Hawaiian Islands Satellite Interpretation Message
Tue, 21 Dec 2010 18:30:00 -0600
Based on data through 0000 UTC December 22 2010.
Water vapor imagery shows a broad upper level ridge over the central Pacific. An embedded shortwave trough is located near 26°N 166°W, or about 600 miles northwest of Kauai. This trough is moving to the northeast at 30 mph. A second trough is located from 21°N 152°W to 14°N 160°W, located just east of the Big Island. This trough is moving to the east at 15 mph.
The northern edge of a 200 mile wide band of clouds associated with a dissipating front extends from 30°N 162°W to 25°N 154°W to 22°N 140°W. The band is composed mainly of overcast cumulus and stratocumulus elements, but with areas of broken middle and high level clouds as well. Isolated towering cumulus and cumulonimbus clouds are also located along the western edge of this frontal band north of 27°N. Cloud tops extend up to 34000 ft. The overall band is nearly stationary. However individual cloud elements are moving to the northwest at 20 mph west of 150°W, and to the west southwest at 15 mph east of 150°W.
Additional areas of broken layered clouds are located south of the frontal band, generally north of 15°N between 150°W and 157°W. Isolated cumulonimbus clouds are embedded within these layered clouds. Cloud tops extend up to 46000 ft. The cumulonimbus clouds themselves are nearly stationary, although debris clouds from the convection and nearby cirrus clouds are moving to the east at 30 mph.
Additional cumulonimbus clouds are located within 150 miles either side of a line from 10°N 180° to 18°N 171°W to 19°N 163°W. Cloud tops extend as high as 46000 ft east of 170°W, and as high as 40000 ft west of 170°W. Individual convective updrafts are short lived, but additional convective clouds continue to develop through the same area. These cumulonimbus clouds are embedded within a larger area of layered middle and high level clouds associated with the two upper troughs.
Across the main Hawaiian islands, overcast low clouds cover the interior and coastal sections of Kauai. Broken to overcast low clouds cover the slopes of the Koolau and Waianae ranges on Oahu. Broken to overcast low clouds cover the eastern half of Molokai, with scattered to broken low clouds across the western half. Overcast low clouds cover the interior of Lanai. Overcast low clouds cover the west Maui mountains. Eastern Maui and the Big Island are located under a general band of broken to overcast layered clouds. Isolated cumulonimbus clouds are also located over the leeward slopes of the Big Island. The layered clouds extend 50 miles offshore to the west of the Big Island, and nearly 200 miles offshore to the northeast and southeast of the Big Island.
Farther northeast and east of the state, low clouds are embedded in the low-level flow. North of 20°N, clouds are composed of broken stratocumulus and closed cell cumulus elements. These clouds are moving to the south and southwest at 15 to 20 mph. South of 20°N, clouds are composed of scattered to broken cumulus elements. These clouds are moving to the west southwest at 15 to 20 mph.
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