TROPICAL CYCLONE INGRID 10L

TROPICAL CYCLONE INGRID 10L (FOR LATEST POSITION, MOVEMENT AND INTENSITY)

REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY -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 DVORAK TIME SERIES
WUNDERGROUND REAL TIME IMAGERY	REAL TIME RBTOP IMAGERY (CLICK IMAGERY ANIMATE)

FORECAST TRACK

TROPICAL STORM RISK

VISIBLE SATELLITE IMAGERY (WITH SUNSHINE ONLY)

VISIBLE MODIS IMAGERY (250M ZOOOM)

RELATIVE VORTICITY

WIND SHEAR

SATCON AMSU BRIGHTNESS TEMPERATURE

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

STEERING WIND ANALSIS

SHALLOW LAYER STEERING

MIDDLE LAYER STEERING

DEEP LAYER STEERING

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

RAMMB-CIRA REAL TIME SITENRL REAL TIME INFO SITENRL RAINRATETRACK FILE TROPICAL STORM RISK30MIN JTWC REAL TIME ADVANCE DVORAK TECHNIQUES30MIN RSMC REAL TIME ADVANCE DVORAK TECHNIQUESDISCUSSION/PROGNOSIS-----------------------------NO IMAGERY AVAILABLE YET-----------------------------

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