Hong Kong Observatory - 21 March 2005 Briefing on Windshear and Turbulence Alerting Service S.T....
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Transcript of Hong Kong Observatory - 21 March 2005 Briefing on Windshear and Turbulence Alerting Service S.T....
Hong Kong Observatory - 21 March 2005
Briefing on Windshear and Briefing on Windshear and Turbulence Alerting ServicTurbulence Alerting Servic
ee
S.T. Chan & P.W. Chan21 March 2005
Hong Kong Observatory - 21 March 2005
Agenda
Understanding of WS & TURB in HKUnderstanding of WS & TURB in HK Freq. of occurrence Freq. of occurrence Typical conditions conducive to WS & TURBTypical conditions conducive to WS & TURB CharacteristicsCharacteristics
HKO WS & TURB alerting serviceHKO WS & TURB alerting service Recent improvementsRecent improvements How do we performHow do we perform Operational aspectsOperational aspects
Looking forwardLooking forward Q&AQ&A
Hong Kong Observatory - 21 March 2005
What is windshear and turbulence? Windshear – sustained change in wind directiWindshear – sustained change in wind directi
on/speed for more than a few secondson/speed for more than a few seconds change in headwind/tailwindchange in headwind/tailwind change in liftchange in lift Scale several hundred metres - 4 kmScale several hundred metres - 4 km
Hong Kong Observatory - 21 March 2005
What is windshear and turbulence?
Glide slope of aircraft on APP or DEP Glide slope of aircraft on APP or DEP typically 3 – 6 deg.typically 3 – 6 deg.->Glide path in a plane close to horizontal->Glide path in a plane close to horizontal
Systematic vertical shear (e.g. low-level Systematic vertical shear (e.g. low-level jets) not the only reason for WS jets) not the only reason for WS encounteredencountered
Most often horizontal shear (e.g. interface Most often horizontal shear (e.g. interface between different air masses) mattersbetween different air masses) matters
Hong Kong Observatory - 21 March 2005
What is windshear and turbulence?
Turbulence – rapid irregular motion of airTurbulence – rapid irregular motion of air Rapid bumps or joltsRapid bumps or jolts effect on flight path relatively minimaleffect on flight path relatively minimal aircraft may be tossed about, momentarily aircraft may be tossed about, momentarily
out of control in severe eventsout of control in severe events
Hong Kong Observatory - 21 March 2005
Frequency Distribution by Month
Significant windsSignificant windshear: 1 in every 5hear: 1 in every 500 flights00 flights
Significant TURB: Significant TURB: 1 in every 2,000 fli1 in every 2,000 flightsghts
1st peak
2nd peak
Hong Kong Observatory - 21 March 2005
In Hong Kong…
5 typical weather scenarios5 typical weather scenarios Winds blowing across terrainWinds blowing across terrain
(terrain-induced)(terrain-induced) Sea breezeSea breeze Gust frontsGust fronts MicroburstsMicrobursts Low-level jetsLow-level jets
Decreasing freq. of occurrence
Hong Kong Observatory - 21 March 2005
Winds Blowing Across Terrain Winds Blowing Across Terrain (Terrain-induced)(Terrain-induced)
Windy occasions liWindy occasions like during TC…ke during TC…
In lighter wind conIn lighter wind conditions, low-level tditions, low-level temperature inversiemperature inversion also triggers wion also triggers windshear (spring mndshear (spring months)onths)
Hong Kong Observatory - 21 March 2005
Sea breeze Usually develops under fine weatherUsually develops under fine weather Sea breeze converges with prevailing E’liesSea breeze converges with prevailing E’lies Mostly in the form of headwind gains, but headwind losses also possibleMostly in the form of headwind gains, but headwind losses also possible
Hong Kong Observatory - 21 March 2005
Gust front Leading edge of cool air spreading out from the Leading edge of cool air spreading out from the
downdraft of intense stormsdowndraft of intense storms Headwind gainHeadwind gain
Hong Kong Observatory - 21 March 2005
Microburst Most violent form of downdraft from thunderstormsMost violent form of downdraft from thunderstorms Typical horizontal extent: a few kmTypical horizontal extent: a few km Inc. headwind -> Downdraft -> Inc. tailwindInc. headwind -> Downdraft -> Inc. tailwind
Hong Kong Observatory - 21 March 2005
Low-level jet Narrow band of strong windsNarrow band of strong winds Usually affects aircraft on departure (steeper glide path)Usually affects aircraft on departure (steeper glide path) Relatively infrequent at HKIARelatively infrequent at HKIA
Hong Kong Observatory - 21 March 2005
Characteristics of WS & TURB in HK
Most are terrain-induced Most are terrain-induced Transient and sporadicTransient and sporadic More significant on South RWY due to More significant on South RWY due to
closeness to hills in generalcloseness to hills in general Gain and loss events can co-existGain and loss events can co-exist
Hong Kong Observatory - 21 March 2005
Windshear is Sporadic!!Windshear is Sporadic!! Small-scale disturbances Small-scale disturbances
over RWY 25L (multiple over RWY 25L (multiple events)events)
Cold colours (blue, green) – moving towards LIDAR
Warm colours (yellow, orange, pink) – moving away from LIDAR
Hong Kong Observatory - 21 March 2005
0
5
10
15
20
25
30
-1012Distance from runway end (NM)
0
1000
2000
3000
4000
5000
6000
Hei
ght
of 6
-deg
ree
glid
e p
ath
(ft
) LID
AR
's radial velocity (k
nots)
Runway corridor 25 LD
6-degree glide path
LIDAR-Derived Headwind LIDAR-Derived Headwind ProfileProfile
RWY 25L DepartureRWY 25L DepartureHeadwind profile @ 14:41 UTC
Hong Kong Observatory - 21 March 2005
0
5
10
15
20
25
30
-1012Distance from runway end (NM)
0
1000
2000
3000
4000
5000
6000
Hei
ght
of 6
-deg
ree
glid
e p
ath
(ft
) LID
AR
's radial velocity (k
nots)
Runway corridor 25 LD
6-degree glide path
Headwind profile @ 14:41 UTC
LIDAR-Derived Headwind LIDAR-Derived Headwind ProfileProfile
RWY 25L DepartureRWY 25L Departure
Hong Kong Observatory - 21 March 2005
Windshear is Transient!!Windshear is Transient!!
0
5
10
15
20
25
30
-1012Distance from runway end (NM)
0
1000
2000
3000
4000
5000
6000
Hei
ght
of 6
-deg
ree
glid
e p
ath
(ft
) LID
AR
's radial velocity (k
nots)
Runway corridor 25 LD
6-degree glide path
Headwind profile @ 14:41 UTCHeadwind profile @ 14:43 UTC
Sequence of headwind changes reversed in 2 minutes!Sequence of headwind changes reversed in 2 minutes!
Hong Kong Observatory - 21 March 2005
Gain & Loss Events Co-exist!
Gain followed by Gain followed by loss or vice versaloss or vice versa
Common for Common for terrain-induced terrain-induced casescases
Hong Kong Observatory - 21 March 2005
Terrain-Induced MBATerrain-Induced MBA
Terrain-induced events in rain could be so stroTerrain-induced events in rain could be so strong that (i.e. loss of 30 kt or greater) TDWR captng that (i.e. loss of 30 kt or greater) TDWR captures them as MICROBURST!ures them as MICROBURST!
Don’t expect the typical sequence of events Don’t expect the typical sequence of events (gain preceding downdraft followed by loss)(gain preceding downdraft followed by loss)
Hong Kong Observatory - 21 March 2005
WS & TURB Alerting Service
Hong Kong Observatory - 21 March 2005
Automatic Alerts
Issued by WTWS (Issued by WTWS (WWindshear and indshear and TTurbulence urbulence WWarniarning ng SSystem) covering 3 NM from runway thresholdsystem) covering 3 NM from runway thresholds
Nominal update rate 1 min.Nominal update rate 1 min.
Hong Kong Observatory - 21 March 2005
Automatic WS AlertsAutomatic WS Alerts
Microburst Alert (MBA)Microburst Alert (MBA) Generated by TDWR (Generated by TDWR (TTerminal erminal DDoppler oppler WWeaea
ther ther RRadar) and integrated into WTWS adar) and integrated into WTWS Runway-oriented wind speed loss >= Runway-oriented wind speed loss >=
30 kt30 kt and accompanied by precipitation and accompanied by precipitation Windshear Alert (WSA)Windshear Alert (WSA)
Runway-oriented wind speed loss or gain >= Runway-oriented wind speed loss or gain >= 15 kt15 kt
Hong Kong Observatory - 21 March 2005
Automatic TURB AlertsAutomatic TURB Alerts
Moderate or severe in intensityModerate or severe in intensity With reference to heavy category With reference to heavy category
aircraftaircraft
Hong Kong Observatory - 21 March 2005
Warnings Provided on ATIS
Issued by Aviation Met. ForecastersIssued by Aviation Met. Forecasters Based on pilot reports, forecasting Based on pilot reports, forecasting
rules developed from case studies, rules developed from case studies, real-time conditions as revealed by real-time conditions as revealed by TDWR, LIDAR, etc.TDWR, LIDAR, etc.
Hong Kong Observatory - 21 March 2005
Performance of WS WarningsPerformance of WS Warnings(12-month Running Means)(12-month Running Means)
POD approaching upper limit, FAR keeps decreasingPOD approaching upper limit, FAR keeps decreasing
Hong Kong Observatory - 21 March 2005
Improvements Implemented
Hong Kong Observatory - 21 March 2005
New Member of WTWS New Member of WTWS Algorithms - AWAREAlgorithms - AWARE
• AWARE (Anemometer-based Windshear Alerting Rules – Enhanced) launched in mid-2004
• Replaced old LLWAS module
• Based on wind readings at 6 runway anemometers & TMT & 5 weather buoys
• Alerts out of ground truths
TMT
Weatherbuoys
Runway anemometers
Weatherbuoy
Hong Kong Observatory - 21 March 2005
Merits of AWARE…Merits of AWARE…
• More extensive coverage compared More extensive coverage compared with LLWASwith LLWAS
• Enhanced detection of WS associated Enhanced detection of WS associated with:with:– Sea breezeSea breeze– Gust frontGust front– Shear lineShear line
• More sensitive in depicting gain More sensitive in depicting gain events than WTWS/TDWRevents than WTWS/TDWR
Hong Kong Observatory - 21 March 2005
Shear Line Case Shear Line Case WS Episode in July 2004WS Episode in July 2004
• WS reports over 25RA:
0530 B772 +15kt0535 A343 +15kt0546 A306 -10 to +15 kt0619 A306 +15kt0625 B773 ±10 to 15kt
• All captured by AWARECold colours (blue, green) – moving towards LIDAR
Warm colours (yellow, orange, pink) – moving away from LIDAR
Hong Kong Observatory - 21 March 2005
Successful Detection by AWARE Successful Detection by AWARE (Previously gone undetected with (Previously gone undetected with
WTWS)WTWS)
Hong Kong Observatory - 21 March 2005
AWARE – Point to Note
AWARE alerts updated at 10 sec. AWARE alerts updated at 10 sec. intervalsintervals
There may be brief alerts lasting a There may be brief alerts lasting a few sec. in marginal casesfew sec. in marginal cases
They are genuine alerts!They are genuine alerts!
Hong Kong Observatory - 21 March 2005
LILIght ght DDetection etection AAnd nd RRanginganging((LIDARLIDAR) system – Fully Operational in Mi) system – Fully Operational in Mi
d-2004d-2004
Installed in mid-2002Installed in mid-2002IR (2 IR (2 μμm) → eye-safem) → eye-safe
LIDAR ScannerLIDAR Scanner
ATCX Building Roof-top
Hong Kong Observatory - 21 March 2005
How the LIDAR works …How the LIDAR works …
100
Hong Kong Observatory - 21 March 2005
Merits of LIDAR…Merits of LIDAR…
• Demonstrated capability in WS detection in Demonstrated capability in WS detection in non-rainy conditions non-rainy conditions -> indispensable reference tool for issuance -> indispensable reference tool for issuance of forecaster WS warnings on ATISof forecaster WS warnings on ATIS
• Better definition on location of WS detectedBetter definition on location of WS detected-> runway-specific WS warnings-> runway-specific WS warnings
• Automatic windshear detectionAutomatic windshear detection-> new alerting algorithms developed-> new alerting algorithms developed
Hong Kong Observatory - 21 March 2005
Windshear algorithms for automatiWindshear algorithms for automatic alerting based on LIDAR datac alerting based on LIDAR data
• Adaptation of TDWR approach (shear Adaptation of TDWR approach (shear along radar beams) – the radial shear along radar beams) – the radial shear algorithmalgorithm
• Direct view of glide paths – glide-path scan Direct view of glide paths – glide-path scan windshear algorithmwindshear algorithm
Hong Kong Observatory - 21 March 2005
Radial shear algorithmRadial shear algorithmShear line identified by algorithmShear line identified by algorithmShear line discernible on Shear line discernible on
LIDAR velocity pictureLIDAR velocity picture
Shear lineShear line
Hong Kong Observatory - 21 March 2005
Glide-Path Scan WS AlgorithmGlide-Path Scan WS Algorithm
• ““Tube” cross-section:Tube” cross-section:
2000 feet x 400 feet2000 feet x 400 feet• Only points within the Only points within the
“tube” will be “tube” will be consideredconsidered
• Points closest to the Points closest to the flight path will be used flight path will be used to create the headwind to create the headwind profileprofile
Hong Kong Observatory - 21 March 2005
Glide-Path Scan WS Algorithm Glide-Path Scan WS Algorithm
• SuccessfuSuccessful l detection detection of a sig. of a sig. gain gain eventevent
Hong Kong Observatory - 21 March 2005
Trial Operation of LIDAR-based Trial Operation of LIDAR-based Alerting AlgorithmsAlerting Algorithms
Hong Kong Observatory - 21 March 2005
Runway-specific WS Runway-specific WS WarningsWarnings(on ATIS)(on ATIS)
• LIDAR/TDWR/wind sensors, etc., LIDAR/TDWR/wind sensors, etc., reveal weather systems conducive to reveal weather systems conducive to WSWS
• Weather systems moving and Weather systems moving and evolving slowly?evolving slowly?
• WS affects only certain runway WS affects only certain runway corridors -> runway-specific warning corridors -> runway-specific warning issued issued (e.g. warning for APP corridors only)(e.g. warning for APP corridors only)-> more specific and accurate -> more specific and accurate warningswarnings
Hong Kong Observatory - 21 March 2005
Example - Spring Easterly Example - Spring Easterly FlowFlow
(Terrain-induced)(Terrain-induced)Gap flows only Gap flows only affect southern affect southern corridorscorridors
→ → ATIS ATIS windshear windshear warning issued warning issued for southern for southern corridors onlycorridors onlyCold colours (blue, green) – moving towards LIDAR
Warm colours (yellow, orange, pink) – moving away from LIDAR
Hong Kong Observatory - 21 March 2005
Example - Sea BreezeExample - Sea Breeze
Sea breeze front over Sea breeze front over western corridorswestern corridors→ → ATIS windshear warATIS windshear warning will be issued for ning will be issued for all western corridorsall western corridors
Sea breeze front
Background flow
Sea Breeze
Hong Kong Observatory - 21 March 2005
Example - Autumn/Winter Example - Autumn/Winter Northerly FlowNortherly Flow
Gap flows extend Gap flows extend to affect eastern to affect eastern approach approach corridor of north corridor of north runway onlyrunway only
→ → ATIS windshear ATIS windshear alert will be alert will be issued for that issued for that corridorcorridor
Gap Flow
Hong Kong Observatory - 21 March 2005
Some Operational Aspects
Hong Kong Observatory - 21 March 2005
Revision to WS/TURB Info on Revision to WS/TURB Info on ATISATIS
(Ref.: AIC 03/05)(Ref.: AIC 03/05)• Wef 27 January 2005Wef 27 January 2005• New terminology: New terminology: ““FORECASTFORECAST”” (“EXPECT” (“EXPECT”
previously) for forecast warnings by HKO. previously) for forecast warnings by HKO. ““FFORECAST AND REPORTEDORECAST AND REPORTED”” for warnings confi for warnings confirmed by pilot reports.rmed by pilot reports.
• Estimated 2 500 ft wind based on hilltop wind Estimated 2 500 ft wind based on hilltop wind on Lantau be given (Arrival ATIS) when wind son Lantau be given (Arrival ATIS) when wind speed reaches 35 kt:peed reaches 35 kt:“2500 ft estimated wind 160 degree 40 kt”“2500 ft estimated wind 160 degree 40 kt”
Hong Kong Observatory - 21 March 2005
New Format of WS/TURB Info New Format of WS/TURB Info in Local Routine Report / MET in Local Routine Report / MET
PagePage• Revised WS/TURB Revised WS/TURB
warning terminology warning terminology under “ADDN INFO” under “ADDN INFO” following new ICAO following new ICAO templatetemplate
• New “ATIS WS/TURB New “ATIS WS/TURB WRNG” contains WRNG” contains consolidated warnings consolidated warnings for inclusion in ATIS for inclusion in ATIS
• ““FCST AND REP” for FCST AND REP” for warnings validated by warnings validated by pilot reportspilot reports
Hong Kong Observatory - 21 March 2005
• Very common to have multiple occurrences of WS on same corridor in HK
• WTWS consolidates multiple events into ONE integrated alert– TDWR alerts higher priority than WTWS
alerts– Sinking shear (loss events) higher
priority than lifting shear (gain events)– Max intensity given in alerts
Alert PhraseologyAlert Phraseology
Hong Kong Observatory - 21 March 2005
• E.g. APP to RWY 25L
• ‘Caution Microburst Minus 30 knots on final approach’ (instead of specific location as in US)
• Note: – The max intensity (-30 kt) can occur anywhere along the c
orridor– First encounter (+15 kt @ 3NM) not the worst encounter (-
30 kt @ 1NM)
Alert PhraseologyAlert Phraseology
-30 +15RWY 25L
Hong Kong Observatory - 21 March 2005
• E.g. APP to RWY 25L
• ‘Caution Windshear Minus 15 knots on final approach’
• Note: – Some may report -15 kt, while others +20 kt (especially th
ose who conducted a missed APP on encounter of the lifting shear)
Alert PhraseologyAlert Phraseology
-15 +20RWY 25L
Hong Kong Observatory - 21 March 2005
Looking Forward
Validation and tuning of LIDAR-based alerting algorithms – integration with WTWS
Backup LIDAR Uplink of WS & TURB
information to cockpit
Hong Kong Observatory - 21 March 2005
Validation and Tuning ofValidation and Tuning ofLIDAR-based Alerting LIDAR-based Alerting
AlgorithmsAlgorithms
• Case study 28-Case study 28-30 Aug 200430 Aug 2004
• Strong Strong southerly flow southerly flow across Lantauacross Lantau
• ~70 WS ~70 WS reports during reports during the episodethe episode
Hong Kong Observatory - 21 March 2005
PerformancePerformanceRunway
Items 25RA 25LD 25LA
Number of aircraft windshear reports 42 25 4
Number of hits 31 24 4
Probability of detection (hit rate) 0.74 0.96 1.00Number of null reports with alerts 7 7 0
False alarm rate 0.23 0.29 0.00Total alert duration (minutes) 730 1757 925
Alert duration per hit (minutes) 24 73 231
Hong Kong Observatory - 21 March 2005
Limitations of the LIDAR in Limitations of the LIDAR in windshear detectionwindshear detection
• Not enough range coverage in Not enough range coverage in humid/rainy situationshumid/rainy situations
• ‘‘Dead zone’ with no LIDAR data Dead zone’ with no LIDAR data (about 400 m from the LIDAR)(about 400 m from the LIDAR)
• Misses of WS events between re-Misses of WS events between re-visits of scans – visits of scans – WS is transientWS is transient
• Delay in relay of alerts (data to Delay in relay of alerts (data to alerts to pilots) – out of phase alerts to pilots) – out of phase alertsalerts
Hong Kong Observatory - 21 March 2005
• Windshear algorithm is verified against pilot Windshear algorithm is verified against pilot reports of windshearreports of windshear
• If in doubt, flight data will be obtained and aIf in doubt, flight data will be obtained and analyzed nalyzed
• More pilot reports (details as intensity and loMore pilot reports (details as intensity and location) are required to help tuning windsheacation) are required to help tuning windshear algorithmsr algorithms
• HKO needs your help! Keep reporting to us HKO needs your help! Keep reporting to us WINDSHEARWINDSHEAR or or NO WINDSHEARNO WINDSHEAR
Tuning of LIDAR-basedTuning of LIDAR-basedWS AlgorithmWS Algorithm
Hong Kong Observatory - 21 March 2005
Current LIDAR locationBackup LIDAR location – Northern Fire Station
Backup LIDARBackup LIDAR
Hong Kong Observatory - 21 March 2005
Backup LIDARBackup LIDAR
• To backup existing LIDARTo backup existing LIDAR• To improve coverage over the north To improve coverage over the north
runwayrunway• Funding approvedFunding approved• Installation scheduled in late 2006Installation scheduled in late 2006
Hong Kong Observatory - 21 March 2005
Uplink of WS & TURB Info to Uplink of WS & TURB Info to CockpitCockpit
• For immediate attention of the pilotsFor immediate attention of the pilots• WS & TURB alerts most-wanted WS & TURB alerts most-wanted
information in cockpit according to a information in cockpit according to a recent survey of pilots’ viewsrecent survey of pilots’ views
• Graphical products to be developed Graphical products to be developed by HKO for future uplink applicationsby HKO for future uplink applications
Hong Kong Observatory - 21 March 2005
International RecognitionInternational Recognition
International Federation of International Federation of Airline Pilots Association Airline Pilots Association
(2002)(2002)
International Civil International Civil Aviation OrganizationAviation Organization
(2003)(2003)
World Meteorological World Meteorological OrganizationOrganization
(2004)(2004)
Hong Kong Observatory - 21 March 2005
Finally…Finally…
We are working on further reduction of false warnings while maintaining high hit rate
Closer coordination with ATC Continue to appeal for assistance from pilo
ts in providing reports to ATC via voice / HKO via pilot report form: http://www.weather.gov.hk/aviat/amt_e/report_form.pdf
Hong Kong Observatory - 21 March 2005
THANK YOU!
S.T. ChanS.T. [email protected]@hko.gov.hkTel: (852) 2926 8434Tel: (852) 2926 8434Fax: (852) 2375 2645Fax: (852) 2375 2645
P.W. ChanP.W. [email protected]@hko.gov.hkTel: (852) 2926 8331Tel: (852) 2926 8331Fax: (852) 2375 2645Fax: (852) 2375 2645