Floods & Flash Floods

The transformation of a tranquil river or normally dry wash into a destructive flood occurs hundreds of times each year, in every part of the United States. Every year, floods drive some 75,000 Americans from their homes; on the average, 127 persons are killed each year. These destructive overflows have caused property damage in some years estimated at more than $2 billion. During the years 1985–2001, the total annual number of floods or flash floods ranged from 361 (1988) to 3,376 in 1998. A total of 32,047 flash flood/flood events were recorded in 1985–2001.

HOW FLOODS HAPPEN

Floods begin when soil and vegetation cannot absorb falling rain or melting snow, or when water runs off the land in such quantities that it cannot be carried in normal stream channels or retained in natural ponds and human-made reservoirs. Flash floods are the result of too much rain falling in too small an area, in too short a time. Flash floods frequently occur in seconds and minutes, while floods occur over hours and days. River Forecast Centers issue flood

forecasts and warnings when the rain that has fallen is enough to cause waterways to overflow their banks, and when melting snow combines with rainfall to produce similar effects.

FLASH FLOODS

Typically, flash floods occur primarily at night and when there is an abundance of atmospheric moisture; in addition, there is usually little, if any, vertical wind shear present. Flash flooding can be produced by large, slow-moving storms or as a result of "train effect" storms (i.e., sequential mature storms that release precipitation over the same area). Train effect storms can be part of multicell cluster or squall line storm systems.

Flash-flood waves, moving at incredible speeds, can roll boulders, tear out trees, destroy buildings and bridges, and scour out new channels. Killing walls of water can reach 10–20 ft.

On small streams, especially near the headwaters of river basins, water levels may rise quickly in heavy rainstorms,

and flash floods can begin before the rain stops falling. There is little time between detection and flood crest. Swift action is essential for the protection of life and property.

FLOOD EVENTS

The Great Flood of 1993

In terms of precipitation amounts, record river stages, extent of flooding, persons displaced, crop and property damage, and flood duration, the Great Flood of 1993 was perhaps the worst hydrometeorological event to occur since the United States started to provide weather services in the late 1800s.

Record and near-record precipitation during the spring of 1993, on soil saturated from previous seasonal precipitation, resulted in flooding along many of the major river systems and their tributaries in the Upper Midwest during the summer of 1993.

Spring flooding began in March as a result of a previous wet fall, normal to above-normal snow accumulation, and rapid spring snowmelt accompanied by heavy spring rainfall.

By May 8, however, record flooding occurred in South Dakota on Split Rock Creek at Corson and in Minnesota on the Rock River in Luverne. On May 22–24, heavy thunderstorms produced 3–7 in of rain in three hours over Sioux Falls, South Dakota, resulting in major urban and residential flooding across the city. The Big Sioux and Vermillion Rivers in South Dakota went above flood stage in late May and remained in flood through mid-June. Major flooding continued throughout the summer along the Missouri and Mississippi Rivers—by September 1, 1993, for example, the towns of Hannibal, Louisiana, and Clarksville, Missouri, had experienced 153 consecutive days of flooding. Flooding at levels above the flood stages continued through the middle of September in many regions along the Mississippi River.

Records broken in 1993

In 1993, flood records were broken at 44 forecast points on the upper Mississippi River system, at 49 forecast points on the Missouri River system, and at two forecast points on the Red River of the North system. Within the Mississippi River system, 1993 floods of record include those set at 15 forecast points on the main stem, at four forecast points on the Iowa River, at five forecast points on the Des Moines River, and at two forecast points on the Raccoon River.

Within the Missouri River system, 1993 records were set at 14 forecast points on the main stem and at four forecast points on each of the Saline, Smoky Hill, and Grand Rivers. Record 1993 flood stages surpassed old record stages by more than 6 ft in some cases. For example, in 1993, flood records set more than 42 years ago on the main stem of the Missouri were broken by more than 4 ft at multiple forecast points. In at least one case, a new record was established early on but was broken by higher water later. The historic record on the Mississippi at St. Louis was established on April 28, 1973, at 43.2 ft; reestablished on July 21, 1993, with a flood stage of 46.9 ft; and again reestablished 11 days later on August 1, 1993, with a record flood stage of 49.6 ft.

Flood damages of 1993

Damage caused by these record flood stages was massive. Over 17,000 mi ² were inundated by the flood (the 1937 flood in the same region affected only 12,700 mi ² ). It is estimated that the region suffered over $8 billion in damages; President Clinton declared more than 200 counties federal disaster areas, including all 99 counties in Iowa. Amazingly, only 26 individuals died as a direct result of the flood. Compare that figure to 23 killed in the 1973 flood and 250 in the 1937 flood of the same region and then to the 2,100 killed in the one-day Jamestown, Pennsylvania, flood in 1889. The decreased death tolls can be attributed to abundant warnings, well-executed evacuation plans, lack of flash floods, and foremost, the protection provided by the system of flood-controlling levees in the area.

The duration and magnitude of the Great Flood of 1993, as well as its leading conditions, strongly support the premise that this event was a significant climate variation rather than simply a sequence of meteorological events. It is quite possible that one or more climate-driving forces significantly contributed to this variation. (For example, a shift in the jet stream acted as a barrier to a cold front, bringing 150–200% more precipitation to the area than usual.) A more thorough analysis of this situation is expected to result in improved understanding of the roles contributing factors may have played.

Flooding in California, 1995

In January and March of 1995, large sections of northern and central California were hit with heavy precipitation and subsequent flooding, resulting in record losses of $2–3 billion. Over 10,000 homes were lost or destroyed and 27 lives were lost. In the end, all state counties but one were declared federal disaster areas.

Throughout the early winter and spring of 1995, a strong and displaced Pacific jet stream funneled storm systems and heavy moisture into California. These systems produced severe thunderstorms and sometimes tornadoes. The heavier-than-normal precipitation flooded small streams; this flooding spread to tributaries and larger rivers. Precipitation

(which accumulated as snow) at altitudes of 5,000 ft or more also contributed to the flooding as melting and runoff. By March, the snow depth in some areas of the Sierra Nevada range were reported to be as high as 40 ft.

Floods of 1997

During the winter of 1996-97, substantial snow fell across north-central and western sections of the United States. As this snow began to melt, the potential for significant flooding existed across these areas. Heavy rainfall during February 1997 caused flooding across portions of the Southeast, middle and lower Mississippi Valley, and the Great Lakes regions, and added to the possibility of continued flooding in these areas with heavy spring rains. In early March, torrential rains of up to 12 in in 36 hours fell across the Ohio River Basin. This caused disastrous flooding throughout the basin, and the flood crest in March reached the confluence with the Mississippi.

Areas of elevated risk for spring flooding included the northern Plains, most of the Mississippi Valley, the western Great Lakes region, and much of the lower Missouri and Ohio Valleys, as well as a substantial area in the Southeast, extending from eastern Texas through South Carolina, excluding southern Alabama, Georgia, and all of Florida. Of particular concern were the Red River along the North Dakota-Minnesota state line, and the James River in South Dakota. There, the water content of the snow over the entire drainage south of Fargo, North Dakota, was exceptionally high and could cause serious flooding.

Flooding of March 1997

During February 1997, the middle third of the nation saw the passage of several very wet storm systems, and many of these areas accumulated more than 150% of normal precipitation for the month. In early March, this general pattern continued, and included the deluge that caused catastrophic flooding in portions of the Ohio Valley.

During late February or early March, a total of 18 states across the central and eastern United States were affected by river flooding, the most serious of which was observed along the south of the middle and lower Ohio River. Flow volume was reported four to 10 times the normal (for the date) along smaller rivers and creeks in Kentucky and Ohio alone. As of March 10, flooding had resulted in: 98 counties being declared federal disaster areas; damage to at least 100,000 structures; destruction of roads and bridges, and contamination of public water supplies; and the deaths of approximately 30 people.

Pacific Northwest floods, 1997

In 1997, there was also serious concern for spring flooding in the northern and central Rocky Mountains—particularly in Idaho and Montana—and in parts of Wyoming, Utah, and Colorado, as snow pack totals were well above average. Most of the higher elevations of Washington and northern Oregon also had much above-average snow packs and were in some jeopardy of flooding. Finally, deep snow packs in the central and southern Sierra Nevada increased the possibility of snowmelt flooding in western Nevada and in the Sacramento and San Joaquin River drainages in California.

Precipitation and snow accumulation since the end of January was lighter than normal throughout much of the West. In particular, there was some optimism that areas along the West Coast, disastrously inundated at the start of the year, might escape the spring without additional serious flooding. This dry period allowed water managers to draw down reservoirs to provide storage capacity for at least some of the spring snowmelt. Many reservoirs had filled to very high levels earlier in the year.

PRECIPITATION WORLDWIDE IN 2000

Global precipitation was also above-average in 2000. It is estimated that 2000 ended as one of the 10 wettest years on record. Precipitation in the tropics was heavily influenced by La Niña throughout much of the year, with above average precipitation in Indonesia and the western tropical Pacific, while drier than normal conditions were common in the central tropical Pacific. La Niña also contributed to above normal precipitation in northeast South America and southern Africa and enhanced monsoonal precipitation in southern Asia. Below normal precipitation across equatorial areas of East Africa and the Gulf Coast of the United States is also attributable to La Niña conditions.

PRECIPITATION WORLDWIDE IN 2001

Global precipitation was below the 1961–1990 average in 2001. A drought that has persisted for nearly three years continued in 2001 across Afghanistan, Pakistan, and neighboring countries. In Iran, estimated agricultural losses approached $2.6 billion (USD). Much of Central America experienced drought during the middle part of the year, which is traditionally the rainy season. Late season tropical activity eased drought in these areas, although drought in Honduras and neighboring regions continued through the latter part of 2001. In Africa, drought in Kenya persisted during 2001, despite one of the wettest Januaries in 40 years. In Australia, drought affected much of Western Australia and parts of Queensland.

Several typhoons brought excessive rains to parts of Southeast Asia, including the southeast coast of China, Taiwan, the Philippines, and Vietnam. Monsoon rains in Southeast Asia promoted extensive flooding along the Mekong Delta with at least several hundred deaths between August and October. Across Siberia, spring rains and a rapid thaw brought flooding across a vast area from the Ural Mountains to the Russian Far East, with some of the worst flooding in the Sakha region along the Lena River. A third consecutive year of spring flooding along the Tisza River in Hungary displaced tens of thousands of people from their homes, with the Tisza rising to its highest level in 100 years by early March.

PRECIPITATION IN THE UNITED STATES FOR 2001

Precipitation was below average for the conterminous United States in 2001. The estimated January–December anomaly was 0.7 inches below the long-term mean. This value could change based on conditions in December. This year marked the third consecutive year of below normal precipitation, following nine years of precipitation surpluses.

PRELIMINARY GLOBAL PRECIPITATION FOR 2002

Global precipitation was below the 1961–1990 average in 2002. Much of Australia experienced severe drought, with the eastern part of the country the worst affected. India monsoon rainfall was 19% below normal, with the resulting drought characterized as the worst since 1987. Other drought-affected areas included the western United States and portions of the north coast of China.

After a dry beginning to 2002, several typhoons brought excessive rains to parts of Southeast Asia and Japan, the southeast coast of China, Taiwan, and the Philippines. In contrast to drought conditions during the first half of 2002, the onset of monsoon rains in Southeast Asia promoted extensive flooding along the Mekong Delta. Seasonal flooding in much of south Asia (Nepal, Bangladesh, and northeastern India) during June–August claimed more than 1,000 lives. In the eastern United States, long-term drought was ameliorated by a turn to wetter weather, due in part to moisture from tropical systems.

PRELIMINARY NATIONAL PRECIPITATION FOR 2002

During 2002, more than a tenth of the country was very dry in 8 of the 11 months, and in February and May more than 20% of the country was very dry. Only in September and October did the percentage area of very wet conditions exceed 10%, though in October more than 20% of the country was very wet. This was due in part to several landfalling tropical systems during these two months. Drought improvement generally occurred in the eastern U.S. during 2002, while in much of the western half of the country and the central and southern Great Lakes drought worsened.

Precipitation in the United States in 2002 was characterized by extreme dryness in the West, above-average wetness in the Mississippi Valley region, and dryness giving way to near average conditions for the East. Colorado is on pace to have its driest year on record during 2002, and Wyoming and Arizona to have their second driest years. Eight states will likely be much drier than normal, and the West region as a whole will be the driest on record.

Louisiana had its wettest fall on record, in part due to two landfalling tropical systems that hit the state in September and October. It was the third driest July and August combined for the Northeast. Considerable improvement in drought conditions for the East Coast occurred in the fall.

FLOOD WARNINGS

Early flood warnings allow time for residents to leave low-lying areas, and to move personal property, mobile equipment, and livestock to higher ground. Sometimes valuable crops can be harvested in advance of a destructive flood. Emergency and relief organizations can prepare to handle refugees and combat the inevitable health hazards caused by floods.

Flood warnings are forecasts of impending floods, and are distributed to the public by radio and television, and through local emergency forces. The warning message tells the expected severity of flooding (minor, moderate, or major), the affected river, and when and where flooding will begin. Careful preparation and prompt response will reduce property loss and ensure personal safety.

Flash-flood warnings can be issued in minutes and flood warnings can be issued hours to days in advance of the flood peak on major tributaries. Main river flood forecasts can be issued several days or even weeks in advance. In general, the time lapse between rainfall or snowmelt and the rise in river height increases with the size of the river.

WARNING SYSTEMS

Thirteen regional river forecast centers are the first echelon offices that prepare river and flood forecasts and warnings for approximately 3,000 communities.

National Oceanic and Atmospheric Administration's National Weather Service (NWS) has helped set up additional flash-flood warning systems in about 100 communities. In these, a volunteer network of rainfall and river-observing stations is established in the area, and a local flood warning representative is appointed to collect reports from the network. The representative is authorized to issue official flash-flood warnings based on a series of graphs prepared by the NWS. These graphs show the local flooding that will occur under different conditions of soil moisture and rainfall. On the basis of reported rainfall, the representative can prepare a flood forecast from these graphs, and spread a warning within minutes. (Flash-flood warnings are the most urgent type of flood warning issued, and are transmitted to the public over radio, television, and by sirens and other signals.) Communities within range of a NWS radar have the additional protection of advance warning when flood-producing storms approach.

Successful operation of a flash-flood warning system requires active community participation and planning, but very little financial outlay. Still, the communities with cooperative flash-flood warning systems are only a small fraction of the thousands of communities that need them.

USGS FLOOD MEASUREMENTS

The USGS currently (2000) maintains more than 7,000 stream-gaging stations throughout the United States, Puerto Rico, and the Virgin Islands that monitor streamflow and provide data to various federal, state, and local cooperating agencies as well as the general public. Some of these stream-gauging stations have been in operation since before 1900, providing more than a century of water information for the nation. In addition to providing critical information on flood heights and discharges, these stations provide data used in the effective management of water-supply and water-quality needs, protection of aquatic habitat, recreation, and water-resources research.

The basic building block for a stream-flow data network is the stage-discharge relation that is developed at each gauging-station location. Measurements of the flow (discharge) are related graphically to the respective water depths (stage), which then enables discharge to be determined from stage data.

Discharge measurements can either be direct, using a current meter, or indirect, using mathematical flow equations. Both methods require that an elevation of the flood-water surface be determined by a water-depth gauge or by a detailed survey of high-water marks. If time allows and conditions are safe, a direct measurement by USGS hydrographers is preferred. However, during major floods, direct measurements are often impossible or extremely dangerous, and indirect methods must be used.

Accurate identification and measurement of high-water marks from floods are very important in the accurate mapping of inundated areas as well as in the analysis of water-surface profiles for indirect discharge measurements. These elevations, in combination with flood-frequency analysis using many years of annual flood maximums, are used by the Federal Emergency Management Agency (FEMA) to determine flood-insurance rates.

SIGNIFICANT FLOODS OF THE TWENTIETH CENTURY

During the twentieth century, floods were the number-one natural disaster in the United States in terms of number of lives lost and property damaged. They can occur at any time of the year, in any part of the country, and at any time of the day or night. Most lives are lost when people are swept away by flood currents, whereas most property damage results from inundation by sediment-laden water. Flood currents also possess tremendous destructive power, as lateral forces can demolish buildings and erosion can undermine bridge foundations and footings leading to the collapse of structures. The accompanying map and table locate and describe 32 of the most significant floods of the twentieth century.

Floods are the result of a multitude of naturally occurring and human-induced factors, but they all can be defined as the accumulation of too much water in too little time in a

specific area. Types of floods include regional floods; flash floods; ice-jam floods; storm-surge floods; dam- and levee-failure floods; and debris, landslide, and mudflow floods.

Regional floods

Some regional floods occur seasonally when winter or spring rains, coupled with melting snow, fill river basins with too much water too quickly. The ground may be frozen, reducing infiltration into the soil and thereby increasing runoff. Such was the case for the New England flood of March 1936, in which more than 150 lives were lost and property damage totaled $300 million.

Extended wet periods during any part of the year can create saturated soil conditions, after which any additional rain runs off into streams and rivers, until river capacities are exceeded. Regional floods are many times associated with slow-moving, low-pressure, or frontal storm systems, including decaying hurricanes or tropical storms. Persistent wet meteorological patterns are usually responsible for very large regional floods, such as the Mississippi River Basin flood of 1993 wherein damages were $20 billion.

Flash floods

Flash floods can occur within several seconds to several hours, with little warning. Flash floods can be deadly because they produce rapid rises in water levels and have devastating flow velocities. Several factors can contribute to flash flooding. Among these are rainfall intensity, rainfall duration, surface conditions, and topography and slope of the receiving basin. Urban areas are susceptible to flash floods because a high percentage of the surface area is composed of impervious streets, roofs, and parking lots where runoff occurs very rapidly. Mountainous areas also are susceptible to flash floods, as steep topography may funnel runoff into a narrow canyon. Floodwaters accelerated by steep stream slopes can cause the floodwave to move downstream too fast to allow escape, resulting in many deaths. A

Significant Floods of the 20th Century

[M, million; B, billion]

Flood type	Map no.	Date	Area or stream with flooding	Reported deaths	Approximate cost (uninflated)	Comments
Regional flood	1	Mar.-Apr. 1913	Ohio, statewide	467	$143M	Excessive Regional rain.
	2	Apr.-May 1927	Mississippi River from Missouri to Louisiana	unknown	$230M	Record discharge downstream from Cairo, Illinois.
	3	Mar. 1936	New England	150+	$300M	Excessive rainfall on snow.
	4	July 1951	Kansas and Neosho River Basins in Kansas	15	$800M	Excessive regional rain.
	5	Dec. 1964-Jan. 1965	Pacific Northwest	47	$430M	Excessive rainfall on snow.
	6	June 1965	South Platte and Arkansas Rivers in Colorado	24	$570M	14 inches of rain in a few hours in eastern Colorado.
	7	June 1972	Northeastern United States	117	$3.2B	Extra tropical remnants of Hurricane Agnes.
	8	Apr.-June 1983	Shoreline of Great Salt Lake, Utah	unknown	$621M	In June 1986, the Great Salt Lake reached its highest elevation and caused $268M more in property damage.
	9	May 1983	Central and northeast Mississippi	1	$500M	Excessive regional rain.
	10	Nov. 1985	Shenandoah, James, and Roanoke Rivers in Virginia and West Virginia	69	$1.25B	Excessive regional rain.
	11	Apr. 1990	Trinity Arkansas, and Red Rivers in Texas, Arkansas, and Oklahoma	17	$1B	Recurring intense thunderstorms.
	12	Jan. 1993	Gila, Salt, and Santa Cruz Rivers in Arizona	unknown	$400M	Persistent winter precipitation.
	13	May-Sept. 1993	Mississippi River Basin in central United States	48	$20B	Long period of excessive rainfall.
	14	May 1995	South-central United States	32	$5-6B	Rain from recurring thunderstorms.
	15	Jan.-Mar. 1995	California	27	$3B	Frequent winter storms.
	16	Feb. 1996	Pacific Northwest and western Montana	9	$1B	Torrential rains and snowmelt
	17	Dec. 1996-Jan. 1997	Pacific Northwest and Montana	36	$2-3B	Torrential rains and snowmelt
	18	Mar. 1997	Ohio River and tributaries	50+	$500M	Slow-moving frontal system.
	19	Apr.-May 1997	Red River of the North in North Nakota and Minnesota	8	$2B	Very rapid snowmelt.
	20	Sept. 1999	Eastern North Carolina	42	$6B	Slow-moving Hurricane Floyd.
Flash flood	21	June 14, 1903	Willow Creek in Oregon	225	unknown	City of Heppner, Oregon, destroyed.
	22	June 9-10, 1972	Rapid City, South Dakota	237	$160M	15 inches of rain in 5 hours.
	23	July 31, 1976	Big Thompson and Cachela Poudre Rivers in Colorado	144	$39M	Flash flood in canyon after excessive rainfall.
	24	July 19-20, 1977	Conemaugh River in Pennsylvania	78	$300M	12 inches of rain in 6-8 hours.
Ice-jam flood	25	May 1992	Yukon River in Alaska	0	unknown	100-year flood on Yukon River.
Storm-surge flood	26	Sept. 1900	Galveston, Texas	6,000+	unknown	Hurricane
	27	Sept. 1938	Northeast United States	494	$306M	Hurricane
	28	Aug. 1969	Gulf Coast, Mississippi and Louisiana	259	$1.4B	Hurricane Camille
Dam-failure flood	29	Feb. 2, 1972	Buffalo Creek in West Virginia	125	$60M	Dam failure aafter excessive rainfall.
	30	June 5, 1976	Teton River in Idaho	11	$400M	Earthen dam breached.
	31	Nov. 8, 1977	Toccoa Creek in Georgia	39	$2.8M	Dam failure after excessive rainfall.
Mudflow flood	32	May 18, 1980	Toutle and lower Cowlitz Rivers in Washington	60	unknown	Result of eruption of Mt. St. Helens.

flash flood caused by 15 inches of rain in 5 hours from slow-moving thunderstorms killed 237 people in Rapid City, South Dakota, in 1972.

Floodwaves more than 30-feet high have occurred many miles from the rainfall area, catching people unaware. Even desert arroyos are not immune to flash floods, as distant thunderstorms can produce rapid rises in water levels in otherwise dry channels. Early-warning gauges upstream save lives by providing advanced notice of potential deadly floodwaves.

Ice-Jam Floods

Ice-jam floods occur on rivers that are totally or partially frozen. A rise in stream stage will break up a totally frozen river and create ice flows that can pile up on channel obstructions such as shallow riffles, log jams, or bridge piers. The jammed ice creates a dam across the channel over which the water and ice mixture continues to flow, allowing for more jamming to occur. Backwater upstream from the ice dam can rise rapidly and overflow the channel banks. Flooding moves downstream when the ice dam fails, and the water stored behind the dam is released. At this time the flood takes on the characteristics of a flash flood, with the added danger of ice flows that, when driven by the energy of the floodwave, can inflict serious damage on structures. An added danger of being caught in an ice-jam flood is hypothermia, which can kill quickly. Ice jams on the Yukon River in Alaska contributed to severe flooding during the spring breakup of 1992.

Storm-Surge Floods

Storm-surge flooding is water that is pushed up onto otherwise dry land by onshore winds. Friction between the water and the moving air creates drag that, depending upon the distance of water (fetch) and the velocity of the wind, can pile water up to depths greater than 20 feet. Intense low-pressure systems and hurricanes can create storm-surge flooding. The storm surge is unquestionably the most dangerous kind of flood. Nine out of 10 hurricane fatalities are caused by the storm surge. Worst-case scenarios occur when the storm surge occurs concurrently with high tide. Stream flooding is much worse inland during the storm surge because of backwater effects. In September 1900, the hurricane and storm surge at Galveston, Texas, killed more than 6,000 people, making it the worst natural disaster in the nation's history.

Dam- and levee-failure floods

Dams and levees are built for flood protection. They usually are engineered to withstand a flood with a computed risk of occurrence. For example, a dam or levee may be designed to contain a flood at a location on a stream that has a certain probability of occurring in any one year. If a larger flood occurs, then that structure will be overtopped. If during the overtopping the dam or levee fails or is washed out, the water behind it is released to become a flash flood. Failed dams or levees can create floods that are catastrophic to life and property because of the tremendous energy of the released water. Warnings of the Teton Dam failure in Idaho in June 1976 reduced the loss of life to 11 people.

Debris, landslide, and mudflow floods

Debris or landslide floods are created by the accumulation of debris, mud, rocks, or logs in a channel, which form a temporary dam. Flooding occurs upstream as water becomes stored behind the temporary dam and then becomes a flash flood as the dam is breached and rapidly washes away. Landslides can create large waves on lakes or embayments and can be deadly. Mudflow floods can occur when volcanic activity rapidly melts mountain snow and glaciers, and the water mixed with mud and debris moves rapidly downslope. These mudflow events are also called lahars and, after the eruption of Mt. St. Helens in 1980, caused significant damage downstream along the Toutle and Cowlitz Rivers in southwest Washington.

U.S. Flash Flood/Flood Fatalities 1960-2001 [CONTINUED]

Year	AL	AZ	AR	CA	CO	CT	DE	FL	GA	ID	IL	IN	IA	KS	KY	LA	ME	MD	MA	MI	MN	MS	MO	MT	NE	NV	NH
1960				7							1			3	2			2	3
1961			4						1		1		5	5
1962				2	1		7						1		1			4
1963	1		1	3			1				1		1		2			2	1				1
1964				19				4	5						10	28							1	36		1
1965	2			8	22			5	2				4			58		1			12	1	5	2	1
1966				6					1				1			2									1
1967	7			4			3		1				1		3			1			1		1
1968	4			1					1		1		5			2		2	2	4			1
1969	1		2	58	1				2			4	1		3	3		4			6	132	2		1
1970	1	23	1	21								1			1						3	1
1971		1													1			16							1
1972	2	8		1				1			1		2		11			19	4		3	3
1973	2		4	5					1		1	11		4		3	3		3			19	12			1	8
1974		3	3	5			1	5			3		1	3	1	5					1	9	4	2		9
1975	2		3	1	1	2	2				1	2	1	2	7	2		1		1		31				3
1976	2	1		4	139				1	11				3
1977			1						39		1			6	8	1							26
1978	1	17	10	26							2	2			2	6		1			13				1
1979	15		2	1		1		5	3		4	4			6	4		1				4	3
1980	3	5		6	1			4							2						1	2			1
1981		8		8							1	3	2	3	2	2		1		1			1				1
1982	1	3	10	25	4	5		3	1		5		2	6	2	6						110				1
1983	1	15	2	7							2	2		6	1	6	2	1				5	1
1984		1	1	2											7	1							4	2	2	8
1985		1	2								6				4			1					4
1986				13							1		1					1	1	2	1		4	2		1
1987			4						4		1	2		1	2		1			1	2
1988	1	1		3				4				2				5
1989			4	1			3	1				2		2	3	3		7					1
1990	16	3	1	3					14		5	3	3		2					4	1	2	5		1	2
1991	1	1	1	1								3	3		3	3	1					2		1	1
1992		1		2				2	2			1		1	5	1							5			1
1993		3	2	17				2	2		1	1	3	2	2						2	130			4
1994				2					28		2	1		1								1	3
1995	1	2		7							1	2			2	6						1	2
1996	1			5	3					1	2	2		2	2		1	3		2			7	4			1
1997	1	23	1	13	9	2		2		1	1	1	1		161									6			3
1998	8	4	2	19				2	1		1	2		3	1	1	1				2		13			1	1
1999	2			1		1	2				1	5	1		1							2	4		1	1
2000		1		6	1						4	1	2		1						1		2
2001			6					1	1		1	2		1	2					3	3	1	3
2002
2003
2004
2005
2006
2007
2008
2009
2010
Totals	76	125	67	313	181	12	19	37	114	13	52	59	41	54	116	151	9	68	14	18	52	190	162	49	15	32	11

(Chart by GGS. Data compiled by Richard A. Wood, Ph.D.)

Year	NJ	NM	NY	NC	ND	OH	OK	OR	PA	RI	SC	SD	TN	TX	UT	VT	VA	WA	WV	WI	WY	AK	HI	PR	VI	Totals
1960	9		7	3				1	1					15		1			1	1				111		168
1961			1	1				2						36	6		1		22					8		93
1962	15		7	3			2							4			4		1			1				53
1963												2	4	4			2		12				3			41
1964				3		8		18			2			5				1					1			142
1965		3		1				1			9		6	28	7		1	2			1			6		188
1966		1			4									36									2	2		56
1967	1	7	3	1					3				3	10					3							53
1968	8					3							2	16										5		57
1969	1	2				30		1	2		2	3	2	12			153		4	2				10	1	445
1970								1	3					17		2								55	1	131
1971	3					2				17				23				1					2	1		68
1972	2	5	21	2				7	51			237	1	24			20	4	125					1		555
1973	9		2	16		1	10		7		3		11	27		5	3		3					4		178
1974	3	2		1	1		1	9	1				2	22									5	9		111
1975	6		6	4	5	2			4		1		5	13			2		3					41		127
1976		2	3	4	1		3		1		2		1	9		21		1						2		193
1977			6	11		1	5	78					11	5				4	1	2				4		210
1978		7	1			3	2		1					40			1		2	1			1	3		143
1979		3	5	6		1	3						2	28			8	2	1					9		121
1980			6			3	2	2	9				3	6	1				2	1			2			62
1981						2	4		4				3	36						1				1		84
1982		1				3	10	1	1		1	1	9	8				7				2		2		131
1983			4		1	1	4	2			3		5	19		1		5							1	97
1984		6	4	5			15		5		2		3	7		5			2					1		83
1985							8		3					16			19		38		12			52		166
1986		2	4			1	2		9		4		1	18	1	3	3	1	1	1				2		80
1987			11				3	1	1		1		3	17		1	3						3	9		71
1988		3												7										5		31
1989		2	4	6		4	1		1				12	17			6		4		1					85
1990		2		1		32	1		1		9		5	14		1		2	7					2		142
1991		4		1				1	1			1	2	16			3		3				7	3		61
1992	2		2	3		2	3							4			2									39
1993			8	2	1		5					5		6			1			1	1				1	103
1994	1		2			1	5		1				3	28					5	2			3			89
1995				9		5	2		1		3			26		1	5	1		1				1		79
1996	2	5	12	14	2	3	5	12	28		2			7	1	2	10		12					19		172
1997		2		3	2	5	2		4				5	23	1				6					1		135
1998			3			9	2	2			1		10	45	2		1		2	3				8		150
1999	6		2	22		2	2		6					2			2		1					4	1	72
2000			1		2	4	1				1			9			1		4	1						43
2001						3			1		1		1	31	1		1	1	5					3		72
2002
2003
2004
2005
2006
2007
2008
2009
2010
Totals	68	59	125	122	19	131	98	66	228	17	47	249	115	736	20	24	256	29	270	15	15	3	29	384	5	5180