Global Repository | Documentation for the Hurricane Weather Research and Forecasting (HWRF) Model
Documentation for the Hurricane Weather Research and Forecasting (HWRF) Model
Summary
Note: The following information applies to the 2012 operational version of HWRF.
Model type: | Full physics, three dimensional dynamical model |
Model timeliness: | Late |
Model status: | Operational |
Basins run in: | AL, EP, WP, and IO |
ATCF TECH identifier: | HWRF |
Forecast period: | 0 to 126 hours |
Included in TCGP: | AL, EP, CP, WP, and IO |
Domain: | Three domains: D01 (parent domain): 216 x 432 points, 80 x 80 deg, 27 km grid spacing D02 (intermediate nest): 88 x 170 points, 11 x 10 deg, 9 km grid spacing D03 (inner nest): 154 x 272 points, 6.0 x 5.5 deg, 3 km grid spacing Domain top: 50 hPa |
Vertical coordinate (# of levels): | Sigma-pressure hybrid coordinates (42 levels) |
Grid: | Arakawa E-grid on rotated latitude and longitude projection |
Cumulus parameterization: | Simplified Arakawa-Schubert (SAS) scheme |
Microphysics parameterization: | Ferrier scheme |
Boundary layer parameterization: | GFS PBL (non-local mixing) |
Radiation parameterization: | GFDL radiation scheme |
Ocean coupling: | Full 3D POM coupled in AL basin, 1D POM coupled in EP basin and no ocean coupling in WP and IO basins |
Initialization method: | Grid-scale Statistical Interpolation (GSI) with vortex bogusing method |
Initial and boundary conditions: | Analysis and forecast data of NCEP Global Forecast System |
Primary contact: | Dr. Vijay Tallapragada, Hurricane Team Leader, NOAA/NWS/NCEP/EMC |
Official model website: | http://www.emc.ncep.noaa.gov/index.php?branch=HWRF |
Scientific documentation: | http://www.emc.ncep.noaa.gov/HWRF/HWRFScientificDocumentation2011.pdf |
User's Webpage (community code): | http://www.dtcenter.org/HurrWRF/users/ |
User's Guide: | http://www.dtcenter.org/HurrWRF/users/docs/users_guide/HWRF_UG_v3.4a.pdf |
HWRF Products Portal site: | http://www.emc.ncep.noaa.gov/gc_wmb/vxt/ |
Brief Technical Description
The HWRF system is one of the NOAA's operational regional hurricane models, which has two vortex following finer nest domains with grid space of 9 and 3km resolution respectively with75 by 75 degree outer most static domain (27km). The HWRF system consists of a set of pre-processors that include vortex initialization software, two numerical forecast models (one for atmosphere and one for ocean), and a set of post-processors. The atmospheric pre-processors of the HWRF include procedures of interpolating GFS spectral data to HWRF model grids, constructing an initial vortex consistent to observation, and assimilating observation data. The initial and lateral boundary data for the HWRF model are the final product of the pre-processors. A separate ocean initialization that includes feature based assimilation of oceanic conditions and a spin-up phase based on observed tropical cyclone location and intensity and will generate initial conditions for the ocean model. Using these IC/BC data, the HWRF coupled modeling system predicts the location and intensity of a storm up to five days into the future. The dynamic core of the HWRF model is originated from WRF-NMM while some of dynamic features are modified to hurricane conditions, such as horizontal diffusion, vortex following algorithm and other characteristics. The physics suite of the HWRF model is also designed towards more appropriate representation of tropical conditions. Some examples are modifying air-sea exchange coefficients and vertical diffusivity inside boundary layer. The post-processors of HWRF system are built upon NHC's requests. The major products are hurricane track and intensity at 6-hrly interval, high temporal frequency data for storm location, maximum wind and minimum pressure, swaths for maximum wind and rainfall totals, synthetic satellite imagery, vertical wind shear plot, vertical cross-sections of major variables and other graphical products generated from the model output.
References
The information in this page was provided by Young Kwon (NOAA/EMC) on 07 December 2012. It has been reviewed by Dr. Vijay Tallapragada.