Taylor and Schwartz Equation for Time Base Calculator

✖Modified Basin Lag for an effective duration rainfall.ⓘ Modified Basin Lag [t'_p]			+10% -10%
✖Non-standard rainfall duration to derive modified basin lag.ⓘ Non-standard rainfall duration [t_R]			+10% -10%

✖Time Base is the time from which the direct runoff begins until the direct-runoff.ⓘ Taylor and Schwartz Equation for Time Base [t_b]

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Taylor and Schwartz Equation for Time Base Solution

STEP 0: Pre-Calculation Summary

Formula Used

Time Base = 5*(Modified Basin Lag+Non-standard rainfall duration/2)
t_b = 5*(t'_p+t_R/2)
This formula uses 3 Variables

Variables Used

Time Base - (Measured in Second) - Time Base is the time from which the direct runoff begins until the direct-runoff.
Modified Basin Lag - (Measured in Second) - Modified Basin Lag for an effective duration rainfall.
Non-standard rainfall duration - (Measured in Second) - Non-standard rainfall duration to derive modified basin lag.

STEP 1: Convert Input(s) to Base Unit

Modified Basin Lag: 6.22 Hour --> 22392 Second (Check conversion here)
Non-standard rainfall duration: 2 Hour --> 7200 Second (Check conversion here)

STEP 2: Evaluate Formula

Substituting Input Values in Formula

t_b = 5*(t'_p+t_R/2) --> 5*(22392+7200/2)

Evaluating ... ...

t_b = 129960

STEP 3: Convert Result to Output's Unit

129960 Second -->36.1 Hour (Check conversion here)

FINAL ANSWER

36.1 Hour <-- Time Base

(Calculation completed in 00.004 seconds)

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< Synder's Synthetic Unit Hydrograph Calculators

Regional Constant given Peak Discharge for Nonstandard Effective Rainfall

LaTeX Go Regional Constant (Snyder) = Peak Discharge*Modified Basin Lag/(2.78*Area of Catchment)

Peak Discharge for Nonstandard Effective Rainfall

LaTeX Go Peak Discharge = 2.78*Regional Constant (Snyder)*Area of Catchment/Modified Basin Lag

Catchment Area given Peak Discharge for Nonstandard Effective Rainfall

LaTeX Go Area of Catchment = Peak Discharge*Modified Basin Lag/(2.78*Regional Constant)

Modified Basin Lag given Peak Discharge for Nonstandard Effective Rainfall

LaTeX Go Modified Basin Lag = 2.78*Regional Constant*Area of Catchment/Peak Discharge

Taylor and Schwartz Equation for Time Base Formula

LaTeX Go

Time Base = 5*(Modified Basin Lag+Non-standard rainfall duration/2)
t_b = 5*(t'_p+t_R/2)

What is Basin lag?

Basin lag time is defined as the elapsed time between the occurrences of the centroids of the effective rainfall. and of the storm runoff hydrograph, is an important factor in determining the time to peak of the unit. hydrograph and the intensity of peak discharge.

What is difference between Synthetic Unit Hydrograph & Unit Hydrograph?

A Synthetic Unit Hydrograph retains all the features of the unit hydrograph but does not require rainfall-runoff data. A synthetic unit hydrograph is derived from theory and experience, and its purpose is to simulate basin diffusion by estimating the basin lag based on a certain formula or procedure.
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 Taylor and Schwartz Equation for Time Base?

Taylor and Schwartz Equation for Time Base calculator uses Time Base = 5*(Modified Basin Lag+Non-standard rainfall duration/2) to calculate the Time Base, The Taylor and Schwartz Equation for Time Base formula is defined as the hydrograph is a crucial parameter in such studies, and its speedy and accurate determination is essential for both economic and hydrologic reasons. Time Base is denoted by t_b symbol.

How to calculate Taylor and Schwartz Equation for Time Base using this online calculator? To use this online calculator for Taylor and Schwartz Equation for Time Base, enter Modified Basin Lag (t'_p) & Non-standard rainfall duration (t_R) and hit the calculate button. Here is how the Taylor and Schwartz Equation for Time Base calculation can be explained with given input values -> 0.010028 = 5*(22392+7200/2).

FAQ

What is Taylor and Schwartz Equation for Time Base?

How to calculate Taylor and Schwartz Equation for Time Base?

The Taylor and Schwartz Equation for Time Base formula is defined as the hydrograph is a crucial parameter in such studies, and its speedy and accurate determination is essential for both economic and hydrologic reasons is calculated using Time Base = 5*(Modified Basin Lag+Non-standard rainfall duration/2). To calculate Taylor and Schwartz Equation for Time Base, you need Modified Basin Lag (t'_p) & Non-standard rainfall duration (t_R). With our tool, you need to enter the respective value for Modified Basin Lag & Non-standard rainfall duration 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 Time Base?

In this formula, Time Base uses Modified Basin Lag & Non-standard rainfall duration. We can use 1 other way(s) to calculate the same, which is/are as follows -

Time Base = (72+3*Modified Basin Lag)

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