Analyses of Rainfall

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Analyses of Rainfall Hydrology and Water Resources RG744 Institute of Space Technology October 04, 2013

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Analyses of Rainfall. Hydrology and Water Resources RG744 Institute of Space Technology October 04, 2013 . Mean Rainfall. Mean Annual Rainfall: determined by averaging the total rainfall of several consecutive years at a place - PowerPoint PPT Presentation

Transcript of Analyses of Rainfall

Page 1: Analyses of Rainfall

Analyses of Rainfall

Hydrology and Water Resources RG744Institute of Space TechnologyOctober 04, 2013

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Mean Rainfall Mean Annual Rainfall: determined by averaging the total rainfall of several consecutive years at a place

Mean Monthly Rainfall: by averaging the monthly total rainfall for several consecutive years

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Interception and Net Precipitation

Vegetation influence on pattern of deposition and amount of precipitation reaching the soil surface

Interception losses are less in arid and semiarid regions that have sparse vegetation

Net precipitation is gross precipitation (measured by gauge) minus interception loss

Net precipitation is the amount available either to replenish soil water deficits or to become surface, subsurface, or ground water flow.

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Effective Rainfall Rainfall component causing perceptible change in the stream flow

That is only a portion of the total rainfall recorded over the catchment

Rainfall that does not infiltrate the soil and moves into the stream as overland flow

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Flood/Storm Frequency Flood frequency: number of times a particular flood/storm can be expected in a river/watershed in a given number of years

Example: 100 year flood – a flood that can be expected once in 100 years. (usually worked out by extrapolating the observed data)

Frequency is the percentage of years, during which a storm of a given magnitude may be equaled or exceeded

Recurrence interval/return period: Time interval after which a similar flood can be forecasted or expected.

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Frequency Analysis Objective: to develop a frequency curve Precipitation frequency curves can be developed to evaluate maximum events

Used for planning water resources structures Relationship between the magnitude of events and either the associated probability or the recurrence interval

Weather systems vary year to year and hence magnitude of future events can not be predicted accurately

Have to rely on statistical analyses of rainfall amounts over certain period

Frequency distribution of past events Probability or likelihood of having certain events occurring over a specified period is estimated

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Recurrence Interval of a Storm Number of years within which a given storm may equal or exceed once - Also known as return period

Means this precipitation value or more than that occurs m times in n years

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Probability of Exceedance

The probability of occurrence of a flood (having a recurrence interval T-year) in any year,

Probability: Reciprocal of the return periodp = 1/ T

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Frequency

Frequency: Probability expressed in terms of percentage

Frequency = p * 100

Frequency of a rainfall of a given magnitude = the number of times the given event may be expected to be equaled or exceeded in 100 years

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Example:

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The probability of having a 24 hr rainfall event of 100mm or more in any given year is about 0.02 (or a 50 year recurrence interval)

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Once the frequency curve is developed, the probability of exceeding certain rainfall amount over a specified period can be determined

The probability that an event with probability p will be equaled or exceeded x times in N years is determined by:

If x=0 (no occurrence in N years) thenProb (no occurrence in N years) = (1-p)N

Therefore; Prob (at least 1 occurrence in N years) = 1-(1-p)N

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Remaining slides will be covered in the next class.