THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 19.2N 134.7E,
IS NOW LOCATED NEAR 20.0N 134.0E, APPROXIMATELY 505 NM SOUTHEAST OF NAHA,
OKINAWA. RECENT ANIMATED MULTISPECTRAL IMAGERY DEPICTS AN AREA OF CONVECTION
ASSOCIATED WITH A HIGH-AMPLITUDE, INVERTED SURFACE TROUGH. A 050050Z TRMM
PASS REVEALS A POSSIBLE LOW LEVEL CIRCULATION CENTER AT THE SOUTHERN END
OF THE SURFACE TROUGHING. UPPER LEVEL ANALYSIS SHOWS THE PRESENCE OF AN
ANTICYCLONE OVER THE AREA OF CONVECTION AND LOW VERTICAL WIND SHEAR. MAXIMUM
SUSTAINED SURFACE WINDS ARE ESTIMATED AT 15 TO 20 KNOTS. MINIMUM SEA LEVEL
PRESSURE IS ESTIMATED TO BE NEAR 1006 MB. GIVEN A VERY FAVORABLE UPPER LEVEL
ENVIRONMENT, THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL
CYCLONE WITHIN THE NEXT 24 HOURS IS UPGRADED TO FAIR.
05/1433 UTC 20.8N 131.8E T2.5/2.5 91W -- West Pacific Ocean

If two at the same time were not enough, may three will be.