And it is now medium!

THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 21.5N 
121.5E, IS NOW LOCATED NEAR 21.8N 122.3E, APPROXIMATELY 185 NM SOUTH-
SOUTHWEST OF ISHIGAKIJIMA, JAPAN. ANIMATED MULTISPECTRAL SATELLITE 
IMAGERY (MSI) DEPICTS A WELL-DEFINED, EXPOSED LOW-LEVEL CIRCULATION 
CENTER (LLCC) WITH ISOLATED BURSTS OF DEEP CONVECTION SHEARED EAST 
AND SOUTHEAST OF THE LLCC. A 092344Z SSMIS IMAGE INDICATES 
FORMATIVE, WEAK BANDING DISPLACED OVER THE SOUTHERN SEMI-CIRCLE OF 
THE SYSTEM. A 100104Z ASCAT IMAGE SHOWS A SYMMETRIC CIRCULATION WITH 
15 TO 20 KNOT WINDS AND STRONGER FLOW OVER THE SOUTHERN FLANK OF THE 
SYSTEM, ASSOCIATED WITH THE AFOREMENTIONED WEAK CONVECTIVE BANDING. 
MSI AND ASCAT IMAGERY INDICATE THAT THE LLCC IS LOCATED WELL SOUTH 
OF A WEAK BAROCLINIC ZONE, WHICH EXTENDS FROM NORTHERN TAIWAN SOUTH-
SOUTHWESTWARD INTO THE SOUTH CHINA SEA. UPPER-LEVEL ANALYSIS SHOWS 
THAT THE LLCC IS LOCATED JUST POLEWARD OF THE SUBTROPICAL RIDGE AXIS 
IN A MARGINAL ENVIRONMENT WITH LOW TO MODERATE (15 TO 20 KNOTS) 
VERTICAL WIND SHEAR ASSOCIATED WITH UPPER-LEVEL WEST-SOUTHWESTERLY 
FLOW. DUE TO THE SMALL SIZE OF THE SYSTEM, THE DYNAMIC MODELS ARE 
NOT INITIALIZING THE CIRCULATION ACCURATELY. HOWEVER, THE MODEL 
FIELDS INDICATE A TWO TO THREE DAY PERIOD OF POTENTIAL DEVELOPMENT 
BEFORE THE SYSTEM BECOMES ABSORBED IN THE BAIYU BOUNDARY SOUTH OF 
KYUSHU. MAXIMUM SUSTAINED SURFACE WINDS ARE ESTIMATED AT 15 TO 20 
KNOTS. MINIMUM SEA LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1001 MB. 
BASED ON THE STRENGTH AND SYMMETRY OF THE LOW-LEVEL WIND FIELD, THE 
POTENTIAL FOR THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE 
WITHIN THE NEXT 24 HOURS IS UPGRADED TO MEDIUM.