Archive for August, 2007

Linear Mesoscale Convective System in the Upper Midwest

Tuesday, August 28th, 2007

GOES-12 visible image

GOES-12 visible channel images (above; Java animation) showed a linear mesoscale convective system developing across parts of Iowa, Minnesota, and Wisconsin on 28 August 2007. Note the picturesque shadows cast by the individual cumulonimbus towers building in northeastern Iowa between 21:00 and 22:00 UTC. The larger cluster of thunderstorms in north-central/northeastern Wisconsin produced several reports of hail (up to 1.0 inch in diameter) and wind gusts of 60-80 mph (SPC storm reports). An AWIPS image of the MODIS 11.0µm IR channel around 19:09 UTC depicted cloud top brightness temperatures as cold as -79º C (-110º F) in north-central Wisconsin, with numerous cloud to ground lightning strikes.

AWIPS GOES-12 sounder Derived Product Images (DPI) of Convective Available Potential Energy (CAPE), Lifted Index (LI), and Total Precipitable Water (TPW) at 17:00 UTC (below) indicated that instability and moisture were increasing within a narrow zone along and just ahead of a wavy frontal boundary that was advancing slowly southeastward through the region. Isolated CAPE values were in excess of 4000 J/kg, LI values were less than -8º C, and TPW values were greater than 50 mm (2.0 inches) in the general area where new convection was seen to develop rapidly in north-central Iowa about 4 hours later on the GOES-12 visible images above.

GOES-12 sounder CAPE

GOES-12 sounder LI

GOES-12 sounder PW

Hurricane Dean remnants affect southern California

Sunday, August 26th, 2007

GOES-11 water vapor images (Animated GIF)

An animation of GOES-11 water vapor channel images (above) showed that Atlantic Hurricane Dean made landfall in Mexico on 22 August 2007, and eventually emerged into the Pacific basin on 23 August; the middle/upper tropospheric moisture associated with the remnants of Dean then moved slowly northward across the Baja California region toward southern California during the next several days. AWIPS GOES-11 water vapor imagery on 26 August 2007 (below) indicated that a good deal of this moisture had spread across much of the southern half of California — this residual moisture (and vorticity) was responsible for helping to initiate numerous thunderstorms (radar animation), some of which produced flash flooding, record daily rainfall, and even a waterspout in the San Diego area.
AWIPS GOES-11 water vapor images (Animated GIF)

GOES sounder Total Precipitable Water (TPW) derived product imagery (below) revealed PW values as high as 40-50 mm (1.6-2.0 inches) over southern California at 14 UTC on 26 August.

GOES sounder total precipitable water

Since the GOES sounder has 3 separate water vapor channels (6.5 µm, 7.0 µm, and 7.4 µm), the TPW can be partitioned into 3 vertical layers: High Layer PW, Mid Layer PW, and Low Layer PW components (below); on this particular day, the bulk of the TPW across southern California appeared to be in the middle layer, which is generally between 700 and 900 hPa (1-3 km, or 3000-10,000 feet).

GOES sounder PW (high layer)

GOES sounder PW (mid layer)

GOES sounder PW (low layer)