(1) AN AREA OF CONVECTION (INVEST 93W) HAS PERSISTED NEAR
32.2N 136.3E, APPROXIMATELY 248 NM SOUTHWEST OF YOKOSUKA, JAPAN.
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A BROAD
AREA OF CONVECTION WITH MINIMAL TURNING. A 221629Z AMSR2 89GHZ
SATELLITE IMAGE REVEALS POCKETS OF DEEP CONVECTION DISPLACED TO THE
EAST AND SOUTHEAST OF A LOW LEVEL CIRCULATION (LLC) WITH SOME LOW-
LEVEL CONVECTIVE BANDING WRAPPING INTO THE LLC. A 221030Z SCATSAT
IMAGE DEPICTS A BAND OF 30-35KT WINDS DISPLACED TO THE SOUTHEAST OF
THE LLC. THE ENVIRONMENT IS CONDUCIVE FOR FURTHER DEVELOPMENT WITH
POLEWARD UPPER LEVEL OUTFLOW, AND A MARGINAL EQUATORWARD OUTFLOW
CHANNEL THAT IS INHIBITED BY THE OUTFLOW OF TC 09W, AND WARM (30-31
CELSIUS) SEA SURFACE TEMPERATURES OFFSET BY MODERATE (10-15 KT)
VERTICAL WIND SHEAR. NUMERICAL MODELS ARE IN GENERAL AGREEMENT THAT
THE SYSTEM WILL DISSIPATE AS IT TRACKS EAST-NORTHEASTWARD. MAXIMUM
SUSTAINED SURFACE WINDS ARE ESTIMATED AT 10 TO 15 KNOTS. MINIMUM SEA
LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1007 MB. THE POTENTIAL FOR
THE DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24
HOURS IS LOW.
(1) THE AREA OF CONVECTION (INVEST 93W) PREVIOUSLY LOCATED
NEAR 32.3N 137.3E HAS DISSIPATED AND IS NO LONGER SUSPECT FOR THE
DEVELOPMENT OF A SIGNIFICANT TROPICAL CYCLONE IN THE NEXT 24 HOURS.