EARLY GUIDANCE FOR TROPICAL WEATHER SYSTEMS - UNDERSTANDING WHAT'S OUT THERE JENNIFER MCNATT - PREPARING TEXAS
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Early Guidance for Tropical Weather Systems Understanding What’s Out There Jennifer McNatt National Weather Service Material from: Dan Brown, Mike Brennan and John Cangialosi, National Hurricane Center
Which of the following is not true for “Invests” a. Allows NHC to collect additional data and run model guidance b. Implies that the system is likely to develop c. Model guidance is not always run for invests d. The initial location can be moved tens of miles from cycle to cycle
What is an “Invest” A weather system for which a tropical cyclone forecast center (NHC, CPHC, or JTWC) is interested in collecting specialized data sets and/or running model guidance. (In other words, something we want to investigate further.)
Caveats for Invests • Opening an “invest” allows NHC to monitor disturbances more carefully: • Collection of microwave data • Ability to run model guidance • No standard for opening an invest • Guidance is typically run when a cloud system center is apparent • More meteorological uncertainty associated with invests! • Extreme caution should be used when looking at model plots for invests
Tropical Cyclone Tropical WeatherTrack Outlook Overview • Track forecasting is a relatively simple problem – “Cork in a stream” analogy • Important atmospheric features that control track are relatively large and easy to measure 7
Tropical Cyclone Tropical WeatherModels Outlook Statistical and Dynamical • Statistical – Tells you what normally occurs based on the behavior of previous storms in similar situations (i.e., storm location, time of year, current motion, intensity, environment) • Dynamical – Attempt to predict what will happen in this specific situation 8
Tropical Cyclone Tropical WeatherModels Outlook Spaghetti Plots • What does this set of lines represent? • Do they accurately convey the uncertainty in the track forecast? • Are they all created equal? • What’s missing? 9
Tropical Cyclone Tropical WeatherModels Outlook Extrapolated Motion Useful if models aren’t handling initial motion well in the very short term No utility beyond 6 or 12 hours at most 12
Tropical Cyclone Tropical WeatherModels Outlook Climatology and Persistence Used as a baseline to compare other forecasts with Not used as a forecast tool 13
Tropical Cyclone Tropical WeatherModels Outlook Global Models • Best forecast models for TC track • Developed for general weather forecasting • Handle large-scale pattern and steering flow well • Can’t see details of TC inner core • Sometimes struggle with storm structure and intensity, which can affect track forecasts 14
Tropical Cyclone Tropical WeatherModels Outlook Regional Hurricane Models • Developed specifically for TCs • Higher resolution means they can potentially do better job of handling interactions between TC and environment • Limited coverage means features far away from TC may not be handled as well, which can degrade longer- range forecasts 15
Tropical Cyclone Models Consensus Models Typically the best track guidance, especially if the member models all show a similar forecast scenario Doesn’t work well when members forecast very different track scenarios 16
Tropical Cyclone Models Model Plots Spaghetti Plots – Caution! • People looking at publically available model track plots, aren’t seeing the whole picture • Some of the best guidance (ECMWF, FSSE) isn’t publicly available for proprietary reasons • No sense of continuity from cycle to cycle for the various models, trends, etc. • Users/viewers don’t have the forecaster’s perspective and knowledge to know model strengths and weaknesses, trends, etc. 17
Consensus Models Consensus Example Examples – Tropical Storm Cristobal (2014) •Model errors are often random (e.g., small variations on a common theme) 18 •Consensus frequently cancels out these random errors, resulting in a better forecast
Consensus Models Consensus Example Examples – Tropical Storm Cristobal (2014) •Model errors are often random (e.g., small variations on a common theme) 19 •Consensus frequently cancels out these random errors, resulting in a better forecast
Consensus Models Consensus Example Examples – Hurricane Joaquin (2015) HWFI GFDI GFSITVCA ERGI EMXI •Consensus approach doesn’t always work, especially when model scenarios are completely different •Sometimes the forecaster might want to exclude certain models and form a “selective consensus”, if the discrepancies among the models can be resolved 20 •Resolving these discrepancies is very difficult
Track Yearly Model Track ModelVerification Performance Trends Atlantic – 2017 (Preliminary) OFCL very skillful and was near best-performing consensus models (HCCA, TCVA, FSSE) EMXI was best individual model at all lead times, but trailed OFCL and consensus EGRI and UEMI were next best models GFSI, HWFI, AEMI, and CMCI were fair performers NVGI, HMNI, and CTCI lagged 29 April 2018 2018 National Hurricane Conference 22
Track Yearly Model Track ModelTrends Performance Trends Best 48-h Track Model by Storm – 2017 Considerable variability from storm to storm, with no clear best model at 48-h across the board EGRI: Gert, Harvey EXMI: Irma, Ophelia GFSI: Jose, Maria HWFI: Nate 29 April 2018 2018 National Hurricane Conference 23
Track Yearly Model Track ModelTrends Performance Trends Best 48-h Track Model 1996-2017 Due to model changes and other factors, the best performing model often varies from season to season ECMWF (EMXI) was best model in 2017, just edging UKMET and HWRF A global model has been the best at 48 h every year since 2006 except 2013 29 April 2018 2018 National Hurricane Conference 24
Track Yearly Model Track ModelTrends Performance Trends Best 5-day Track Model 2001-2017 Due to model changes and other factors, the best performing model often varies from season to season EMXI was best model at 5 days in 2017 and has been since 2015 years running HWFI was tied with EGRI for second place in 2017 A global model has been the best at 5 days every year since 2001 except one 25
Tropical Cyclone TC Track Models Models – The NAM The NAM TC track errors from the NAM are about 50% higher than the GFS The NAM should not be used for TC forecasting 29 April 2018 2018 National Hurricane Conference 26
TC TrackForecast Forecasting Continuity Forecast Challenges • Large track forecast errors often result from the following scenarios 1. Low predictability in the large-scale steering pattern 2. Misrepresentation of TC structure in models, resulting in improper steering flow 3. Weak steering currents, resulting in track being driven by mesoscale or convective scale factors 27
Tropical Weather Outlook Two-Day Graphic Current location of disturbances (discussed in the Tropical Weather Outlook) Formation chance during the next 48 hrs • Categorical (Low, Medium, and High) • Probabilities
Tropical Weather Outlook Five-Day Graphic • Formation potential during the next 5 days • Initial location of disturbance (X) indicated • Shading represents potential formation area • Single disturbance-based graphics available to help when areas overlap
Potential Formation Area Not a 5-day Track Forecast Tropical Outlook 31 @ 8am July 28 70% 2 Day – 30% 5 Day – 70%
Special Tropical Weather Outlook • Issued anytime there are significant changes with respect to disturbances in the TWO. • Can be updated for either the 2- or 5-day probabilities • Most commonly updated when formation probabilities are too low • Often used to report findings of a recon invest mission
Verification of TWO Probabilities 48 hour Forecasts very reliable. For example, when NHC has issued a 30% chance of formation of a disturbance within 48 hours, about 32% of the time they have become a TC within that time period. Low bias High bias
Verification of TWO Probabilities 5-day probabilities Forecasts generally well- calibrated. Low bias for probabilities from 50-70 % Low bias High bias
Potential Tropical Cyclone Advisories How Did We Make Due Without This Capability • Allows timely issuance of watches and warnings before a tropical cyclone has formed
Summary of 2017 Pre-TC Watches/Warnings Additional Lead Time* Storm (hours) Bret 24 Cindy 21 Franklin 6 Harvey 6 Ten False Alarm Lidia (EPAC) 27 Maria 6 Philippe 21 Average 15.9 hours *Based on Operational Assessments
Watches and Warnings Before Tropical Cyclone Formation • Issued only for systems threatening land within the watch/warning time frame. • Initial advisory issuance is not directly tied to tropical cyclone formation chance. • Initial issuance criteria include: • Likely impacts • Need for tropical cyclone watches or warnings • Desire to avoid switching warning types (tropical vs. non-tropical)
Reminders of Messaging Considerations for Potential Tropical Cyclones • Advisory packages will be discontinued when watches POTENTIAL TROPICAL CYCLONE ONE PUBLIC ADVISORY NUMBER 1 NWS NATIONAL HURRICANE CENTER MIAMI FL AL012016 and warnings are no longer 400 PM CDT WED JUN 5 2016 ...TROPICAL DISTURBANCE OVER THE EAST-CENTRAL GULF OF necessary. MEXICO EXPECTED TO BECOME A TROPICAL STORM... ...TROPICAL STORM WARNING ISSUED FOR PORTIONS OF THE WEST COAST OF FLORIDA... • When the threat is not SUMMARY OF 400 PM CDT...2100 UTC...INFORMATION ----------------------------------------------- LOCATION...25.3N 86.5W imminent this could result ABOUT 310 MI...500 KM SW OF TAMPA ABOUT 320 MI...510 KM SSW OF APALACHICOLA FLORIDA in occasional gaps in MAXIMUM SUSTAINED WINDS...35 MPH...55 KM/H PRESENT MOVEMENT...N OR 360 DEGREES AT 3 MPH...6 KM/H MINIMUM CENTRAL PRESSURE...1010 MB...29.92 INCHES product issuance. WATCHES AND WARNINGS -------------------- CHANGES WITH THIS ADVISORY... A Tropical Storm Warning has been issued for the west coast of Florida from Boca Grande to Ochlockonee River. SUMMARY OF WATCHES AND WARNINGS IN EFFECT... A Tropical Storm Warning is in effect for... * The west coast of Florida from Boca Grande to Ochlocknee River A Tropical Storm Warning means that tropical storm conditions are expected somewhere within the warning
Potential Tropical Cyclone Messaging Considerations • Earlier NHC advisories for systems that pose a long-range threat to the United States or other land areas. • Forecasts likely to have greater uncertainty. • Intensity forecasts are likely to be conservative. • False alarms could: • Reduce long-term effectiveness of watches and warnings • Affect reputation & trust of NHC tropical cyclone forecasts
Pre-Harvey Timeline (Texas) • NHC began mentioning potential hazards for Texas in 1 PM CDT Tuesday Tropical Weather Outlook, a little more than 24 hour before redevelopment occurred • Storm surge • TS or hurricane-force winds • Heavy rainfall • Mentioned likelihood of a TS or hurricane watch at 1 AM CDT Wednesday • Hurricane and Storm Surge Watch issued at 10 AM CDT Wednesday when Harvey regenerated as a Tropical Depression • If confidence in development and potential impacts to land are high, should NHC have the option to issue Potential Tropical Cyclone advisories before the watch phase? • Would the potential for additional false alarms outweigh the need for watch, warning, and forecast information before formation?
Potential Tropical Cyclone Invest in New Terminology? • Feedback suggests that Potential Tropical Cyclone wording is not well understood by the public • Media indicated that it was difficult to communicate • Suggested wording has included: • Potential Tropical Storm • Potential Hurricane • Potential Tropical Threat • Tropical Disturbance • Others? • Does the name Potential Tropical Cyclone cause public confusion? • Is there a better naming convention?
Key Takeaways • Invests say nothing about a systems development potential. Users should refer to the Tropical Weather Outlook! • Genesis probabilities are reliable – Low does not mean no! • Hatched areas on the 5-day Graphical TWO represent the potential formation area – not a true track forecast. • NWS/NHC now able to provide appropriate lead time for watches and warnings for potential tropical cyclones!!
TCConcluding Track Models Remarks – Track Models Summary • Global models are the most skillful for TC track prediction • Consensus aids are more skillful than most individual models, and often beat the official track forecast – NHC forecasters have philosophical constraints on the official forecast that leads to a certain amount of response lag – May contribute to forecast biases and slightly poorer performance than the consensus • While it is possible to beat the models from time to time, model performance has improved significantly over the years, and they are very difficult to beat consistently 47
TCConcluding Track Models Remarks – Track Models Summary • Large track forecast errors often occur due to – Uncertainty in large-scale atmospheric flow – Uncertainty in TC intensity and structure • Track guidance for invests should be treated with extreme caution 48
NHC Forecast Philosophy Forecast Continuity Forecast Continuity • Previous official forecast exerts a strong constraint on the current forecast • Credibility can be damaged by making big changes from one forecast to the next, and then having to go back (flip- flop, windshield-wiper) – Changes to the previous forecast are normally made in small increments – We strive for continuity within a given forecast (e.g., gradual changes in direction or speed from 12 to 24 to 36 h, etc.) • As a result, NHC official forecasts are often slower to reflect big changes than the model guidance 49
Rapid Changes Forecast Continuity Messaging Large Forecast Shifts • Large shifts in the NHC track forecast are sometimes necessary, typically due to large shifts in the guidance • This can be difficult to message, since the shift may occur over 2 or 3 forecast cycles • Look for key messages in the TCD, and can be discussed by your local TS Debby (2012) Cone Graphics office or NHC Advisories 4 through 9 50
Rapid Changes Forecast Continuity Messaging Large Forecast Shifts THE TRACK FORECAST IS EVEN MORE COMPLEX. THE GFS INSISTS ON A TRACK TOWARD THE NORTHEAST AS DEBBY BECOMES EMBEDDED WITHIN A LARGE MID-LATITUDE TROUGH. HOWEVER...THE ECMWF AND THE HWRF BUILD A RIDGE TO THE NORTH OF DEBBY AND FORECAST A WESTWARD TRACK. GIVEN THE WESTWARD TURN INHERITED FROM THE PREVIOUS FORECAST...AS WELL AS THE HISTORICAL STRONG RECORD OF THE ECMWF...THE NEW OFFICIAL FORECAST MOVES DEBBY INITIALLY A LITTLE BIT TO THE NORTHEAST TO REFLECT CURRENT TRENDS BUT THEN TURNS THE CYCLONE BACK TOWARD THE WEST OR WEST-NORTHWEST IN 24 TO 36 HOURS. A MAJORITY OF THE GFS ENSEMBLE MEMBERS NOW ARE CONSISTENT WITH THE DETERMINISTIC RUN...WHICH WAS NOT THE CASE YESTERDAY...MAKING A STRONGER CASE FOR THE EASTWARD SOLUTION. WE MUST BE READY TO MAKE A CHANGE OF THE FORECAST TRACK AT ANY TIME. TS Debby (2012) Advisory 5 Discussion TS Debby (2012) Advisory 5 Cone Graphic 51
Rapid Changes Forecast Continuity Messaging Large Forecast Shifts THERE HAS BEEN A SIGNIFICANT CHANGE IN THE FORECAST TRACK WITH THIS ADVISORY. THE OFFICIAL FORECAST NO LONGER BRINGS DEBBY WESTWARD ALONG THE NORTHERN GULF OF MEXICO AND INSTEAD KEEPS THE CYCLONE MEANDERING OVER THE NORTHEASTERN GULF FOR THE NEXT 3 TO 4 DAYS. THIS FORECAST IS A COMPROMISE BETWEEN THE CONSISTENT EASTWARD SOLUTION PROVIDED BY THE GFS FOR THE PAST SEVERAL DAYS AND THE NEW TWIST OF THE ECMWF. THE ECMWF MODEL...WHICH HAS BEEN FORECASTING DEBBY TO MOVE WESTWARD ALONG THE GULF OF MEXICO... NOW HAS THE CYCLONE MEANDERING FOR THE NEXT 3 DAYS OVER THE NORTHEASTERN GULF. SINCE THESE TWO RELIABLE MODELS ARE IN MARGINALLY BETTER AGREEMENT...I AM A LITTLE MORE CONFIDENT...BUT NOT COMPLETELY...THAT DEBBY IS NOT GOING TO TURN WESTWARD OVER THE GULF. HOWEVER...NEW OFFICIAL TRACK REMAINS A LOW- CONFIDENCE FORECAST. TS Debby (2012) Advisory 6 Discussion TS Debby (2012) Advisory 6 Cone Graphic 52
Rapid Changes Forecast Continuity Messaging Large Forecast Shifts BEST GUESS AT INITIAL MOTION IS QUASI- STATIONARY. DEBBY REMAINS IN A COL REGION OF THE MID-TROPOSPHERIC STEERING FLOW BETWEEN TWO ANTICYCLONES...AND IS LIKELY TO REMAIN SO FOR THE NEXT COUPLE OF DAYS. THEREFORE LITTLE MOTION IS ANTICIPATED DURING AT LEAST THE FIRST HALF OF THE FORECAST PERIOD. IN THE LONGER-TERM...THE TRACK GUIDANCE CONTINUES TO BE ALL OVER THE PLACE...WITH SOME MODELS TAKING DEBBY WEST AND NORTH OF ITS CURRENT POSITION AND OTHERS MOVING EAST OR NORTHEAST AND ULTIMATELY INTO THE ATLANTIC. THE LATTER SCENARIO ASSUMES THAT DEBBY WILL EVENTUALLY BE INFLUENCED BY A MID-TROPOSPHERIC TROUGH OVER THE NORTHEASTERN UNITED STATES. THIS SCENARIO SEEMS MORE LIKELY SINCE IT IS SUPPORTED BY BOTH THE GFS AND THE ECMWF MODELS. REGARDLESS OF WHICH SCENARIO PLAYS OUT...THE CYCLONE DOES NOT SEEM TO BE GOING ANYWHERE ANYTIME SOON. TS Debby (2012) Advisory 8 Discussion TS Debby (2012) Advisory 8 Cone Graphic 53
Rapid Changes Forecast Continuity Messaging Large Forecast Shifts GLOBAL MODELS DEPICT AN AMPLIFYING TROUGH OFFSHORE THE EASTERN SEABOARD CAUSING DEBBY TO MOVE GENERALLY EASTWARD THROUGH THE FORECAST PERIOD...WITH THE CENTER EMERGING OVER THE SOUTHWEST ATLANTIC BY DAY 5. THE ECMWF/GFS SOLUTIONS BEGIN TO LIFT OUT THE WESTERN ATLANTIC TROUGH IN ABOUT 72 HOURS...WHICH COULD LEAVE DEBBY IN WEAK STEERING CURRENT AGAIN AFTER THAT TIME. SINCE YESTERDAY... THE GUIDANCE HAS COME INTO BETTER AGREEMENT...WITH ONLY THE UKMET NOW SHOWING A WESTWARD MOTION. IN ADDITION...THE LATEST GFS ENSEMBLE MEMBERS FAVOR AN EASTWARD MOTION BY ABOUT A 3 TO 1 RATIO. THE NEW FORECAST TRACK REPRESENTS A SUBSTANTIAL CHANGE FROM THE PREVIOUS ONE BUT IS STILL SLOWER THAN THE MULTI-MODEL CONSENSUS IN THE SHORT TERM. TS Debby (2012) Advisory 9 Discussion TS Debby (2012) Advisory 9 Cone Graphic 54
Are the NHC track forecasts improving?
Atlantic Track Error Trends 1960-69 1970-79 1960-69 1980-89 1970-79 1980-89 2000-09 1990-99 2000-09 1990-99 2010-16 1954-59 2010-17 2017 preliminary
3 day average track errors 1990
3 day average track errors 1990 2017
Track Errors over the past 5 years In general, track errors increase about 30-40 n mi per day. 210 181 158 138 113 98 77 67 45 37
Average track errors
Average track errors
Average track errors
Average track errors
Average track errors
Average track errors Outside RMW, significant storm surge
Average track errors Direct hit, highest surge and strongest winds
Average track errors
Averages are nice to know, but each case is different
2017 Storms 5-year average
48-h Model Track Errors by Storm Considerable storm-to-storm variability
Track Errors by Intensity As the initial intensity of the storm increases, NHC track errors on average get smaller.
NHC Forecast Cone • Represents probable track of tropical cyclone center • Formed by connecting circles centered on each forecast point (at 12, 24, 36 h, etc.) • Size of the circles determined so that, for example, the actual storm position at 48 h will be within the 48-h circle 67% of the time
2018 Atlantic Cone Forecast period (h) Circle radii Change from 2010 (n mi) 12 26 28% smaller 24 43 31% smaller 36 56 34% smaller 48 74 31% smaller 72 103 36% smaller 96 151 31% smaller 120 198 31% smaller
NHC Track Cone Questions Does the cone tell you about impacts? No Does the cone know if the system is big or small? No Does the cone know if the forecast is confident or highly uncertain? Nope
Will the NHC track forecasts continue to improve? Skill has been levelling off for the past few years.
Tropical Cyclone Tropical Intensity Cyclone Intensity Overview • Much more complex forecast problem than track – Involves interactions between thunderstorms in the core, the environment, and atmosphere-ocean interactions • Important factors – Track – Wind, temperature, and moisture patterns in the core and the near environment – Internal processes, such as eyewall replacement cycles, that are poorly understood 76
Tropical Cyclone Tropical Intensity Cyclone Intensity Overview • Statistical models tell us normal behavior in a given situation – Extremely difficult to forecast unusual or extreme changes in intensity – Consequently, confidence is usually not high enough to show rapid changes in intensity in the official forecast • Dynamical intensity models have typically lagged the statistical models, but HWRF and HMON both beat the statistical models in 2017 • Intensity consensus aids typically shows the most skill • Official forecast tries to maintain continuity with previous forecast, if possible 77
Intensity Model Concluding RemarksVerification – Track Models Atlantic – 2017 (Preliminary) OFCL skillful at all times, but trailed consensus models at most time periods FSSE best model from 24 to 72 h HWFI was a strong performer, best individual model HMNI not as good as HWFI, but beat statistical aids DSHP and LGEM were fair performers, but not as good as HWFI, HMNI, and consensus models CTCI showed increased skill with time, strong performer days 3-5 GFSI had some skill, but not competitive; EMXI not skillful 29 April 2018 2018 National Hurricane Conference 78
Tropical Cyclone Tropical Intensity Cyclone Intensity Challenges – Rapid Intensification • Intensity guidance from first forecast when Harvey regenerated in the Gulf of Mexico (12Z 23 August MH 2017) • Actual intensity increased 30 kt in 24 h and 65 kt in 48 h H • No guidance from this cycle showed Harvey reaching hurricane intensity before landfall • Landfall intensity 115 kt (cat 4) 29 April 2018 2018 National Hurricane Conference 79
TCConcluding Intensity Models Remarks – Track Models Summary • Forecasting rapid intensification remains a big challenge, but we are making some progress • Regional dynamical hurricane models are now competitive with statistical approaches • Proper specification of the initial vortex remains a big roadblock to improving dynamical model forecasts – How to best use the data in the models? – What do you use for storms with little in situ data? 29 April 2018 2018 National Hurricane Conference 83
Are the NHC intensity forecasts improving?
Atlantic Intensity Error Trends 1970-79, 80-89, 90-99 2000-09 2010-16 2017 Prelim Only small improvements between 1980-2009, but errors have decreased more sharply this decade.
Intensity Errors over the past 5 years Intensity errors increase for 3 days, then level off. 15 15 13 11 8
So What WILL you see in NWS briefings before guidance is available?
Instead of Spaghetti Plots…
Setting the Stage
We still struggle with words!
Verification Web Page
Questions? Thanks again to Dan Brown, Mike Brennan and John Cangialosi at the National Hurricane Center!!!!
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