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NWPTA Sample Message - 5.
Revision of the Advisory.
WEPA40 RJTD 240934

TSUNAMI BULLETIN NUMBER 002
  ISSUED BY NWPTAC(JMA)
  ISSUED AT 0929Z 24 MAR 2005
PART 01 OF 01 PARTS

HYPOCENTRAL PARAMETERS(REVISION)
ORIGIN TIME:0858Z 24 MAR 2005
PRELIMINARY EPICENTER:LAT 3.5SOUTH LON148.2EAST
  EASTERN CAROLINE ISLANDS, MICRONESIA
  PACIFIC BASIN
MAG:8.3

EVARUTION
  THERE IS A POSSIBILITY OF A DESTRUCTIVE OCEAN-WIDE TSUNAMI

THIS BULLETIN IS FOR
  EAST COASTS OF PHILIPPINES(REVISION)
  NORTH COASTS OF IRIAN JAYA(REVISION)
  NORTH COASTS OF PAPUA NEW GUINEA(REVISION)
  CELEBES SEA

ESTIMATED TSUNAMI ARRIVAL TIME AND ESTIMATED TSUNAMI WAVE AMPL
EAST COASTS OF PHILIPPINES
  LOCATION
COODINATES ARRIVAL TIME AMPL
  LEGASPI
13.2N 123.8E (ALREADY ARRIVED)
  DAVAO
06.9N 125.7E 1237Z 24 MAR 1M(ADDITION)
NORTH COASTS OF IRIAN JAYA
  LOCATION
COORDINATES ARRIVAL TIME AMPL
  MANOKWARI
00.8S 134.2E 1116Z 24 MAR 0.5M(REVISION)
  WARSA
00.6S 135.8E 1046Z 24 MAR 1M
  JAYAPURA
02.4S 140.8E 1002Z 24 MAR 3M
NORTH COASTS OF PAPUA NEW GUINEA
  LOCATION
COORDINATES ARRIVAL TIME AMPL
  VANIMO
02.6S 141.3E 0953Z 24 MAR 2M
  WEWAK
03.5S 143.7E 0931Z 24 MAR 4M
  MADANG
05.2S 145.8E 0935Z 24 MAR 8M
  MANUS IS.
02.0S 147.5E 0858Z 24 MAR 4M
  RABAUL
04.2S 152.3E (CANCELLATION)

AMPL - AMPLITUDE IN METERS FROM MIDDLE TO CREST

HOWEVER AT SOME COASTS, PARTICULARLY THOSE NEAR THE EPICENTER, HIGHER
TSUNAMIS MAY ARRIVE THAN OUR ESTIMATION AT THE NEARBY
FORECAST POINTS
AUTHORITIES SHOULD BE AWARE OF THIS POSSIBILITY.

FURTHERMORE THE EVALUATION OF TSUNAMIGENIC POTENTIAL AND ESTIMATED
ARRIVAL TIME OF TSUNAMIS MAY BE DIFFERENT FROM THOSE OF PTWC
DUE TO DIFFERENCES IN THE ESTIMATED EARTHQUAKE PARAMETERS
AUTHORITIES SHOULD USE THE EARLIEST ARRIVAL TIMES FOR
GREATEST SAFETY.

MEASUREMENTS OR REPORTS ON TSUNAMI
  LOCATION
  COORDINATES ARRIVAL TIME AMPL
  LEGASPI
  13.2N 123.8E
  MAXIMAM TSUNAMI WAVE 0810Z 10 JAN 0.5M

MAXIMUN TSUNAMI WAVE -- HALF OF AMPLITUDE FROM THE TROUGH
TO THE CREST

THIS WILL BE THE FINAL BULLETIN UNLESS THERE ARE CHANGES ABOUT
THE POTENTIAL OF TSUNAMI GENERATION BY RE-EVALUATION OF THE
EARTHQUAKE OR THERE ARE REPORTS ON TSUNAMI OBSERVATIONS.

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