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Normalized Intensity Distribution

The rainfall intensity distribution given in equation 1:3.3.1 can be normalized to eliminate units. To do this, all time values are divided, or normalized, by the storm duration and all intensity values are normalized by the average storm intensity. For example,

i^=iiave\hat i =\frac{i}{i_{ave}}i^=iave​i​ 1:3.3.2

t^=TTdur\hat t=\frac{T}{T_{dur}}t^=Tdur​T​ 1:3.3.3

where i^\hat ii^ the normalized rainfall intensity at time t^\hat tt^, iii is the rainfall intensity at time T (mm/hr), iavei_{ave}iave​ is the average storm rainfall intensity (mm/hr),t^\hat tt^ is the time during the storm expressed as a fraction of the total storm duration (0.0-1.0), TTT is the time since the beginning of the storm (hr), and TdurT_{dur}Tdur​ is the duration of the storm (hr).

The normalized storm intensity distribution is:

1:3.3.4

,

where the normalized rainfall intensity at time , is the normalized maximum or peak rainfall intensity during the storm, is the time during the storm expressed as a fraction of the total storm duration (0.0-1.0), is the time from the beginning of the storm till the peak intensity expressed as a fraction of the total storm duration (0.0-1.0), and are equation coefficients.

The relationship between the original equation coefficients and the normalized equation coefficients is:

1:3.3.5

1:3.3.6

where is the equation coefficient for rainfall intensity before peak intensity is reached (hr), is the normalized equation coefficient for rainfall intensity before peak intensity is reached, is the equation coefficient for rainfall intensity after peak intensity is reached (hr), is the normalized equation coefficient for rainfall intensity after peak intensity is reached, and is the storm duration (hr).

Values for the equation coefficients, and , can be determined by isolating the coefficients in equation 1:3.3.4. At = 0.0 and at = 1.0,

1:3.3.7

1:3.3.8

where is the normalized equation coefficient for rainfall intensity before peak intensity is reached, is the normalized equation coefficient for rainfall intensity after peak intensity is reached, is the time during the storm expressed as a fraction of the total storm duration (0.0-1.0), is the time from the beginning of the storm till the peak intensity expressed as a fraction of the total storm duration (0.0-1.0), is the normalized rainfall intensity at time , and is the normalized maximum or peak rainfall intensity during the storm.

i^(t^)=i^mxβˆ—exp[t^βˆ’t^peakd1],i^mxβˆ—exp[t^peakβˆ’t^d2]\hat i(\hat t)={\hat i_{mx}*exp[\frac{\hat t - \hat t_{peak}}{d_1}] , \hat i_{mx}*exp[\frac{\hat t_{peak}-\hat t}{d_2}]}i^(t^)=i^mxβ€‹βˆ—exp[d1​t^βˆ’t^peak​​],i^mxβ€‹βˆ—exp[d2​t^peakβ€‹βˆ’t^​]
0≀t^≀t^peak0 \le \hat t \le \hat t_{peak}0≀t^≀t^peak​
t^peak<t^<1.0\hat t_{peak} < \hat t< 1.0t^peak​<t^<1.0
i^\hat ii^
t^\hat tt^
i^mx\hat i_{mx}i^mx​
t^\hat tt^
t^peak\hat t_{peak}t^peak​
d1d_1d1​
d2d_2d2​
Ξ΄1=d1βˆ—Tdur\delta_1=d_1*T_{dur}Ξ΄1​=d1β€‹βˆ—Tdur​
Ξ΄2=d2βˆ—Tdur\delta_2=d_2*T_{dur}Ξ΄2​=d2β€‹βˆ—Tdur​
Ξ΄1\delta_1Ξ΄1​
d1d_1d1​
Ξ΄2\delta_2Ξ΄2​
d2d_2d2​
TdurT_{dur}Tdur​
d1d_1d1​
d2d_2d2​
t^\hat tt^
t^\hat tt^
i^i^mxβ‰ˆ0.01\frac{\hat i}{\hat i_{mx}} \approx 0.01i^mx​i^β€‹β‰ˆ0.01
d1=t^βˆ’t^peakln(i^i^mx)=0βˆ’t^peakln(0.01)=t^peak4.605d_1=\frac{\hat t-\hat t_{peak}}{ln(\frac{\hat i}{\hat i_{mx}})}=\frac{0-\hat t_{peak}}{ln(0.01)}=\frac{\hat t_{peak}}{4.605}d1​=ln(i^mx​i^​)t^βˆ’t^peak​​=ln(0.01)0βˆ’t^peak​​=4.605t^peak​​
d2=t^peakβˆ’t^ln(i^i^mx)=t^peakβˆ’1ln(0.01)=1.0βˆ’t^peak4.605d_2=\frac{\hat t_{peak}-\hat t}{ln(\frac{\hat i}{\hat i_{mx}})}=\frac{\hat t_{peak}-1}{ln(0.01)}=\frac{1.0-\hat t_{peak}}{4.605}d2​=ln(i^mx​i^​)t^peakβ€‹βˆ’t^​=ln(0.01)t^peakβ€‹βˆ’1​=4.6051.0βˆ’t^peak​​
d1d_1d1​
d2d_2d2​
t^\hat t t^
t^peak\hat t_{peak}t^peak​
i^\hat ii^
t^\hat tt^
i^mx\hat i_{mx}i^mx​