(June 2013)
INTRODUCTION
Commercial and personal
lines insurance coverage forms and policies both cover windstorm and hail
damage. As with fire and explosion, they do not define these terms. As a
result, dictionary definitions and court precedents must be used to determine
losses that are covered and those that are not. The Insurance Services Office
(ISO) CP 10 10–Causes of Loss–Basic Form and CP 10 20–Causes of Loss–Broad Form
cover windstorm and hail but exclude loss or damage caused by or that results
from:
- Frost
- Cold weather
- Ice, snow, or sleet
Note: This does not include hail.
- Interior damage to buildings or structures (or
personal property located inside a building or structure caused by rain,
snow, sand, or dust) unless these damaging elements entered the interior
through breaches or openings made in the roof or walls
The last two exclusions
specifically state that the exclusion applies regardless of whether the element
was wind-driven or not.
CP 10 30–Causes of
Loss–Special Form approaches things a bit differently. It does not specifically
list windstorm or hail as covered but coverage applies because neither is
excluded. However, it excludes loss or damage caused by rain, snow, ice, or
sleet, or damage to personal property in the open. It also limits damage to the
interior of the building or structure and to personal property inside from
rain, sleet, sand, or dust to apply only if a covered cause of loss first
breaches or damages the building and that allows the elements to enter. The
limitation states that coverage does not apply unless the building or structure
is first breached or damaged, even if the elements are wind-driven.
Related Court Cases:
"Opening" In Roof as Condition of Interior Damage Coverage Examined
Storm Damage
Held Not Covered By Virtue Of Ice, Snow, or Sleet Exclusion
Note: All maps
used in this article are copyrighted by and used with the permission of CDS
Business Mapping at www.cdsys.com.
DEFINITIONS
Several terms must be
defined to better understand the coverages provided. Each is the dictionary
definition or as defined in scientific or research articles and papers. Black's
Law Dictionary does not define any of these terms.
The American
Heritage Science Dictionary
defines rain as water
that condenses from water vapor in the atmosphere that falls to Earth as
separate drops from clouds.
The American
Heritage College Dictionary defines wind as moving air, especially a
natural and perceptible movement of air parallel to or along the ground.
The American Heritage Science Dictionary
defines wind as a current of air,
especially a natural one, that moves along or parallel to the ground, moving
from an area of high pressure to an area of low pressure.
The American
Heritage College Dictionary
defines windstorm as a storm with high winds or violent gusts but with
little or no rain.
· Hail
The America
Heritage College Dictionary
defines hail as precipitation in the form of spherical or irregular
pellets of ice larger than 5 millimeters (0.2 inches) in diameter.
WINDSTORM
Wind and windstorm are
different causes of loss. Consider the following loss examples:
- The light breeze that blows through the house from
the front to the back often causes the front door to slam. This results in
cracked window frames and panes.
- A storm door left ajar slams constantly against the
outside wall of the house. This causes a crack to develop in the outside
wall.
- A strong blast of wind enters the home through a mesh
screen door and blows over a lamp.
Wind causes these losses.
Insurance coverage does not apply because the loss or damage is not a direct
result of windstorm.
Windstorm refers only to
the wind. It does not refer to the rain and water that may accompany it. This
very important distinction is frequently made following a hurricane. Hurricanes
and tornados are not defined in any insurance coverage, even though both terms
contribute to the lively discussion of what is covered. Windstorm damage is
limited to damage the wind causes. Water damage that may accompany the
windstorm is not covered as windstorm. In addition, sand driven by wind is also
excluded.
Examples:
- Siding ripped from the side of a house is covered
because the wind caused the siding to rip.
- Sand driven by the wind through gaps in the
windows, doors, and siding is not covered because the wind did not
damage the structure. The sand did the damage.
- A wind-driven wave surge floods a building. This is
the major point of dispute following a hurricane. What damage did the
wind cause and what damage did the flood cause?
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In August 2011 RiskMeter Online announced that the following are the top
ten tornado-prone areas in the United States, based on its research:
- Denver,
CO (rural, not urban)
- Hialeah,
FL
- Miami, FL
- Hollywood,
FL
- Aurora,
CO
- Houston,
TX
- Commerce
City, CO
- Tampa, FL
- St.
Petersburg, FL
- North
Little Rock, AR

HAIL
Hail falls along paths
scientists call hail swaths. Their size can vary from a few acres to up to 10
miles wide, 100 miles long, and leave piles of hail that must be removed by
snowplows or bulldozers. Hail causes significant damage to crops in the United
States every year, in amounts that run into the hundreds of millions of
dollars. Farmers cope with the hail hazard by purchasing insurance.
Hail in the United States
is most prevalent in the area known as "Hail Alley." This consists of
the states of Colorado, Kansas, Oklahoma, and Texas. Parts of this region
average between seven and nine hail days per year. Hail is also much more
common along mountain ranges because mountains force horizontal winds upwards.
This intensifies the updrafts within thunderstorms and makes hail more likely.
In September 2011 RiskMeter Online announced that the following are the top
ten hail prone areas in the United States, based on its research:
- Amarillo,
TX
- Wichita,
KS
- Tulsa, OK
- Oklahoma
City, OK
- Midwest
City, OK
- Aurora,
CO
- Colorado
Springs, CO
- Kansas
City, KS
- Fort
Worth, TX
- Denver,
CO


WINDSTORM EXCLUSIONS AND DEDUCTIBLES
Many insurance companies
issue policies that exclude windstorm (or make the coverage subject to
significant deductibles) because of concern about potential hurricane damage.
Properties subject to
windstorm exclusions may be eligible for coverage in a Beach FAIR Plan. These
plans are available in Alabama, Florida, Louisiana, Mississippi, North
Carolina, South Carolina, and Texas. They cover virtually all real and personal
property in the designated beach area. There are variations in the type of
eligible property among the various states. Each state has a maximum limit per
structure but the limits change regularly. It is important to investigate the
plans in each state to determine the cap. These plans are NOT a substitute for
the coverage the National Flood Insurance Program (NFIP) provides. Beach FAIR
Plan policies cover only wind damage. NFIP flood policies cover only flood
damage.
Related Article:
Overview of the National Flood Insurance Program
When a separate windstorm
deductible is used, it is usually a percentage deductible based on the limit of
insurance, not the value of the loss. Most windstorm deductible endorsements
are state-specific and should be read carefully and explained to the insured
thoroughly because of the way they are applied.
Example: Michelle owns a large apartment building and insures if
for $3,000,000. She has a $1,000 deductible on all causes of loss except
windstorm, which is subject to a 5% deductible. A windstorm causes $50,000 in
damage to her building. She expects to receive $50,000 - $2,500 ($50,000 X
.05) or $47,500 for her claim. She is very surprised and extremely
disappointed when informed that her deductible is actually $150,000
($3,000,000 X .05) and that she will not receive anything for her $50,000
loss.
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Note: These same
exclusions and deductible forms can be used in areas of the Midwest where hail
may be a major concern.
CONCLUSION
When does wind become a
windstorm? Was there really hail damage or was it an existing condition? The
observation of damage is the only determining factor and damage unfortunately
is in the “eye of the beholder.” The claims adjustor and the insured may have
differences of opinion that only an impartial court of law can resolve. Because
scientific evidence is important to any argument, the following three different
wind scales are presented that may be cited to justify either side of the
argument.
BEAUFORT WIND SCALE
British Rear-Admiral Sir
Francis Beaufort developed this scale in 1805, based on his observations of the
effects of wind. He was a British hydrographer (a
scientist who studies surface waters, especially with regard to navigating
them). This is the earliest formal wind scale. It provides the standards of
wind velocity measurements that mariners and the United States Weather Bureau
use, with some modifications made for terminology. These meteorological
standards are helpful to clarify the meaning of "windstorm" for
insurance purposes. This wind scale differs from the others in that it measures
straight-line wind forces as opposed to the effects of rotating winds.
The speed of a current of
air and its direction determines whether it is harmful or beneficial. A wind
current of 19 to 24 miles an hour is classified as a fresh breeze and is not
harmful. When wind reaches a speed of 48 miles an hour, it is classified as a
strong gale and may cause some damage to fruit crops. At 64 to 75 miles per
hour, wind is classified as a windstorm and is dangerous to both crops and
property. Hurricanes and tornadoes involve winds in excess of 75 miles per
hour. The Beaufort Wind Scale, based on the effect of wind on ships, and
adopted in substance by the United States Weather Bureau, appears below.
Beaufort Wind Scale
|
Scale
|
Wind Description Wave Height in feet
|
Speed
(mph)
|
Speed
(knots)
|
Effects on land or sea
|
0
|
Calm
None
|
0–1
|
0–1
|
Smoke rises vertically.
Sea is like a mirror.
|
1
|
Light air
0.25
|
1–3
|
1–3
|
Smoke drifts slowly.
Ripples on the water appear as scales.
|
2
|
Light breeze
0.5–1.0
|
4–7
|
4–6
|
Leaves rustle. Small
wavelets. Crests appear glassy.
|
3
|
Gentle breeze
2.0–3.0
|
8–12
|
7–10
|
Leaves and twigs move.
Large wavelets. Crests break. Scattered whitecaps.
|
4
|
Moderate breeze
3.5–5.0
|
13–18
|
11–16
|
Small branches move.
Small waves become longer. Numerous whitecaps.
|
5
|
Fresh breeze
6.0–8.0
|
19–24
|
17–21
|
Small trees sway.
Moderate waves. Many whitecaps. Spray
|
6
|
Strong breeze
9.5–13.0
|
25–31
|
22–27
|
Large branches sway.
Larger waves. Whitecaps. Spray.
|
7
|
Moderate (near) gale
13.5–19.0
|
32–38
|
28–33
|
Whole trees move. Sea
heaps up. White foam from waves.
|
8
|
Gale
18.0–25.0
|
39–46
|
34–40
|
Twigs break off trees.
Medium high and long waves.
|
9
|
Strong gale
23.0–32.0
|
47–54
|
41–47
|
Branches break. High
waves. Sea rolls. Foam. Low visibility.
|
10
|
Whole gale/storm
29.0–41.0
|
55–63
|
48–55
|
Trees snap and blow
down. High waves and overhanging crests. Heavy rolling.
|
11
|
Violent storm
37.0–52.0
|
64–75
|
56–63
|
Widespread damage.
Exceptionally high waves.
|
12
|
Hurricane
45.0 and over
|
Over 75
|
Over 64
|
Extreme damage. Air
filled with foam. Sea completely white with driving spray.
|
ENHANCED FUJITA SCALE (EF SCALE)
This scale was introduced
to the public in 2007. The previous scale was introduced in 1971 before there
were many more advanced meteorological measuring devices. This new table still
depends on observations at the scene of the tornado’s impact but more
accurately estimates a tornado's speed. Tornadoes may develop a counterclockwise,
swirling motion that exceeds 100 miles per hour and cause incredible
destruction. Tornadoes occur most often in the central Mississippi Valley
region of the United States. It is important to note that neither the size of
the funnel nor the length of time it remains on the ground have any effect on
the scale.
Enhanced Fujita Scale (EF Scale)
|
Scale
|
Description
|
Speed
|
Effects
|
|
Light damage
|
65-85 mph
|
Some roof, gutter and
siding damage. Limited amount of branches broken from trees and some shallow
rooted trees pushed over.
|
EF1
|
Moderate damage
|
86-110 mph
|
Severe roof damage. Overturned
and badly damaged mobile homes. Exterior doors and windows lost and glass
broken.
|
EF2
|
Considerable damage
|
111–135 mph
|
Roofs torn off. Home
foundations shift. Complete destruction of mobile homes. Uprooting or
breaking of large trees. Small or light objects turned into missiles. Winds
lift cars off the ground.
|
EF3
|
Severe damage
|
136–165 mph
|
Destruction of upper
levels of well-constructed homes. Large buildings such as shopping malls
severely damaged. Debarking of trees. Overturning of trains. Wind lifts and
throws heavy cars. Any structure without a substantial foundation blown a
distance away.
|
EF4
|
Devastating damage
|
|
Leveling of
well-constructed houses. Cars thrown and small missiles generated.
|
EF5
|
Incredible damage
|
Over 200 mph
|
Well-constructed houses
pulled off foundations and swept away. Heavy items such as automobiles become
missiles. Significant damage to steel reinforced concrete structures. Structural
damage to high-rise buildings.
|
SAFFIR-SIMPSON WIND SCALE
The Saffir-Simpson
wind scale places a hurricane in one of five categories according to its
strength. It was created in the early 1970s. Category one is the weakest
hurricane strength measured and category five is the strongest. A hurricane's
strength is based on its wind speed. The height of the storm surge depends on
the slope of the continental shelf connected to the area where the storm
strikes. Wind speeds below 74 miles per hour are measured according to the
Beaufort Wind Scale. This scale rates the severity of a hurricane based on its
barometric pressure, wind speed, storm surge, and damage potential.
Saffir-Simpson Wind Scale
|
Scale
|
Barometric Pressure
|
Wind Speed
|
Storm Surge
|
Damage
|
Effects
|
1
|
Greater than 28.94
|
74–95 mph
|
4–5 feet
|
Minimal–Gale force
|
No real damage to
building structures. Damage primarily to unanchored mobile homes, shrubbery,
and trees. Some coastal flooding of low-lying roads and minor pier damage.
Storm surge 4 to 5 feet above normal.
Examples: Hurricane Lili in 2002 and
Hurricane Gaston in 2004
|
2
|
28.50 to 28.93
|
96–110 mph
|
|
Moderate force
|
Some roofing material,
door, and window damage to buildings. Considerable damage to shrubbery, trees,
and mobile homes. Flooding damages piers. Small craft in unprotected moorings
may break their moorings. Storm surge 6 to 8 feet above normal.
Example: Hurricane Isabel in 2003 and Hurricane Frances in 2004
|
3
|
27.91 to 28.49
|
111–130 mph
|
9–12 feet
|
Extensive–Significant
force
|
Some structural damage
to small residences and utility buildings. Large trees blown down. Mobile
homes destroyed. Coastal flooding destroys smaller structures. Larger coastal
structures damaged by floating debris. Terrain lower than 5 feet at sea level
flooded 8 miles or more inland. Evacuation of low-lying residences near the
coastline. Storm surge 9 to 12 feet above normal.
Example: Hurricanes Jeanne and Ivan in 2004. Hurricane Katrina in 2005
was a category 4 in the Gulf of Mexico but was only a category 3 when it made
landfall.
|
4
|
27.17 to 27.90
|
131–155 mph
|
13–18 feet
|
Extreme force
|
Severe damage to roofs,
doors, and windows. Mobile homes completely destroyed. Major beach erosion.
Major damage to lower floors of shoreline structures. Low-lying areas flooded
up to 6 miles inland. Massive evacuation of residential areas up to 6 miles
inland. Storm surge 13 to 18 feet above normal.
Examples: Hurricane Charlie in 2004 and Hurricane Dennis in 2005
|
5
|
Less than 27.17
|
|
Over 18 feet
|
Catas-
trophic
|
Complete roof failure
on many residences and industrial buildings. Some complete building failures.
Small utility buildings overturned or blown away. Major flooding damage to
lower floors of structures located less than 15 feet above sea level and
within 500 yards of the shoreline. Massive evacuation of low-lying
residential areas within 10 miles of shore. Storm surge over 18 feet above
normal.
Examples: Only three made landfall in the U.S.: The Labor Day
Hurricane of 1935, Hurricane Camille in 1969, and Hurricane Andrew in 1992
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