
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 4.9S 87.6E,
IS NOW LOCATED NEAR 4.9S 84.4E, APPROXIMATELY 840 NM EAST-NORTHEAST
OF DIEGO GARCIA. RECENT ANIMATED INFRARED SATELLITE IMAGERY SHOWS
DEEPENING CONVECTION OVER AN INCREASINGLY CONCENTRATED LLCC. A
090548Z OSCAT PASS INDICATES 25 TO 30 KNOT WINDS IN THE VICINITY OF
A SYMMETRIC LLCC. A RECENT SHIP REPORT INDICATING 25 KNOT WEST-
NORTHWESTERLY WINDS ALONG THE NORTHEASTERN PERIPHERY OF THE LLCC AND
A SEA LEVEL PRESSURE OF 1006 MB SUPPORTS THE OSCAT OBSERVATION. THIS
DISTURBANCE REMAINS EQUATORWARD OF AN UPPER-LEVEL RIDGE AXIS UNDER
THE INFLUENCE OF STRONG (30-40 KNOTS) VWS. HOWEVER, AS THE SYSTEM
SLOWLY MOVES TO THE SOUTHWEST TOWARD THE UPPER-LEVEL RIDGE AXIS, THE
VWS IS EXPECTED TO DECREASE. MAXIMUM SUSTAINED SURFACE WINDS ARE
ESTIMATED AT 25 TO 30 KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED
TO BE NEAR 1005 MB. IN VIEW IF IMPROVING EMVIRONMENTAL CONDITIONS,
THE POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE
WITHIN THE NEXT 24 HOURS IS UPGRADED TO MEDIUM.