Drainage Manual - County of Santa Clara
Drainage Manual - County of Santa Clara
Drainage Manual - County of Santa Clara
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<strong>Drainage</strong> <strong>Manual</strong> 2007<br />
<strong>County</strong> <strong>of</strong> <strong>Santa</strong> <strong>Clara</strong>, California<br />
Flood Frequency – The frequency <strong>of</strong> flood and precipitation events are described in<br />
practice and in this manual using complementary terminology. “Exceedance frequency”<br />
refers to the probability <strong>of</strong> any individual precipitation or run<strong>of</strong>f event in any water year<br />
exceeding a certain threshold. Ten‐percent peak discharge is that flow rate with a ten<br />
percent chance <strong>of</strong> being equaled or exceeded during any water year. A “one percent, 6‐<br />
hour precipitation depth” is that 6‐hour depth <strong>of</strong> rainfall that has a one percent<br />
probability (chance) <strong>of</strong> being equaled or exceeded during any water year.<br />
An alternate terminology used in practice is the “recurrence interval,” which is also<br />
referred to as a “return period.” This terminology uses a number <strong>of</strong> years to specify a<br />
flood event. For example, a “ten‐year peak discharge” would be that discharge expected<br />
to be equaled or exceeded once every ten years on the average. The “100‐year, 6‐hour<br />
precipitation depth” is the 6‐hour depth <strong>of</strong> rainfall expected to be equaled or exceeded at<br />
a location once every 100 years on the average. Annual hydrologic events are considered<br />
to be independent <strong>of</strong> one another; so there is a finite probability <strong>of</strong> exceeding the 100‐<br />
year run<strong>of</strong>f in back‐to‐back water years. Experiencing a rainfall or run<strong>of</strong>f event <strong>of</strong> a<br />
certain magnitude does not lessen the chance (probability) <strong>of</strong> experiencing another event<br />
<strong>of</strong> equal or greater magnitude in subsequent years.<br />
These two frequency terminologies are related as the reciprocal <strong>of</strong> one another. The ten‐<br />
percent event (0.10 probability) is equivalent to the ten‐year event because the reciprocal<br />
<strong>of</strong> 0.10 is 10. Similarly the one‐percent event (0.01 probability) is the 100‐year event.<br />
Freeboard – The vertical distance between an elevation <strong>of</strong> interest (e.g. water surface,<br />
hydraulic grade line, or energy grade line) and the elevation <strong>of</strong> containment, such as the<br />
top <strong>of</strong> stream bank, street grade, or floodwall. Freeboard is intended to provide for a<br />
factor <strong>of</strong> safety in the design <strong>of</strong> stormwater storage and conveyance facilities.<br />
Frequency Interval – The frequency interval (or recurrence interval) <strong>of</strong> a peak flow is the<br />
number <strong>of</strong> years, on average, in which the specified flow is expected to be equaled or<br />
exceeded one time. Exceedance probability and frequency interval are mathematically<br />
inverse <strong>of</strong> each other; thus, an exceedance probability <strong>of</strong> 0.01 is equivalent to a frequency<br />
interval <strong>of</strong> 100 years. For example, a peak flow with a 100‐year frequency interval will,<br />
on average, be equaled or exceeded once every 100 years and has an exceedance<br />
probability <strong>of</strong> 0.01 (a 1‐percent chance <strong>of</strong> being exceeded in a given year). Frequency<br />
intervals refer to the average number <strong>of</strong> occurrences over a long period <strong>of</strong> time; for<br />
example, a 100‐year flood is statistically expected to occur about 10 times in a 1,000‐year<br />
period, rather than exactly once every 100 years. Additionally, it should be noted that<br />
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