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Japan Meteorological Agency 1
How to issue How to issue SIGMET SIGMET
Shikembaru, Toru志堅原 透
Japan Meteorological Agency (JMA)日本 気象庁
SIGMET Seminar for Asia/Pacific Region
Bangkok, Thailand, 11-13 July 2007
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Contents of lectureContents of lecture
I. Outline of SIGMETII. How to issue SIGMET
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I. Outline of SIGMETI. Outline of SIGMET
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Definition of SIGMET informationDefinition of SIGMET information
Information issued by a meteorological watch office concerning the occurrence or expected occurrence of specified en-route weather phenomena which may affect the safety of aircraft operations.
Excerpt from WMO Technical Regulations [C.3.1.] 1.1
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Importance of SIGMET informationImportance of SIGMET information
SIGMET information is the highest priority among other types ofmeteorological information provided to the aviation users.
SIGMET information is used for flight planning of the airlines globally.
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Principal operation as a Meteorological watch office (MWO) Principal operation as a Meteorological watch office (MWO) for issuing SIGMET informationfor issuing SIGMET information
To prepare SIGMET and other information relating to its area ofresponsibility.
To supply SIGMET information and, as required, other meteorological information to associated air traffic services units.
To disseminate SIGMET information.
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Dissemination of SIGMETDissemination of SIGMET
SIGMET messages shall be disseminated toMWOs,WAFCsother meteorological offices
SIGMET messages for volcanic ash shall be disseminated to VAACs.
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Note to issue SIGMETNote to issue SIGMET
Although SIGMET information is required to be issued for cruising level, there is no stated lower limit regarding the height.
MWOs should not issue SIGMET for weather phenomena of lower intensity, transient nature, or smaller scale, which do not affect significantly the flight safety.
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Type of SIGMET at subsonic cruising levelsType of SIGMET at subsonic cruising levels
OBSC TS EMBD TSFRQ TSSQL TSOBSC TSGREMBD TSGRFRQ TSGRSQL TSGR
TC (+ cyclone name) where the criterion of 10-minute
mean surface wind speed is 63km/h(34kt) or more.
SEV TURB
SEV ICESEV ICE(FZRA)
SEV MTW
HVY DS
HVY SS
VA (+ volcano name, if known)
ThunderstormThunderstorm Tropical cycloneTropical cycloneTurbulenceTurbulence
IcingIcing
Mountain waveMountain wave
DuststormDuststorm
SandstormSandstorm
Volcanic ashVolcanic ash
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Type of SIGMET Type of SIGMET at transonic and supersonic cruising levelsat transonic and supersonic cruising levels
ISOL CB OCNL CBFRQ CB
MOD TURBSEV TURB
VA (+ volcano name, if known)CumulonimbusCumulonimbus TurbulenceTurbulence Volcanic ashVolcanic ash
GR HailHail
Note :
Only one of the weather phenomena should be selected and included in each SIGMET.
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Period of validity of SIGMETPeriod of validity of SIGMET
Up to 6 TC, VAUp to 4TURB, TS, ICE, MTW, DS, SS, CB, GRHoursPhenomena
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Update and cancellation of SIGMETUpdate and cancellation of SIGMET
When the Sig-WX phenomena (which is on SIGMET) is growing, MWO should issue a new updated SIGMET.
When the phenomena is no longer occurring nor expected to occur, MWO should cancel the SIGMET speedily.
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Principal components of SIGMET message of Principal components of SIGMET message of ICAO Amendment 74 to Annex 3ICAO Amendment 74 to Annex 3
Direction of the requirement of SIGMET for transonic and supersonic cruising level.
Elimination of OTLK from SIGMET messages related to VA and TC.
See the ICAO Working Paper “APPROVAL OF DRAFT REPORT TO COUNCIL ONAMENDMENT 74 TO ANNEX 3 - METEOROLOGICAL SERVICEFOR INTERNATIONAL AIR NAVIGATION ”.
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II. How to issue SIGMETII. How to issue SIGMET
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Example of SIGMET for phenomena excluded TC and VAExample of SIGMET for phenomena excluded TC and VA
RJJJ SIGMET 4 VALID 260725/261125 RJTD-RJJJ FUKUOKA FIR SEV TURB OBS AT 0715Z S OF N3450 E13950 FL280/320 MOV NE 20KT INTSF
(This SIGMET is fictitious)
ICAO Location indicator of FIR or CTA
Message indicator Validity period Location indicator of MWO and hyphen
ICAO Location indicator and name of the FIR(/UIR) or CTA
Phenomenon Indication of observed and expected to
continue, or forecast
Expected changes in intensity
Movement or expected movement
Location
Daily sequence number Validity indicator
Vertical extent or level
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Types of satellite imageTypes of satellite image
Visible image Infrared image Water-vapour image
The Visible image or infrared image is useful for judging occurrences or expected occurrences phenomena to SIGMET information. But the water-vapour image is more useful for expected occurrences TURB. (To know occurrences of air turbulences, we need to get pilot reports.) It is because that occurring TURB, especially CAT, is connected with pattern of Jet Streams. If estimated position of Jet Streams can be understood with a water-vapour image, it will be possible to issue SIGMET information for turbulence.
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NWP data over the satellite imageNWP data over the satellite image
Relationship between position of Jet Streams, trough and ridge, value of wind shears and cloud can be understood with NWP data over the satellite image.
The left image is that the NWP data of 300hPa winds and 300hPa parallel of altitude lap over the infrared image.
(at 26 Feb. 2007 00UTC)
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AerologicAerologic observation and NWP data over the satellite observation and NWP data over the satellite imageimage
Additionally, three dimensional meso-scale phenomena can be understood using aerologic observation and NWP data over the satellite image.
The left image is that the aerologic observation wind data at 300hPa, light blue pennants, the NWP data of 300hPa winds and 300hPa parallel of altitude lap over the infrared image.
(at 26 Feb. 2007 00UTC)
T Td
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How to make SIGMET information for TSHow to make SIGMET information for TS
RJJJ FUKUOKA FIR FRQ TS FCST WI N40E148 - N40E158 -N45E156 - N45E150 - N43E148 MOV NE 15KT INTSF
The moving direction and moving velocity will be estimated with the animated satellite images.
This red area is described in SIGMET information.
Area except at a stationary area may be widened in consideration of validity period and moving direction and velocity.
mov
ing d
irect
ion
This blue area is estimated the area of frequent TS on this image.
The following SIGMET main body is determined in this situation. Where the name of the FIR is Fukuoka FIR, the moving direction is northeastward, the moving velocity is 15kt and the phenomenon’s intensity is intensifying.