Title: Design storms
1Design storms
- Manuel Gómez Valentín
- Universitat Politècnica de Catalunya
- E.T.S. Ing. de Caminos, Canales y Puertos
2Rain data necessary for the study
- Information to level of hyetograph
- Minimal level of information a curve IDF/DDF
- In general, there is little suitable information
for direct use in studies of urban hydrology
3Level of usual information
- Information of rainfall in 24 hours
- Level of insufficient detail (problems in urban
areas in a few hours or even minutes) - Difficulty of disagregrating information
- To propose relationships between rains of
duration D and those of duration 24 hours - Problems due to that the information of rain in
24 hours can be a consequence of 2 or more rain
events
4How to obtain a curve IDF
- Available in some observatories
- Obtained from the analysis of a historical time
series of rain events (20/30 years) - If it is not available
- Options to establish synthetic IDF (Spanish
procedure in 5.2.IC regulation)
5Synthetic IDF
- Instruction 5.2. I.C.
- Use of the maximum rainfall in 24 hours for the
considered return period P24 - Regionalización of the rain from a certain
factor, variable according to the geographical
situation of the observatory
6Expression of the synthetic IDF
- Expression proposed (studies of the CEH)
- Relation between duration and average maximum
intensity
7 Maximum rainfall in 24 hours
- Information from the information provided in the
meteorological zonal centers - Utilization of a statistical extreme
distributions (Gumbel, SQRT-ET) - All of them give practically equal results for
low return periods
8 Regional factor
- Ratio between the maximum hourly average
intensity, and the daily average intensity
9Design storms
- 1.- Historical rains or time series of
- rains generated from statistical methods
- 2.- Design stor, obtained from
- information included in the shape of curve
- Intensity - Duration - Frequency.
10Rainfall patterns
- Defined the duration of rain, and known the
quantity of rainfall associated for the return
period T, it is necessary to to distribute the
temporarily above mentioned quantity of rain - To study guidelines of temporal distribution of
rainfall that repeat themselves in different rain
events - Huff's distribution
- Distribution of the Soil Conservation Service
11Huff's distribution
12Distribution of accumulated rainfall depending on
time that fits to the first quartil, and for
different probability values
Probability
13Rainfall patterns - Huff's temporal distribution
14S.C.S's distribution.
The IIIrd
Acumulated rainfall
The IInd
IA
I
Time (hours)
15Rainfall patterns of the SCS
16 Rainfall patterns summary
- Interesting approach, but with proper pattterns
extracted in the local observatory - Do not use patterns derived from different
observatories reflex of meteorological
situations that do not have anything to see with
our zone of study - Obtaining of local patterns from registers of
rain events of few years (5-8)
17 Design storms from IDF curves
- 2.1. constant Rain or in block
- 2.2. triangular Storm
- 2.3. storm type Sifalda
- 2.4. Double Triangle rainfall
- 2.5. Keifer-Chu rainfall
- 2.6. method of the Alternated Blocks
18 Constant rain or in Block
19 Triangular rain
20Sifalda rain type
21 Double triangle rainfall
I
P1 (10 years P.R.)
P2 (3 years P.R.)
30 mint
3 h.
D
4 h.
22Keifer-Chu type
f (ta) f (tb) for any Td, then
Also
Differing
Defining
Replacing
23Example Calculation with Keifer-Chu
r 0.50 Td 60 min c 4,477.44 e 1 f 19.031
24 Hietograma of the obtained rain
25Alternating blocks method
I5 '
I10 '
I15 '
26Calculation process
I5 ' I1
- Rain of the block 1
- I5 ' I1
- Rain of the block 2
- I10 x 10 ' I1 x 5 ' I2 x 5 '
- Rain of the block 3
- I15 x 15 ' I10 x 10 ' I3 x 5 ' I1 x 5 '
I2 x 5 ' I3 x 5 '
I2I10 x 10- I1 x 5
27Example Calculation with the Alternated Blocks
method
28 Hyetograph of Intensities
200
186.32
150
122.14
100
86.25
Intensity (mm/h)
64.15
49.58
39.47
50
32.16
26.72
22.54
19.28
16.67
14.56
0
1
2
3
4
5
6
7
8
9
10
11
12
Blocks of 5 minutes