First Moment of ERH about Time Origin divided by Total Effective Rainfall Solution

STEP 0: Pre-Calculation Summary
Formula Used
First Moment of the ERH = First Moment of the DRH-(Constant n*Constant K)
MI1 = MQ1-(n*K)
This formula uses 4 Variables
Variables Used
First Moment of the ERH - First Moment of the ERH about the time origin divided by the total effective rainfall.
First Moment of the DRH - First Moment of the DRH about the time origin divided by the total direct runoff.
Constant n - Constant n is for the catchment to be determined by the effective rainfall of the catchment.
Constant K - Constant K is for the catchment to be determined by flood hydrograph characteristics of the catchment.
STEP 1: Convert Input(s) to Base Unit
First Moment of the DRH: 22 --> No Conversion Required
Constant n: 3 --> No Conversion Required
Constant K: 4 --> No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
MI1 = MQ1-(n*K) --> 22-(3*4)
Evaluating ... ...
MI1 = 10
STEP 3: Convert Result to Output's Unit
10 --> No Conversion Required
FINAL ANSWER
10 <-- First Moment of the ERH
(Calculation completed in 00.006 seconds)

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Determination of n and S of Nash's Model Calculators

Second Moment of ERH about Time Origin divided by Total Excess Rainfall
​ LaTeX ​ Go Second Moment of the ERH = Second Moment of the DRH-(Constant n*(Constant n+1)*Constant K^2)-(2*Constant n*Constant K*First Moment of the ERH)
Second Moment of DRH about Time Origin divided by Total Direct Runoff
​ LaTeX ​ Go Second Moment of the DRH = (Constant n*(Constant n+1)*Constant K^2)+(2*Constant n*Constant K*First Moment of the ERH)+Second Moment of the ERH
First Moment of ERH about Time Origin divided by Total Effective Rainfall
​ LaTeX ​ Go First Moment of the ERH = First Moment of the DRH-(Constant n*Constant K)
First Moment of DRH about Time Origin divided by Total Direct Runoff
​ LaTeX ​ Go First Moment of the DRH = (Constant n*Constant K)+First Moment of the ERH

First Moment of ERH about Time Origin divided by Total Effective Rainfall Formula

​LaTeX ​Go
First Moment of the ERH = First Moment of the DRH-(Constant n*Constant K)
MI1 = MQ1-(n*K)

What is Hyetograph and Hydrograph?

A Hyetograph is a plot of the intensity of rainfall against the time interval it is usually represented by a bar chart.
A Hydrograph is a graphical plot of the discharge of a natural system for river versus time.

What is the use of Unit Hydrograph?

A Unit Hydrograph shows the temporal change in flow, or discharge, per unit of runoff. In other words, how the flow of a stream will be affected over time by the addition of one unit of runoff. The unit hydrograph is a useful tool in the process of predicting the impact of precipitation on streamflow.

How to Calculate First Moment of ERH about Time Origin divided by Total Effective Rainfall?

First Moment of ERH about Time Origin divided by Total Effective Rainfall calculator uses First Moment of the ERH = First Moment of the DRH-(Constant n*Constant K) to calculate the First Moment of the ERH, The First Moment of ERH about Time Origin divided by Total Effective Rainfall formula is defined as the moment of effective rainfall hyetograph corresponding to the moment of Direct Runoff Hydrograph. First Moment of the ERH is denoted by MI1 symbol.

How to calculate First Moment of ERH about Time Origin divided by Total Effective Rainfall using this online calculator? To use this online calculator for First Moment of ERH about Time Origin divided by Total Effective Rainfall, enter First Moment of the DRH (MQ1), Constant n (n) & Constant K (K) and hit the calculate button. Here is how the First Moment of ERH about Time Origin divided by Total Effective Rainfall calculation can be explained with given input values -> 21.67 = 22-(3*4).

FAQ

What is First Moment of ERH about Time Origin divided by Total Effective Rainfall?
The First Moment of ERH about Time Origin divided by Total Effective Rainfall formula is defined as the moment of effective rainfall hyetograph corresponding to the moment of Direct Runoff Hydrograph and is represented as MI1 = MQ1-(n*K) or First Moment of the ERH = First Moment of the DRH-(Constant n*Constant K). First Moment of the DRH about the time origin divided by the total direct runoff, Constant n is for the catchment to be determined by the effective rainfall of the catchment & Constant K is for the catchment to be determined by flood hydrograph characteristics of the catchment.
How to calculate First Moment of ERH about Time Origin divided by Total Effective Rainfall?
The First Moment of ERH about Time Origin divided by Total Effective Rainfall formula is defined as the moment of effective rainfall hyetograph corresponding to the moment of Direct Runoff Hydrograph is calculated using First Moment of the ERH = First Moment of the DRH-(Constant n*Constant K). To calculate First Moment of ERH about Time Origin divided by Total Effective Rainfall, you need First Moment of the DRH (MQ1), Constant n (n) & Constant K (K). With our tool, you need to enter the respective value for First Moment of the DRH, Constant n & Constant K and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
How many ways are there to calculate First Moment of the ERH?
In this formula, First Moment of the ERH uses First Moment of the DRH, Constant n & Constant K. We can use 1 other way(s) to calculate the same, which is/are as follows -
  • First Moment of the ERH = (Second Moment of the DRH-Second Moment of the ERH-(Constant n*(Constant n+1)*Constant K^2))/(2*Constant n*Constant K)
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