TYPHOON AND WEATHER IMAGERY: TROPICAL CYCLONE GLENDA 14S

TROPICAL CYCLONE GLENDA 14S (FOR LATEST POSITION, MOVEMENT AND INTENSITY)

REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)

-30°C: +2.5mm; -50°C: +5mm; -70°C: +15mm; -85°C: +25mm -95°C: +35mm; -110°C: +50mm

REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)

REAL TIME THERMAL IR IMAGERY (UPDATED EVERY 30 MINUTES)

REAL TIME VISIBLE (UPDATED EVERY 30 MINUTES)

REAL TIME WIND AND IR IMAGERY	REAL TIME MICROWAVE ANIMATION
REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE)	WUNDERGROUND REAL TIME IMAGERY

FORECAST TRACK

TROPICAL STORM RISK

CLOSE UP RELATIVE VORTICITY (CLICK TO VIEW LARGER)

CLOSE UP WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)

VISIBLE SATELLITE IMAGERY (WITH SUNSHINE ONLY)

VISIBLE MODIS IMAGERY (250M ZOOOM)

REAL TIME DVORAK TIME SERIES

SATCON WIND CHART

LOW LEVEL CONVERGENCE (CLICK TO VIEW LARGER): To identify potential areas where TC development may occur. Since the development of the TC secondary circulation (low-level inflow, updrafts in the TC eyewall, and upper-level outflow) is essential in the maturation and sustainment of a TC, identification of regions where strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments

UPPER LEVEL DIVERGENCE (CLICK TO VIEW LARGER): To estimate the strength of the TC secondary circulation, including the low-level inflow into the TC core, the convective updraft strength within the TC eyewall, and the resulting outflow/venting at the top of the TC. This dynamic can be important for storm growth and development