Volume 56, Number 3 December 2012 Photo by Denice Drass
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.