Probabilities Flashcards

1
Q

Exactly r times in n years

A

(n/r)p^r(1-p)^n-r

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2
Q

At least once in n years

A

1-(1-p)^n

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3
Q

Not occurring in n years

A

1-(1-(1-p)^n)

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4
Q

Trapezoidal Rule

A

Vi = ((Q1+Q2)/2)*(t2-t1)

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5
Q

H > UH

A

Write time and runoff flowrates (-baseflow)
Determine rainfall excess (-losses) (if different to uniform rain, use Phi-index to determine losses)
Scale q by rainfall excesses
Rainfall event procedure
Determine UH flowrates

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6
Q

UH > H

A

Write time and runoff flowrates
Set up table for rainfall events (r1UH, r2UH…)
Align rainfalls with starting time of events
Multiply UH by event rainfall starting with UH1, start multiplication where event starts!
Sum columns for UH
Multiply by net rain (-losses)
Add baseflow

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7
Q

To Produce S-curve

To Change an S-curve

A

[Time][UH][Lagged by D1 (x times until S values level out)][S curve (addition of UH to Laggedn columns)]

[Lagged S curve (by target D2)][Difference (Lag S - S)][UH D2 ((D1/D2)*diff)]

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8
Q

Superposition Procedure

A

For short to long D>nD n=integer

Lag identical UH by D1 x times (x=D2/D1 integer)
Sum columns for DRH runoffs
Divide DRH by x

[Time][UH][lagged UH][DRH][DRH/n]

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9
Q

UH Assumptions

A
Time invariant
Linear response
No baseflow
Total volume (depth) = 1 unit (usually 10mm)
Losses can be determined and seperated
Rainfall uniformly distributed
Rainfall intensity constant
Superposition applicable
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10
Q

SV Equation

A

dv/dt + v dv/dx + g dh/dx - g(So-Sf) = 0

LA CA PF GF FF

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11
Q

Kinematic Wave SV Component

A

g(So-Sf) = 0
GF FF
Steady Uniform

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12
Q

Diffusion Wave SV Component

A

g dh/dx - g(So-Sf) = 0

PF GF FF

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13
Q

Dynamic Wave SV Component

A

dv/dt + v dv/dx + g dh/dx - g(So-Sf) = 0
LA CA PF GF FF
Unsteady Non-Uniform

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14
Q

Steady Non-Uniform SV Component

A

v dv/dx + g dh/dx - g(So-Sf) = 0

CA PF GF FF

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15
Q

Hydrological Cycle

A

Evaporation, transpiration, precipitation, run off, ground water

P-R-ET=0

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16
Q

Absolute Humidity

A

The mass of the water vapour per

unit volume of the moist air, in kg/m 3

17
Q

Specific Humidity

A

The mass ratio between the water

vapour and the the moist air, in g/kg

18
Q

Relative Humidity (%)

A
h = e / es 
% = water vap p / sat water vap p
19
Q

Pyschometric Chart

A

(ew-e)=y(t-tw)