Floods of November 1996 through January 1997 in the Umpqua River Basin, Oregon |
U.S. Geological Survey Fact Sheet 2004-3134 |
Prepared in cooperation with the USDA Forest Service, the Bureau of Land Management, |
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During November 1996 through January 1997, a series of storms caused flooding throughout southeastern Oregon, northern California, and parts of Nevada. In Oregon's Umpqua River Basin (fig. 1), the most significant flooding occurred on November 18-19, December 4-9, and January 1-2. The combination of heavy rains, snowmelt, saturated soils, and flooding also resulted in debris flows and landslides. Four people were killed by a debris flow on November 18, 1996, near Rock Creek, a tributary to Hubbard Creek near Millwood. Over the 3-month period, flooding and land disturbances caused over $11 million in damage to public and private property within the Umpqua River drainage basin (Mikeal Jones, U.S. Forest Service, Umpqua National Forest, Roseburg, Oregon, written commun., 2004; Lowell Duell, U.S. Bureau of Land Management (BLM), Roseburg District, Roseburg, Oregon, written commun., 2004; Wayne Stinson, Douglas County, Sheriff's Office, Roseburg, Oregon, written commun., 2004). The Umpqua National Forest and Oregon State highways within Douglas County incurred over $4 million and $3 million in damage, respectively. Damage to BLM lands, local municipal infrastructure, and private property were each over $1 million.
November FloodsFlooding on November 18-19 was caused by heavy rains that fell on many locations throughout the Umpqua River Basin (table 1). The rains resulted from the convergence of a broad upper-air weather system of moist subtropical air, which originated over the tropical Pacific, and a cold-air mass over Washington (fig. 2). Roseburg received a record 4.35 inches of rainfall in a single day, which surpassed the previous record of 3.28 inches set in 1965. Prior to the storm, soil moisture and precipitation levels throughout the basin were already above average. October 1996 precipitation amounts at Drain, Roseburg, Riddle, and Toketee Falls were 178-215 percent of average. Most of the precipitation during the period of November 17-19 was rainfall. Air temperature and snowpack data collected at the King Mountain and Diamond Lake snow telemetry (SNOTEL) stations indicated that there was no significant snow accumulation. These stations, operated by the U.S. Department of Agriculture Natural Resources Conservation Service, are located at 4,000 and 5,200 feet elevation, respectively. Because the storm event occurred prior to the winter season and there was no preexisting snowpack at either of these two stations, snowmelt did not provide a significant contribution to the flooding. Although precipitation from the November 17-19 storm was broadly distributed over the entire Umpqua River Basin, flooding in the North Umpqua River Basin was more severe than flooding in the South Umpqua River Basin (table 2), possibly due to differing antecedent conditions. The recurrence interval for the November peak discharges within the entire basin ranged from less than 2 years to more than 50 years. A 50-year flood has a magnitude that would be expected to occur every 50 years, on average. Such a flood has a 2 percent chance of being equalled or exceed in any given year. The November flood for Boulder Creek near Toketee Falls (14316495) had an unusually high magnitude in comparison to the other basins. The event had a greater than 50-year recurrence and a unit discharge of 372 cubic feet per second per square mile. |
Table 1: Daily precipitation, in inches, for principal storms from November 1996 through January 1997 at selected locations, Umpqua River Basin, Oregon.
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Table 2. Peak discharge, peak stage, and recurrence intervals for November 1996-January 1997 floods at selected sites, Umpqua River Basin, Oregon.
[Abbreviation and symbol: no. number; fig., figure; mi2, square miles; ft3/s, cubic feet per second; flood events in red print are the annual peaks for water year 1997]
Map no. (fig. 1) | USGS station number | Station name | Drainage area (mi2) | Flood frequency period of record | November 1996 Flood | Map no. (fig. 1) | December 1996 Floods | Map no. (fig. 1) | January 1997 Floods | 100-year peak discharge (ft3/s) | Largest recorded historical flood peak | ||||||||||
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Date | Peak discharge (ft3/s) | Peak stage (ft) | Recurrence interval (years) | Date | Peak discharge (ft3/s) | Peak stage (ft) | Recurrence interval (years) | Date | Peak discharge (ft3/s) | Peak stage (ft) | Recurrence interval (years) | Date | Magnitude (ft3/s) | ||||||||
1 | 14308000 | South Umpqua River at Tiller | 449 | 1911, 1940-2002 | 111/18/1996 | 146,000 | 122.17 | 1>25 | 1 | 12/4/1996 | 27,500 | 17.2 | <5 | 1 | 1/1/1997 | 31,700 | 18.45 | <10 | 58,890 | 12/22/1964 | 60,200 |
2 | 14308500 | Elk Creek near Drew | 54.4 | 1955-1982; 1987-2002 | 11/18/1996 | 4,810 | 8.8 | <5 | 2 | 12/8/1996 | 5,000 | 9.02 | >5 | 2 | 11/1/1997 | 18,550 | 110.87 | 1<25 | 13,310 | 1/9/1995 | 9,120 |
3 | 14308685 | Days Creek above May Creek near Days Creek | 13 | 1985-2002 | 11/18/1996 | 1,610 | 3.79 | <25 | 3 | 112/8/1996 | 11,730 | 13.88 | 1<25 | 3 | 1/1/1997 | 691 | 2.84 | <5 | 3,118 | 12/8/1996 | 1,730 |
4 | 14308990 | Cow Creek above Galesville Reservoir near Azalea | 64.7 | 1986-2002 | 11/18/1996 | 3,010 | 7.81 | <5 | 4 | 12/8/1996 | 4,900 | 10.01 | <10 | 4 | 11/1/1997 | 16,130 | 111.25 | 1<25 | 10,070 | 1/9/1995 | 6,980 |
5 | 14309000 | Cow Creek near Azalea2 | 78 | 1928-1931, 1933-1985 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 5 | ( 3 ) | ( 3) | ( 3 ) | ( 3 ) | 5 | 11/2/1997 | 12,490 | 19.69 | 1<2 | 10,920 | 1/15/1974 | 10,600 |
6 | 14309220 | Cow Creek below McCollough Creek near Glendale4 | 195.1 | 1986-2002 | 11/18/1996 | 2,160 | 7.68 | <2 | 6 | 12/8/1996 | 7,560 | 14.56 | >10 | 6 | 11/1/1997 | 17,870 | 114.87 | 1>10 | 15,060 | 1/9/1995 | 7,970 |
7 | 14309500 | West Fork Cow Creek near Glendale | 86.9 | 1956-2002 | 111/18/1996 | 18,560 | 113.2 | 1<5 | 7 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 7 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 15,540 | 12/22/1964 | 15,700 |
8 | 14310000 | Cow Creek near Riddle | 456 | 1955-2002 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 8 | 112/8/1996 | 127,400 | 122.52 | 1>5 | 8 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 52,150 | 1/15/1974 | 38,400 |
9 | 14311200 | Olalla Creek near Tenmile5 | 61.3 | 1980-2002 | 11/18/1996 | 1,810 | 5.45 | <2 | 9 | 112/8/1996 | 16,780 | 19.24 | 1<25 | 9 | 1/1/1997 | 2,350 | 6.45 | >2 | 11,630 | 2/18/1983 | 6,970 |
10 | 14311500 | Lookingglass Creek at Brockway | 158 | 1956-2002 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 10 | 112/8/1996 | 111,300 | 115.72 | 1<5 | 10 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 35,370 | 12/26/1955 | 35,000 |
11 | 14312000 | South Umpqua River near Brockway | 1,670 | 1906-1912; 1924-1927; 1942-2002 | 11/19/1996 | 60,500 | 24.63 | <5 | 11 | 112/8/1996 | 176,300 | 128.46 | 1>5 | 11 | 1/1/1997 | 64,500 | 25.48 | <5 | 127,200 | 12/23/1964 | 125,000 |
12 | 14312170 | South Fork Deer Creek near Dixonville | 15.2 | 1990-2000 | 111/18/1996 | 11,720 | 16.84 | 1<10 | 12 | 12/8/1996 | 1,460 | 6.33 | >5 | 12 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 5,008 | 1/20/1996 | 1,910 |
13 | 14314500 | Clearwater River above Trap Creek near Toketee Falls6 | 41.6 | 1928-2002 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 13 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 13 | 11/1/1997 | 1968 | 16.92 | 1>100 | 824 | 12/23/1964 | 1,020 |
14 | 14316000 | Fish Creek at Big Fish Ranger Station near Toketee Falls7 | 68.8 | 1948-1955; 1957-2002 | 111/18/1996 | 16,390 | 110.66 | 1<25 | 14 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 14 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 10,350 | 12/22/1964 | 12,100 |
15 | 14316495 | Boulder Creek near Toketee Falls | 30.4 | 1987-1993; 1995-2002 | 111/18/1996 | 111,300 | 19.78 | 1>50 | 15 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 15 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 13,010 | 11/18/1996 | 11,300 |
16 | 14316500 | North Umpqua above Copeland Creek near Toketee Falls | 475 | 1950-2002 | 111/18/1996 | 117,200 | 114.56 | 1>10 | 16 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 16 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 34,380 | 12/22/1964 | 40,700 |
17 | 14316700 | Steamboat Creek near Glide | 227 | 1956-2002 | 111/18/1996 | 131,400 | 119.54 | 1<25 | 17 | 12/8/1996 | 14,700 | 11.78 | >2 | 17 | 1/1/1997 | 13,100 | 10.98 | <2 | 40,910 | 12/22/1964 | 51,000 |
18 | 14317600 | Rock Creek near Glide | 97.4 | 1957-1973; 1981-2002 | 111/18/1996 | 113,200 | 112.79 | 1>10 | 18 | 12/4/1996 | 7,130 | 9.74 | >2 | 18 | 1/31/1997 | 3,860 | 7.47 | <2 | 18,630 | 12/22/1964 | 22,800 |
19 | 14319500 | North Umpqua River at Winchester8 | 1,344 | 1909-1913; 1924-1929; 1954-2002 | 111/19/1996 | 190,000 | 127.6 | 1>10 | 19 | 12/8/1996 | 60,200 | 20.61 | <5 | 19 | 1/1/1997 | 50,500 | 18.1 | >2 | 129,400 | 12/22/1964 | 150,000 |
20 | 14319850 | Gassy Creek near Nonpareil | 9.19 | 1989-2000 | 111/18/1996 | 11,940 | 16.59 | 1<25 | 20 | 12/8/1996 | 656 | 4.4 | >2 | 20 | ( 3 ) | ( 3 ) | ( 3 ) | ( 3 ) | 3,032 | 11/18/1996 | 1,940 |
21 | 14320700 | Calapooya Creek near Oakland | 210 | 1956-1980; 1987-2001 | 111/18/1996 | 127,100 | 121.62 | 1>25 | 21 | 12/8/1996 | 12,400 | 18.42 | >2 | 21 | 1/1/1997 | 6,390 | 13.13 | <2 | 34,980 | 11/18/1996 | 27,100 |
22 | 14321000 | Umpqua River near Elkton | 3,683 | 1906; 1908-2002 | 11/19/1996 | 162,000 | 38.41 | <10 | 22 | 112/9/1996 | 1169,000 | 139.42 | 1>10 | 22 | 1/1/1997 | 127,000 | 33.14 | <5 | 254,300 | 12/23/1964 | 265,000 |
23 | 14321400 | Elk Creek near Elkhead | 28.7 | 1987-1999 | 111/18/1996 | 16,670 | 110.82 | 1<50 | 23 | 12/8/1996 | 2,420 | 7.79 | <5 | 23 | 1/1/1997 | 945 | 5.86 | <2 | 8,409 | 11/18/1996 | 6,670 |
24 | 14323085 | Smith River near Drain | 22.74 | 1981-1984; 1986-1989; 1992-2002 | 111/19/1996 | 11,750 | 110.67 | 1>5 | 24 | 12/4/1996 | 1,110 | 7.47 | >2 | 24 | 1/31/1997 | 995 | 6.89 | <2 | 2,987 | 12/6/1981 | 2,040 |
1 Flood events are the annual peaks for water year 1997. |
5 Site is partially affected by Ben Irving Reservoir regulation. |
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December FloodsMost of the December flooding occurred early in the month in response to a series of storms. Precipitation for December 8 at Roseburg, Riddle, and King Mountain was 3.53, 2.75, and 4.2 inches, respectively (table 1). Unlike the November 16-19 storm, the December storms resulted in some snow accumulation at higher elevations. Precipitation for the period of December 3-9 contributed to both snowpack and runoff. The December flooding was more severe in the South Umpqua River Basin than the November flooding, which was more severe in the North Umpqua River Basin. The recurrence interval for the December peak discharges within the entire basin ranged from more than 2 to less than 25 years (table 2). Most of the peak discharges occurred on December 8. |
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January FloodsAnother moist subtropical weather system brought steady rain starting around December 28 and continuing until January 2. Snowpack and air temperature data collected during this period at the King Mountain and Diamond Lake SNOTEL stations showed a net depletion of the preexisting snowpack. Most of the January peak discharges occurred on January 1 within the Umpqua River Basin. However, a separate storm later in the month caused January peak discharges to occur on January 31 in some tributary creeks in the lower section of the Umpqua River. The recurrence interval for the January peak discharges ranged from less than 2 to more than 100 years (table 2). The most severe flooding occurred in the upland reaches of the South Umpqua River Basin. Although the magnitudes of the November floods at some sites were greater than those of the January floods, the January floods caused more damage. After 3 months of above average precipitation throughout the Umpqua River Basin, soils had become saturated by January, and conditions were more conducive to landslides and road failures than they were earlier in the season. Damage to roads and bridges within the Umpqua National Forest caused by the January floods were roughly equivalent to damage caused by the November and December floods combined (Mikeal Jones, USDA Forest Service, written commun., 2004). |
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References CitedU.S. Interagency Advisory Committee on Water Data, 1982, Guidelines for determining flood flow frequency, Bulletin 17B of the Hydrology Subcommittee: Reston, Virginia, U.S. Geological Survey, Office of Water Data Coordination, 183 p. AcknowledgementsThis publication was produced in cooperation with the USDA Forest Service, Umpqua National Forest; Bureau of Land Management, Roseburg District; and the Oregon Water Resources Department, Douglas County Watermaster. Special thanks for assistance from Mikeal Jones, Umpqua National Forest, and Elaine Youngquist, Public Works Department, Douglas County, Oregon. For More Information:The U.S. Geological Survey has served the public and Federal, State, Tribal, and local governments since 1879 by collecting, analyzing, and publishing detailed information about the Nation's mineral, land, and water resources. For more information on water resources in Oregon: Public Information Specialist Selected data and interpretive reports are available from the USGS Oregon District Web site: http://or.water.usgs.gov/. |
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