Flood Risk Assessment: Flood Frequency Analysis Flashcards

(43 cards)

1
Q

What is a flood frequency curve?

A

A plot relating peak discharge to a measure of frequency.

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2
Q

What are the two key questions flood frequency estimation answers?

A
  1. How rare was that flood?
  2. How big a flood should infrastructure be designed for?
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3
Q

POT → __
AM (Annual Maxima) → __

A
  • Values over a threshold, more data
  • One peak per year, simpler
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4
Q

True/False
Annual maxima series includes all floods per year.

A

False (only the largest)

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5
Q

What is the hydrological year start month in the UK?

A

October

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6
Q

If record < 14 years and POT = AM length, use ____ to estimate Q.

A

POT

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7
Q

True/False
Annual maxima should be used if you have long records.

A

True

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8
Q

What are the two rules for independent POT events?

A
  1. Two indepedent peaks must be separated by at least 3× average time to rise
  2. The minimun flow between two peaks must be < 2/3 of the first peak
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9
Q

If average rise time is 15 hrs, peaks must be ≥ __ hrs apart to be independent.

A

45 hrs

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10
Q

Constructing the Flood Frequency Curve (n large)
Formula :
P(q > qd) ≈

A

1 − m/n
Where: m = cumulative frequency, n = total samples

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11
Q

CDF is obtained by dividing cumulative frequency by __.

A

sample size (n)

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12
Q

Formula
Return period: T =

A

1 / P(q > qd)

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13
Q

P(no flood in N years) =

A

(1 − 1/T)^N

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14
Q

P(flood at least once) =

A

1 − (1 − 1/T)^N

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15
Q

Formula
P(x floods in n years) =

A

nCx · p^x · (1 - p)^(n - x)
Where p = P(q > qd)

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16
Q

For POT sampling:
T = _____

A

(n / t) × 1 / (1 − F(qd))
Where: n = years, t = POT samples

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17
Q

What problems arise with small n?

A

Flat sections between points, P(q > qmax) = 0

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18
Q

Why not use P = m/N directly?

A

Leads to T = ∞ for largest value → physically meaningless

19
Q

True/False
Plotting positions give a continuous probability curve.

20
Q

What is a limitation of plotting positions?

A
  • Give discrete estimates not continuous frequency curve
  • Cannot extrapolate beyond observed max value
21
Q

What distribution is fitted for flood frequency extrapolation?

A

The Gumbel distribution (Extreme Value Type I)

22
Q

To estimate floods with return periods longer than your record, you must ______ data.

23
Q

What are possible distributions for extrapolation?

A

Log-normal, Beta, Gamma

24
Q

What distribution is typically used for extreme floods?

25
Transformation Gumbel variate:
z = -ln( -ln[ F(qₐ) ] ) ⇒ qₐ = bz + a
26
What is the Gumbel variate z used for?
It linearises the distribution for regression
27
List the 4 Gumbel parameter estimation methods.
Linear regression, Moment matching, L-moment matching, Maximum likelihood
28
True/False Hydrologists typically prefer maximum likelihood methods.
False (they prefer L-moments)
29
What plotting position formula is used to estimate F(qd)?
Gringorten formula
30
Formula Sample mean:
µ = (1 / N) × Σ qₐ
31
Formula Sample variance:
s² = (1 / (N - 1)) × Σ (qₐ - µ)²
32
Why is the L-moment method more robust?
It reduces sensitivity to outliers by avoiding squaring deviations.
33
True/False Outliers can significantly bias Gumbel parameters.
True
34
List 3 checks to ensure data quality before fitting a distribution.
- Inspect time series for errors - Remove serial dependence - Plot fitted CDF and remove outliers
35
What two methods should be used to estimate Gumbel parameters>
Method of moments and L-moments
36
What two approaches help when flow data is scarce?
1. Use regional flood frequency analysis 2. Generate synthetic flow using hydrological models
37
Regional Flood Frequency Analysis RSMD → S1085 → LAKE →
- wetness index - channel slope - % of catchment routed through lake/reservoir
38
What is the "index flood" in regional analysis?
The median or mean peak flow, used to scale the growth curve.
39
SAAR → FARL → BFIHOST →
- average annual rainfall - fraction of area through lakes/reservoirs - baseflow index
40
Rainfall frequency is summarised using ______ curves.
Depth-Duration-Frequency (DDF)
41
What two factors define a rainfall event's rarity?
Depth and duration
42
What approach is used when no reliable flow data exist?
Use of historical maximum flood or regional/global datasets
43
Why might L-moment estimates be preferred?
More robust to outliers and better suited for skewed data