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Volume 56, Number 3 December 2012 Photo by Denice Drass

Volume 56, Number 3 December 2012 Photo by Denice Drass

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hurricane isaac<br />

<strong>December</strong> <strong>2012</strong> ~ Mariners Weather Log<br />

18<br />

there were 3.5 ft. setups. Since the local<br />

wind speed did not exceed 20 knots, the<br />

over-water wind speed further offshore<br />

must be higher.<br />

Because of the storm track and the<br />

geographic setting of Mississippi Sound<br />

and surrounding waters, both Stations at<br />

WYCM6 and SHBL1 experienced high<br />

wind speeds and storm surges as shown<br />

in Figs.6 through 9.<br />

Fig.6 shows that there were<br />

approximately 8 ft. positive surge and<br />

10 ft. storm tides at Bay Waveland Yacht<br />

Club, MS. At Shell Beach, LA, both<br />

positive surge and storm tides were<br />

11 ft. (Fig.8). During the period from<br />

August 27 through 30 when Isaac was<br />

over the Gulf of Mexico, there were no<br />

set-down or negative surges measured<br />

at WYCM6 and SHBL1. At WYCM6,<br />

the wind speed and gust were over 45<br />

and 55 knots, respectively (Fig.7), and<br />

at SHBL1, they were 55 and 70 knots,<br />

respectively (Fig.9). Note that these<br />

positive surges can propagate into<br />

near<strong>by</strong> Lake Pontchartrain and Lake<br />

Maurepas. They can also block or<br />

prohibit the drainage of large runoff due<br />

to heavy rainfall from many streams.<br />

This phenomenon can cause widespread<br />

coastal flooding.<br />

Characteristics of storm surges, wind<br />

speed and direction, wind gust, and<br />

atmospheric pressure near the center of<br />

Isaac are provided in Figs.10 through 12<br />

for PSTL1 and Figs.13 through 15 for<br />

GISL1, respectively. Notice that during<br />

the passage of the center, wind direction<br />

changed swiftly from northerly to<br />

southerly. At the same time, wind<br />

speed decreased and then increased<br />

rapidly. Storm surge and storm tide<br />

peaked approximately 3.8 ft. and 4.5 ft.,<br />

respectively. Similar condition occurred<br />

at Grand Isle, LA, where storm surge<br />

and storm tide reached 4.2 and 5.7 ft.,<br />

respectively. Note that the minimum<br />

sea-level pressure was 970 millibar<br />

(mb) at both locations. Note also that<br />

at both locations, the sustained wind<br />

speed and gust reached 60 and 80 knots,<br />

respectively.<br />

Fig.2. Storm surges at Naples, FL during isaac.<br />

Fig.3.Wind direction, speed, and wind gust at Naples, FL during isaac.<br />

Fig.4. Storm surges at Pensacola, FL during isaac.

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