REAL TIME WIND AND INSTABILITY

850MB STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)

SURFACE WINDSPEED AND DIRECTION (1 BARB=10kt)
850MB WIND ANALYSIS (UPDATED EVERY 06HRS)
PHILIPPINE HOURLY WIND ANALYSIS		SOUTHEAST ASIA WIND ANALYSIS
10 M WIND ANALYSIS		10 M WIND ANALYSIS SE ASIA
REAL TIME LOW LEVEL CONVERGENCE To identify potential areas where TC development may occur, maturation and sustainment of a TC. Strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments		REAL TIME UPPER LEVEL DIVERGENCE To identify potential areas where TC development may occur, maturation and sustainment of a TC. Strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments

HORIZONTAL DIVERGENCE TC Formation Threshold below 0.525 (The 850 hPa horizontal divergence determined from the average zonal and meridional winds along the boundaries of each 5° by 5° sub-region)

VERTICAL INSTABILITY (°C)TC Formation Threshold above 1.64°C (The vertical average temperature difference between the equivalent potential temperature of a parcel lifted from the surface to 200 hPa, and the saturation equivalent potential temperature of the environment, for each 5° by 5° sub-region)