Último parte del JTWC
THE AREA OF CONVECTION PREVIOUSLY LOCATED NEAR 9.6SS
75.6E, IS NOW LOCATED NEAR 11.2S 77.1E, APPROXIMATELY 355 NM
SOUTHEAST OF DIEGO GARCIA.
RECENT ANIMATED MULTISPECTRAL IMAGERY
SHOWS A WEAK LOW LEVEL CIRCULATION CENTER (LLCC) EMBEDDED WITHIN THE
MONSOON TROUGH. A 02/1301Z
QUIKSCAT PASS SHOWS WINDS OF 15 TO 20 KTS
NEAR THE CENTER. THE CONVECTION ASSOCIATED WITH THE SYSTEM
HAS BEEN
FLARING, SHIFTING ALONG THE MONSOON TROUGH AND IS NOT CURRENTLY
CONSOLIDATING. THE
SEA SURFACE TEMPERATURES FOR THE REGION ARE
FAVORABLE FOR DEVELOPMENT. ANALYSIS OF THE UPPER LEVEL ENVIRONMENT
INDICATES WEAK VERTICAL WIND SHEAR AND GOOD OUTFLOW. MAXIMUM
SUSTAINED SURFACE WINDS ARE ESTIMATED AT 15 TO 20 KNOTS. MINIMUM SEA
LEVEL PRESSURE IS ESTIMATED TO BE NEAR 1006 MB. BASED ON THE WEAK
AND DISORGANIZED LLCC,
THE POTENTIAL FOR THE DEVELOPMENT OF A
SIGNIFICANT TROPICAL CYCLONE WITHIN THE NEXT 24 HOURS REMAINS POORViene a decir: la circulación del sistema es débil, ya que se encuentra embedida por la ITCZ. Los vientos mostrados por Quikscat rondan los 15-20kt cerca del centro. El hecho de encontrarse embedida por la linea monzónica que es el ITCZ, hacen que la convección no se pueda consolidar. La SST es favorable para desarrollo, y el ambiente en alturafavorable, con buen flujo de salida y baja cizalladura. De momento, mantiene el rango de desarrollo bajo (BAJO-POOR; MEDIO-FAIR; ALTO-GOOD. Despues vendría la declaración de Depresión o Tormenta Tropical)
Pues eso, de momento, poca cosa, aunque ya presenta buena organización, como se ve en la animación del post anterior