Super Cyclone Gonu

June 5th, 2007

METEOSAT-7 IR image

Super Cylone 02A (“Gonu”) intensified rapidly in the Arabian Sea on 03-04 June 2007. METEOSAT-7 InfraRed (IR) imagery (above; Java animation) showed very cold brightness temperature values (-80º to -88º C, violet to purple enhancement) in the eyewall region during much of the 2-day period. A distinct eye was apparent on the METEOSAT-7 IR images, as well as on the METEOSAT-7 visible images on 04 June (Java animation).

An overpass of the NOAA-17 satellite occurred at 17:33 UTC on 04 June; the IR image (below) depicted a detailed “banded structure” to the cold brightness temperature field, with a minimum temperature of -89º C (darker purple enhancement). Also note the area of gravity waves south of the eye (within the gray-to-white enhanced area of -75º to -79º C brightness temperatures).

NOAA-17 IR image

The CIMSS Advanced Dvorak Technique is a satellite-based method of estimating tropical cyclone intensity — the ADT plot (below) indicates that Gonu intensified very rapidly from late in the day on 03 June (day 2007154) to early in the day on 04 June (day 2007155), reaching Category 5 intensity (with 140 knot wind speeds). This was the first tropical cyclone of Category 5 strength on record in the Arabian Sea.

Gonu ADT plot

Tropical Storm Barry

June 1st, 2007

AWIPS GOES IR image

Tropical Storm Barry formed in the eastern Gulf of Mexico on 01 June 2007 (the first official day of the Atlantic hurricane season). An AWIPS image of the GOES-12 10.7µm IR channel (above; Java animation) showed that some bursts of convection were developing just north of the center of Barry, with cold IR brightness temperature values of -70º to -80º C (black to white enhancement). The tropical cyclone was embedded in an environment of strong southwesterly wind shear in the middle levels and upper levels of the atmosphere, which was not conducive to further strengthening of Barry.

An AWIPS 4-panel comparison of DMSP SSM/I and POES AMSU imagery (below) revealed that rainfall rates near the center of TS Barry were in the 25-35 mm (1.0-1.4 inch) per hour range (orange to red enhancement, upper panels), while total precipitable water values were increasing to 50-60 mm or 2.0-2.4 inches (violet to purple enhancement, lower panels) in the environment surrounding the storm over the eastern Gulf of Mexico. Note that the times displayed on the AWIPS DMSP and POES images do not necessarily correspond to the actual time of the satellite overpass for the particular region being viewed.

AWIPS DMSP / POES rainfall rate / PW