An Improved Wind Probability Program: A Joint Hurricane Testbed Project Update Mark DeMaria and John Knaff, NOAA/NESDIS, Fort Collins, CO Stan Kidder,

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An Improved Wind Probability Program: A Joint Hurricane Testbed Project Update Mark DeMaria and John Knaff, NOAA/NESDIS, Fort Collins, CO Stan Kidder, CIRA/CSU, Fort Collins, CO Patrick Harr, Naval Postgraduate School, Monterey, CA Chris Lauer, NCEP/TPC, Miami, FL Presented at the Interdepartmental Hurricane Conference March 5, 2008

Monte Carlo Wind Probability Model 1000 track realizations from random sampling NHC track error distributions –Serial correlation and bias of errors accounted for Intensity of realizations from random sampling NHC intensity error distributions –Serial correlation and bias of errors accounted for –Special treatment near land Wind radii of realizations from radii CLIPER model and its radii error distributions –Serial correlation included Probability at a point from counting number of realizations passing within the wind radii of interest

1000 Track Realizations 64 kt h Cumulative Probabilities MC Probability Example Hurricane Dean 17 Aug UTC Major Hurricane Non-major Hurricane Tropical Storm Depression

Project Tasks 1.Improved Monte Carlo wind probability program by using situation-depending track error distributions Track error depends on Goerss Predicted Consensus Error (GPCE) 2.Improve timeliness by optimization of MC code 3.Update NHC wind speed probability table product Extend from 3 to 5 days Update probability distributions (currently based on )

Code Optimization Code profiling showed ~85% of CPU in distance calculation routine Automated procedure added to test for regular grid If yes, rectangular mask added at each time step to reduce number of distance calculations Speed up of ~600% for large grid –25 to 50% expected Implemented before 2007 season

Code Optimization Text Product Grid Graphical Product Grid

Wind Speed Probability Table

Developed by E. Rappaport and M. DeMaria as part of original NHC graphical products Limitations addressed by JHT project –Based on NHC error statistics –Extends only to 3 days Other limitations –Does not directly account for land interaction –Inconsistent with other probability products from MC model Rick Knabb and Dan Brown suggestion*: –Use output from MC model as table input –Addresses all of the above limitations –Will automatically update when MC model updates *via Dave Thomas

Wind Speed Probability Table Evaluation Procedure Examine MC model intensity probability distributions for idealized storms Compare MC intensity probabilities with WSPT values for real forecasts –Frances 29 Aug UTC –Katrina 24 Aug UTC –Katrina 27 Aug UTC –Ernesto 29 Aug UTC –Ernesto 29 Aug UTC –Humberto 12 Sep UTC –Humberto 12 Sep UTC –Ingrid 13 Sep UTC

Straight west track far from land Three cases: Constant max wind of 30, 90 and 150 kt Wind Speed Probability Table Idealized Storm Cases Straight north track close to land Three cases: Constant max wind of 30, 90 and 150 kt

MC Intensity Distributions Far from Land 30 kt fcst 90 kt fcst 150 kt fcst

MC Intensity Distributions 150 kt fcst far from and near land Far from land Near land

MC and Wind Speed Table Probability Comparison Hurricane France Example Nine Forecast Totals

Forecast-Dependent Probabilities Track plots courtesy of J. Vigh, CSU Operational MC model uses basin-wide track error distributions Can situation-dependent track distributions be utilized?

Goerss Predicted Consensus Error (GPCE) Predicts error of CONU track forecast –Consensus of GFDI, AVNI, NGPI, UKMI, GFNI GPCE Input –Spread of CONU member track forecasts –Initial latitude –Initial and forecasted intensity Explains 15-50% of CONU track error variance GPCE estimates radius that contains ~70% of CONU verifying positions at each time

Use of GPCE in the MC Model database of GPCE values created by NRL* Are GPCE radii correlated with NHC and JTWC track errors? –GPCE designed to predict CONU error How can GPCE values be used in the MC model? –MC model uses along/cross track error distributions *Buck: Domestic or Imported?

72 hr Atlantic NHC Along Track Error Distributions Stratified by GPCE ( )

NHC Along and Cross Track Error Standard Deviations Stratified by GPCE ( Atlantic Sample)

MC Model with Track Errors from Upper and Lower GPCE Terciles Lower Tercile Distributions Upper Tercile Distributions Hurricane Frances Sept 00 UTC Example 120 hr Cumulative Probabilities for 64 kt

Remaining Questions How to include GPCE in MC model –Method 1: Sample from appropriate tercile –Method 2: Include GPCE input in serial correlation correction Behavior in other basins Does GPCE correction improve probability verification? Real time tests beginning Aug 2008

Summary Code optimization is complete –Factor of 6 speed up Wind speed table product input from MC model is a reasonable approach –Implementation in 2008 GPCE-dependent MC model is promising –Further evaluation needed –Real time parallel runs in Aug 2008?