMO Activity Assimilation of 2m humidity in KENDA

Allison Monarski, University of Maryland Masters Scholarly Paper, December 6, Department of Atmospheric and Oceanic Science

SPECIAL PROJECT PROGRESS REPORT

Jordan G. Powers Kevin W. Manning. Mesoscale and Microscale Meteorology Laboratory National Center for Atmospheric Research Boulder, Colorado, USA

Convection-Permitting Ensemble Forecasts at CAPS for Hazardous Weather Testbed (HWT)

Convective-scale data assimilation at the UK Met Office

Transcription:

Report on EN6 DTC Ensemble Task 2014: Preliminary Configuration of North American Rapid Refresh Ensemble (NARRE) Motivation As an expansion of computing resources for operations at EMC is becoming available through the support of the Sandy Supplemental Program, plans on how to best utilize these resources to address important forecasting questions have been made. One of the items on the EMC roadmap is an option to create an extension of the existing Short Range Ensemble Forecasting (SREF) system by adding the rapid refresh component. The idea is to have SREF continuing to run on 6- hourly cycles out to 84 forecast hours and NARRE will be a subset of 6 to 8 SREF members updated hourly and running out to 18-24 forecast hours. Having these members as a subset of SREF means that the model uncertainty, at least at the beginning, is going to be addressed by use of two dynamic cores ARW (RAP) and NAM (NMMB) and variations in physics. According to the EMC roadmap, this new system, consisting of 6 members, is expected to be implemented in operations during 2017 for improved aviation and probabilistic forecasts for other short- range applications. The work involves a very close collaboration between GSD, EMC and DTC staff. To further facilitate collaboration between the groups, common NARRE software versioning and revision control (SVN) will be in place by the end of the next DTC performance period, which is April 2016. The SVN development branch, to be set up by GSD, will contain all NARRE related code, including both data assimilation and modeling code. Initial work included development of preliminary configurations that were tested in retrospective experiments. Initialization will ultimately be hourly ( Rapid ), but for the initial testing, the DTC employed less frequent updates. The forecast length used in testing was 24 hrs. The final configuration will depend on computing resources dedicated to this task and discussions with EMC colleagues on pre- NARRE design. NARRE will be configured with 13- km horizontal grid spacing and 60 vertical levels. For the initial testing we used Rapid Refresh (RAP) operational domain, which is somewhat smaller than the domain the system will use in operations. Experiment Design As previously mentioned, NARRE consists of two dynamic cores, ARW and NMMB. The first task was to set up the domain on the same rotated lat/lon grid. The integration domain is the same as the RAP operational domain (Fig. 1), with horizontal grid spacing of 13 km. In operations, the system will run over the larger NAM operational domain. The decision was made to perform experiments using eight members, four coming from RAP and four from NAM models. In addition to

employing two different dynamic cores, model uncertainty is addressed by variations in physics. The experiment was designed to assess how physics diversity affects the ensemble performance. At the time, not many options for different physics packages were available for the NMMB members, so the decision was made to keep the operational physics suite for all NMMB members and perturb only initial and boundary conditions (Table 1). For this purpose, the control member was initialized with the Global Forecasting System (GFS) and the remaining three with three members of the Global Ensemble Forecasting System (GEFS). On the other hand, for ARW members, more physics variations were available, so changes were made in convection, surface physics, PBL physics, and microphysics. The majority of changes were based on combinations of the two, RAP and NAM, operational physics suites. In addition to the control being the RAP configuration, we added eight more members with variations in physics. The same initial and boundary conditions used for the NMMB members were used for the ARW members. Experiment testing, regarding the impact of the physics, focused on a five- day period: May 26-31, 2013. Three members were drawn out of the eight experimental RAP configurations and combined with the control RAP member and four NAM members for eight- member ensemble performance evaluation. This approach resulted in the evaluation of fifty- six different perturbations. For the purpose of assessing the ensemble performance when using variations in physics, the ensemble verification system developed by EMC was employed. To evaluate the fifty- six perturbations of physics, we focused on changes in a few key statistics: RMSE of the ensemble mean, the Spread/Error ratio and the Continuous Rank Probability Skill Score (CRPSS). On average, the difference between the best and the worst ensemble configuration ended up being 8% for the RMSE, 10% for Spread/Error ratio, and 5% in CRPSS. The configuration with the highest scores was selected and the chosen members are highlighted in blue in Table 1. Additional performance measures were evaluated, such as reliability diagrams and rank histograms. Figure 2 illustrates the reliability for 700- mb relative humidity and 850- mb temperature for three different lead times. It can be seen that for these fields reliability was generally good for all times, especially in the case of relative humidity. The 700- mb relative humidity rank histogram indicates some under dispersion, which is not too surprising for an ensemble with such a small number of members (Fig. 3). For the spread/skill measure, the ratio between the ensemble mean RMSE and the spread was evaluated. The ratio results for different lead times and various variables (T2m, T850, u10, v10, U500, V500 and RH700) are presented in Figure 4a. The values indicated fairly good spread skill correlation, with values relatively close to one for all variables. Similar analyses were performed when the same ensemble configuration was used for simulations of the cold season period (Figure 4b). The idea was to confirm that the same configuration would produce similar results for different seasons. Results are presented in Fig. 4b, and it can be seen that for the cold season, the spread- skill relation was slightly improved as compared to the warm season experiment. Based on these results, we proceeded with this configuration for real- time runs.

Since November 15, 2014, the preliminary NARRE configuration has been running in real time. In order to participate in HMT- WPC Winter Weather Experiment (WWE), NARRE had to run out to at least 48 hours. In the real- time mode, the rapid refresh component was employed only for ARW members (the rapid refresh infrastructure for NMMB members was not available at the time). ARW members were cycled hourly but 48- hour forecasts from all members were made only at 00Z and 12Z. Figure 1. Example of the RAP operational domain

Figure 2. Reliability diagrams for 700- mb relative humidity and 850- mb temperature for different lead times and warm season period of interest. Figure 3. Rank Histogram for 700- mb relative humidity for different lead times and the warm season period of interest.

Figure 4. Spread/Error ratio for 2- m temperature, 850- mb temperature, 10- m wind, 500- mb wind and 700- mb relative humidity for different lead times and two periods of interest.

Table 1. List of members tested. The green color indicates NMMB members and blue indicates ARW members selected based on the results of the experiment.