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Last modified
7/14/2011 11:14:48 AM
Creation date
9/30/2006 10:21:51 PM
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Publications
Year
1998
Title
Layperson's Guide to Flood Management
CWCB Section
Watershed & Flood Protection
Author
California Water Education Foundation
Description
Layperson's Guide to Flood Management
Publications - Doc Type
Other
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<br />Flood Forecasting <br /> <br />Predicting the weather is an unsure science but <br />enhanced computers that analyze data have <br />improved the accuracy of short-term weather <br />forecasts, Long.term forecasts (30 to 90 days in <br />advance) usually are limited to general terms such <br />as "wetter than normal," as opposed to delineating <br />specific weather events. Long-term forecasts are <br />about 55 percent accurate. <br /> <br />Determining when to issue flood warnings is fraught <br />with uncertainty because of the unknowns inherent <br />in weather forecasting. As one DWR official noted: <br />"We have to be careful not to cry wolf too often or <br /> <br /> <br />At the .S'tate/Federal <br />Flood COf/trol Operations <br />Ce11fer in Sacramento, <br />hydrologists, Ivcather <br />forecasters llnd olhers <br />)vork together to <br />coordinate floodlights <br />lllld reservoir releases. <br /> <br />16 <br /> <br />we lose credibility, But at the same time, we don't <br />want to lose any lead time that could be used to <br />safely evacuate people," Part of the uncertainty <br />stems from the fact that there are only 100 years <br />of climate data upon which to base weather <br />predications. <br /> <br />Flood control managers, however, often are able to <br />predict with a high degree of accuracy when local <br />flooding is likely to take place, Their forecasts <br />combine storm runoff from unregulated tributaries <br />with reservoir releases to predict river levels. In <br />northern California, the joint state-federal forecast. <br />ing is done by the National Weather Service (NWS) <br />in cooperation with DWR's Division of Flood <br />Management at the California-Nevada River <br />Forecast Center in Sacramento. Federal and state <br />hydrologists can estimate high river stages within <br />12 to 24 hours before the event because of updates <br />on weather, precipitation amounts, and reservoir <br />and river levels. The information is distributed by <br />the State/Federal Flood Operations Center in <br />Sacramento, which cooperates with local flood <br />control and emergency services agencies. Two days <br /> <br />before the full force of the 1997 subtropical series <br />of storms was unleashed, forecasters predicted that <br />40 inches of rain would fall in the upper Feather River <br />watershed, which was within 1 inch of the actual <br />total downpour. <br /> <br />On large, slower-moving rivers such as the Sacra- <br />mento and San Joaquin, forecasters can predict high <br />river stages more than 48 hours in advance. This is <br />because releases from upstream dams can take <br />days to flow down the river to the Delta. In contrast, <br />on smaller, faster-moving rivers, such as the Eel and <br />Smith on the north coast of California, and most <br />southern California waterways, officials can produce <br />accurate flood warnings no more than 12 hours <br />ahead of time, <br /> <br />Weather patterns that worry climatologists and <br />flood managers are those arising from EI Nino and <br />La Nina weather conditions. EI Nino, known formally <br />as EI Nino-Southern Oscillation (ENSO), refers to <br />unusually warm currents along the coasts of Peru <br />and Ecuador, which heats other parts of the ocean <br />and atmosphere. This weather phenomenon can <br />increase tropical water temperatures in the eastern <br />Pacific by as much as 5 degrees Celsius and cause <br />heavier and more frequent storms, particularly in the <br />south coast regions and areas south of San <br />Francisco, In 1982-1983, which was an EI Nino <br />event, more than 26 inches of rain lei I and a record <br />37.7 million acre.feet flowed through the Sacramento <br />River system. However, most of the impact was along <br />the coastal regions because of high tides and waves. <br />There was $100 million in damage to coastal homes, <br />businesses and public recreation facilities. <br /> <br /> <br />La Nina, which is the inverse of EI Nino, causes <br />intense, wet warm storms. The January 1997 deluge, <br />along with the floods of 1955 and 1964 were a result <br />of La Nina, which is caused by the interaction of cold <br />surface ocean water near the equator and air. <br /> <br />Although weather patterns are discernible, the nature <br />of a given storm and the regional impacts are nearly <br />impossible to predict. As a precautionary measure, <br />legislation was enacted in 1997 that allocated $7,5 <br />million to better prepare California to cope with <br />potentially severe storms associated with the EI Nino <br />that battered parts of California in 1998, The funds <br />were for repairing and upgrading levees battered by <br />the New Year's floods, increasing staff to monitor <br />flood forecasts and reservoir operations and for <br />advanced deployment of personnel in the event of <br />flooding, During both the 1982-1983 and late 1997 <br />EI Niiio events, tropical fish were found swimming in <br />the waters off the Golden Gate, <br />
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