Prepare, Prepare and Prepare...
According to the NHC bulk of a hurricane
threat is the tidal surge. It is responsible for more property damage and
loss of life than any other aspect of a hurricane. Tidal surge is the
actual lifting of the ocean by the upward draft of the storm, not the
motion of the surf against the shore. Pacific storms may cause tidal surge
of up to 19 feet. This becomes a particular problem if a storm strikes
your area at high tide. Imagine adding another 19 feet of rise onto the
high tide level! But such extreme tidal surge is rare for the storms that
reach Baja.
Drowning
is the leading cause of death in hurricanes, in the flooding caused by a
tidal surge event. If your property is protected in advance there is no
need for you to be exposed to the elements during the storm.
Once you have made your preparations,
accept that you have done everything you could and retire to a safe place
to observe the storm.
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Also See:
• Prepare, Prepare and Prepare...
• Preparing Particular to Baja
• Batten down the Hatches
• NHC's Hurricane Prep Suggestions

Many people are killed trying to
re-secure property at the height of the storm. Under the force of the wind
and rain you should accept the fact there is very little left you can do.
In 2003 four people died in La Paz
during hurricane Marty from being caught in flood waters. When put in
perspective, more deaths can be attributed to any given severe winter
storm in the US. The majority of the damage in Baja was limited to the
marine community.
Remember to stock your
storm preparedness kit prior
to the onslaught. Learn from experts the best way to protect yourself and
your property. Stay safe, and take wonder at the ferocity of these
monsters of nature.
Stay safe and enjoy!
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The terms "hurricane" and "typhoon" are regionally
specific names for a strong "tropical cyclone". A tropical cyclone is the
generic term for a non-frontal synoptic scale low-pressure system over
tropical or sub-tropical waters with organized convection (i.e.
thunderstorm activity) and definite cyclonic surface wind circulation
(Holland 1993).
Tropical cyclones with maximum sustained surface winds of less than 17 m/s
(34 kt, 39 mph) are called "tropical depressions". (This is not to be
confused with the condition mid-latitude people get during a long, cold
and grey winter wishing they could be closer to the equator ;-)) Once the
tropical cyclone reaches winds of at least 17 m/s they are typically
called a "tropical storm" and assigned a name. If winds reach 33 m/s (64
kt, 74 mph)), then they are called: a "hurricane" (the North Atlantic
Ocean, the Northeast Pacific Ocean east of the dateline, or the South
Pacific Ocean east of 160E); a "typhoon" (the Northwest Pacific Ocean west
of the dateline); a "severe tropical cyclone" (the Southwest Pacific Ocean
west of 160E or Southeast Indian Ocean east of 90E); a "severe cyclonic
storm" (the North Indian Ocean); and a "tropical cyclone" (the Southwest
Indian Ocean) (Neumann 1993).
| Type |
Category |
Pressure (mb) |
Winds
(knots) |
Winds
(mph) |
Surge (ft) |
|
Depression |
TD |
----- |
< 34 |
< 39 |
|
|
Tropical
Storm |
TS |
----- |
34-63 |
39-73 |
|
|
Hurricane |
1 |
> 980 |
64-82 |
74-95 |
4-5 |
|
Hurricane |
2 |
965-980 |
83-95 |
96-110 |
6-8 |
|
Hurricane |
3 |
945-965 |
96-113 |
111-130 |
9-12 |
|
Hurricane |
4 |
920-945 |
114-135 |
131-155 |
13-18 |
|
Hurricane |
5 |
< 920 |
>135 |
>155 |
>18 |
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