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What
are my risks?
Do
I live in a flood prone area?
For
information on flooding in your neighborhood, refer to
a Flood Insurance Rate Map (FIRM). These maps are
computed water surface elevations that are combined with
topographic mapping data to develop flood hazard maps.
They provide information on areas subject to flooding.
They are used to guide future development away from flood-prone
areas and to regulate development that is proposed to
occur within such areas.
Even
so, updates to these maps have not kept up with development
in Maui County. Each year, numerous properties not officially
mapped as “flood prone” are flooded.
Call
your Flood Coordinator for information about flooding.
Or, ask your regional librarian to see the Flood Insurance
Rate Map for your community.
Where
have stream floods been recorded on Maui?
Click
to enlarge
Stream
flooding on Maui is not only common, but is also the very
agent responsible for making it famous as the Valley Island.
Annual
rainfall is greatest (360 inches) at the summit of west
Maui and nearly as high (280 inches) along the eastern
flanks of east Maui just below the trade wind inversion.
Rainfall is lowest (<15 inches) in the vicinity of Kihei
and Lahaina.
Flooding
in areas around Lahaina and Kihei are in part a result
of the abrupt transition in slope at the coastline and
the behavior of flash flooding. Many flash floods in these
areas occurred after heavy rainfall in higher elevations
- in some cases equaling the average annual maximum, like
in December 1988.
The
north central portion of Maui and the Hana coast have
the greatest stream flooding histories. Nearly once a
decade, water sheets into the urban centers of Kahului
and Wailuku (e.g., November 1950 and 1960). Along the
road to Hana temporary road closures are common due to
flash floods and mudslides from the steeper slopes of
East Haleakala.
In
addition, the Lahaina region and Kihei are vulnerable
to standing surface water flooding. This may interrupt
transportation and damage low elevation buildings. Standing
surface water develops after intense rainfall events where
poor soil permeability and urbanization prevent adequate
drainage and temporarily disrupting transportation.
Where
have high waves been recorded on Maui?
Click
to enlarge
Waves
from north and northwest swell tend to be highest on an
annual basis and generally occur between October and March.
Wave heights associated with these swells range between
5-10 feet (Kaanapali) and 10-20 feet (Honolua Bay, Waihee
to Paia).
Occasionally,
waves of 25 feet and greater occur over the deep offshore
reefs of the North Shore. Two of the largest wave events
occurred February 1993 and January 1998, when waves reached
heights of 30 and 40 feet, respectively.
The
southern shores of Maui are partly protected from south
swell in summer by the islands of Kahoolawe and Lanai.
Even so, wave heights range between 4 and 6 feet and,
at times, reach 8-10 feet. During winter months, Kona
Storm waves can reach 5 feet.
Trade
wind waves, usually between 3 and 4 feet, impact the eastern
shores 70% of the time.
In
the summer months, tropical storms and hurricanes can
generate wave heights of 10-20 feet along any portion
of coast on Maui. Hurricanes Susan, Ignacio, and Estelle
generated 10-15 foot waves along the north and east shores.
Along the west shore, Hurricane Emilia caused wave heights
of 6-10 feet.
Fortunately
for Maui, much of its coastline has wide fringing reefs
that dissipate wave energy offshore of its northern and
western shores, where wave heights are highest.
Also,
relative to the other islands, there are only a few locations
where development along the shore is subject to direct
impact by high waves. Unfortunately, however, areas important
for tourism and commerce such as Lahaina, Kaanapali, Honokowai,
Olowalu, Kihei, and Kahului are sited on low coastal plains,
and so experience periodic wave overwash, causing rapid
erosion and temporarily disrupting transportation.
Source:
Fletcher, Charles, Eric Grossman, Bruce Richmond. Atlas
of Natural Hazards in the Hawaiian Coastal Zone. 2000. |