the current status of the uw-cimss p75 advanced dvorak ...the uw-cimss advanced dvorak technique...

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The Current Status of the UW - CIMSS Advanced Dvorak Technique (ADT) Timothy Olander and Christopher Velden Cooperative Institute for Meteorological Satellite Studies (CIMSS) University of Wisconsin Madison Acknowledgements ADT research and development has been supported by ONR/NRL and NOAA/ NESDIS research programs. Algorithm Information Current Work Future Upgrades Another application requested by users is the ability to employ the ADT on subtropical systems. Preliminary work on this extension has begun and will focus on determining whether a bias adjustment, as with the ET work, or a new scene type (or modification of the current Curved Band type) is needed. Research led by Clark Evans from UW-Milwaukee to investigate an extension to the ADT for storms undergoing ET has suggested an intensity adjustment is needed. Two schemes to integrate this adjustment, utilizing Bob Hart’s cyclone phase space files to identify when ET begins, are being evaluated. P75 The UW-CIMSS Advanced Dvorak Technique (ADT) is a mature algorithm utilized to objectively estimate the intensity of tropical cyclones using geostationary infrared data and polar-orbiting passive microwave data. It is based upon the manual (and subjective) Dvorak Technique, but has advanced beyond the scope of the technique. The ADT is currently used around the world by many operational Tropical Cyclone Forecast Centers. A study of the most historically intense tropical cyclones from around the globe during the geo satellite era, as analyzed by the ADT, was performed to determine a “Top Ten” list. What was the strongest storm? Gilbert? Tip? Patricia? Wilma? Related Topics at AMS-TC2016 Webpage Real-time ADT intensity estimates and product information can be found on the CIMSS Tropical Cyclone website at : http://tropic.ssec.wisc.edu/real-time/adt Extratropical Transition Subtropical Storm Analysis Himawari-8/MTSAT Comparisons Hurricane Patricia ARCHER 2.0 Integration Latest Statistics Background Pre-Genesis Identification and Tracking McIDAS-V Integration Himawari-8 vs. MTSAT 25W Generally small differences; slight tendency for higher estimates using Himawari-8 10-min. vs. 30-min. Him-8 (still in evaluation) 28W Generally small differences but 10-min can yield a bit quicker response in emerging eye situations AIRCRAFT RECON Atlantic - 47 total matches bias aae stdv CI# 0.00 0.46 0.60 Wind(kts)-0.83 9.15 12.07 MSLP(mb) -0.89 8.06 10.62 E/C Pacific - 711 total matches bias aae stdv CI# 0.15 0.45 0.58 Wind(kts) 2.52 8.71 11.77 MSLP(mb) -1.98 7.61 10.49 W Pacific - 608 total matches bias aae stdv CI# -0.15 0.42 0.50 Wind(kts)-3.55 9.21 11.09 MSLP(mb) 3.26 7.55 10.99 Hurricane Patricia provided a unique and challenging test for the ADT due to its rapid intensification and extreme maximum intensity. When compared to aircraft reconnaissance, the real-time ADT provided remarkably accurate intensity estimates. HURRICANE PATRICIA DISCUSSION NUMBER 8 NWS NATIONAL HURRICANE CENTER MIAMI FL EP202015 400 AM CDT THU OCT 22 2015 “Patricia has become significantly better organized overnight, with an eye evident on infrared imagery, and the system now has well-defined convective banding features. The initial intensity estimate is set at 75 kt, which is above the Dvorak estimates from TAFB and SAB at 0600 UTC to account for the increased organization since that time. This is also in good agreement with the most recent ADT estimates.” The ADT automated storm center determination process is being updated to utilize the newly-available ARCHER 2.0 algorithm. TC center positions will be objectively derived in real time using a weighted combination of LW-infrared, SW-infrared, visible and microwave imagery, as well as scatterometer data. ARCHER 2.0 graphical output for Super Typhoon Soudelor (13W, 2015) Coincident availability of MTSAT and Himawari-8 data in 2015 allowed for a detailed study of the impact of improved spatial and temporal data on the ADT performance. Minor statistical impact was observed overall, with small impacts noted within individual storms. Himawari-8 10 vs. 30 minute data evaluation http://tropic.ssec.wisc.edu/real-time/adt/AHIeval The ADT has been validated storm-by-storm and basin-wide for the global 2015 tropical cyclone seasons. Validation was performed versus Best Track data from the National Hurricane Center and the Joint Typhoon Warning Center in all basins, however the North Atlantic basin requires coincident reconnaissance aircraft data. Validation statistics for all basins (three are shown here) are similar but indicate that more work regarding the ADT intensity estimates for individual basins to alleviate biases might be needed. Development of a scheme to objectively identify and track pre-tropical systems using satellite imagery has produced mixed results, and more study is needed. The algorithm will eventually serve as a ‘front end’ to the ADT to help identify systems becoming a tropical depression. An initial version of the ADT has been developed to operate within the McIDAS-V platform to provide potential ADT users a free, shareware version of the algorithm. This “lite” version would allow users to run the ADT on a variety of satellite data formats for research needs. Find out at Poster 76… right next door!

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Page 1: The Current Status of the UW-CIMSS P75 Advanced Dvorak ...The UW-CIMSS Advanced Dvorak Technique (ADT) is a mature algorithm utilized to objectively estimate the intensity of tropical

The Current Status of the UW-CIMSSAdvanced Dvorak Technique (ADT)

Timothy Olander and Christopher VeldenCooperative Institute for Meteorological Satellite Studies (CIMSS)

University of Wisconsin – Madison

AcknowledgementsADT research and development has been supported by ONR/NRL andNOAA/ NESDIS research programs.

Algorithm Information Current Work Future Upgrades

Another application requested by users isthe ability to employ the ADT on subtropicalsystems. Preliminary work on this extensionhas begun and will focus on determiningwhether a bias adjustment, as with the ETwork, or a new scene type (or modificationof the current Curved Band type) is needed.

Research led by Clark Evans fromUW-Milwaukee to investigate anextension to the ADT for stormsundergoing ET has suggested anintensity adjustment is needed. Twoschemes to integrate this adjustment,utilizing Bob Hart’s cyclone phasespace files to identify when ETbegins, are being evaluated.

P75

The UW-CIMSS Advanced Dvorak Technique(ADT) is a mature algorithm utilized toobjectively estimate the intensity of tropicalcyclones using geostationary infrared data andpolar-orbiting passive microwave data. It isbased upon the manual (and subjective) DvorakTechnique, but has advanced beyond the scopeof the technique. The ADT is currently usedaround the world by many operational TropicalCyclone Forecast Centers.

A study of the most historically intensetropical cyclones from around theglobe during the geo satellite era, asanalyzed by the ADT, was performedto determine a “Top Ten” list. Whatwas the strongest storm? Gilbert?Tip? Patricia? Wilma?

Related Topics at AMS-TC2016WebpageReal-time ADT intensity estimates and product information can be

found on the CIMSS Tropical Cyclone website at :

http://tropic.ssec.wisc.edu/real-time/adt

Extratropical Transition Subtropical Storm Analysis

Himawari-8/MTSAT Comparisons

Hurricane Patricia

ARCHER 2.0 Integration

Latest Statistics

Background

Pre-Genesis Identification and Tracking

McIDAS-V Integration

Himawari-8 vs. MTSAT

25WGenerally small differences; slight tendency

for higher estimates using Himawari-8

10-min. vs. 30-min. Him-8(still in evaluation)

28WGenerally small differences but 10-min can yield a bit quicker response in emerging eye situations

AIRCRAFT RECON

Atlantic - 47 total matchesbias aae stdv

CI# 0.00 0.46 0.60Wind(kts)-0.83 9.15 12.07MSLP(mb) -0.89 8.06 10.62

E/C Pacific - 711 total matchesbias aae stdv

CI# 0.15 0.45 0.58Wind(kts) 2.52 8.71 11.77MSLP(mb) -1.98 7.61 10.49

W Pacific - 608 total matchesbias aae stdv

CI# -0.15 0.42 0.50Wind(kts)-3.55 9.21 11.09MSLP(mb) 3.26 7.55 10.99

Hurricane Patricia provided aunique and challenging test for theADT due to its rapid intensificationand extreme maximum intensity.When compared to aircraftreconnaissance, the real-time ADTprovided remarkably accurateintensity estimates.

HURRICANE PATRICIA DISCUSSION NUMBER 8NWS NATIONAL HURRICANE CENTER MIAMI FL EP202015400 AM CDT THU OCT 22 2015

“Patricia has become significantly better organized overnight, with an eye evident on infrared imagery, and the system now has well-defined convective banding features. The initial intensity estimate is set at 75 kt, which is above the Dvorak estimates from TAFB and SAB at 0600 UTC to account for the increased organization since that time. This is also in good agreement with the most recent ADT estimates.”

The ADT automated storm centerdetermination process is being updatedto utilize the newly-available ARCHER2.0 algorithm. TC center positions will beobjectively derived in real time using aweighted combination of LW-infrared,SW-infrared, visible and microwaveimagery, as well as scatterometer data.

ARCHER 2.0 graphical output for Super Typhoon Soudelor (13W, 2015)

Coincident availability of MTSATand Himawari-8 data in 2015 allowedfor a detailed study of the impact ofimproved spatial and temporal dataon the ADT performance. Minorstatistical impact was observedoverall, with small impacts notedwithin individual storms.Himawari-8 10 vs. 30 minute data evaluation

http://tropic.ssec.wisc.edu/real-time/adt/AHIeval

The ADT has been validated storm-by-storm and basin-wide for the global2015 tropical cyclone seasons. Validation was performed versus Best Trackdata from the National Hurricane Center and the Joint Typhoon WarningCenter in all basins, however the North Atlantic basin requires coincidentreconnaissance aircraft data. Validation statistics for all basins (three areshown here) are similar but indicate that more work regarding the ADTintensity estimates for individual basins to alleviate biases might be needed.

Development of a scheme to objectively identifyand track pre-tropical systems using satelliteimagery has produced mixed results, and morestudy is needed. The algorithm will eventuallyserve as a ‘front end’ to the ADT to help identifysystems becoming a tropical depression.

An initial version of the ADT has beendeveloped to operate within theMcIDAS-V platform to provide potentialADT users a free, shareware version ofthe algorithm. This “lite” version wouldallow users to run the ADT on a varietyof satellite data formats for researchneeds.

Find out at Poster 76… right next door!