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## Credits

Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 1000+ more calculators!
NSS College of Engineering (NSSCE), Palakkad
Chandana P Dev has verified this Calculator and 1000+ more calculators!

## Average Velocity in Channel for flow through Inlet into the Bay Solution

STEP 0: Pre-Calculation Summary
Formula Used
average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length
V = (Ab*dhb/dt)/Aavg
This formula uses 3 Variables
Variables Used
Surface Area of Bay - Surface Area of Bay is defined as a small body of water set off from the main body. (Measured in Square Meter)
Change of Bay Elevation with Time- Change of Bay Elevation with Time
Average Area over the Channel Length - Average Area over the Channel Length (Measured in Square Meter)
STEP 1: Convert Input(s) to Base Unit
Surface Area of Bay: 20 Square Meter --> 20 Square Meter No Conversion Required
Change of Bay Elevation with Time: 10 --> No Conversion Required
Average Area over the Channel Length: 50 Square Meter --> 50 Square Meter No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
V = (Ab*dhb/dt)/Aavg --> (20*10)/50
Evaluating ... ...
V = 4
STEP 3: Convert Result to Output's Unit
4 Meter per Second --> No Conversion Required
4 Meter per Second <-- Average Velocity in Channel for flow
(Calculation completed in 00.016 seconds)

## < 10+ Inlet Currents and Tidal Elevations Calculators

Ocean Tide Amplitude for known King’s dimensionless velocity
ocean_tide_amplitude = (Average Area over the Channel Length*Maximum Cross-sectionally Averaged Velocity*Tidal Period)/ (King’s Dimensionless Velocity*2*pi*Surface Area of Bay) Go
Average Area over a Channel Length for known King’s Dimensionless Velocity
average_area_over_the_channel_length = (King’s Dimensionless Velocity*2*pi*Ocean Tide Amplitude*Surface Area of Bay)/Tidal Period*Maximum Cross-sectionally Averaged Velocity Go
Surface Area of Bay for known King’s dimensionless Velocity
surface_area_of_bay = (Average Area over the Channel Length*Tidal Period*Maximum Cross-sectionally Averaged Velocity)/King’s Dimensionless Velocity*2*pi*Ocean Tide Amplitude Go
Tidal Period for known King’s Dimensionless Velocity
tidal_period = (2*pi*Ocean Tide Amplitude*Surface Area of Bay*King’s Dimensionless Velocity)/Average Area over the Channel Length*Maximum Cross-sectionally Averaged Velocity Go
Maximum Cross-Sectionally averaged Velocity during a Tidal Cycle
max_avg_velocity_tidal = (King’s Dimensionless Velocity*2*pi*Ocean Tide Amplitude*Surface Area of Bay)/Average Area over the Channel Length*Tidal Period Go
Inlet Length when Tidal Period is given
inlet_length = ([g]*Average Area over the Channel Length*(King’s Inlet Friction Coefficient*Tidal Period/2*pi)^2)/Surface Area of Bay Go
Average Area Over the Channel Length for flow through the Inlet into the Bay
average_area_over_the_channel_length = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Velocity in Channel for flow Go
Change of Bay Elevation with time for flow through the Inlet into the Bay
change_of_bay_elevation_with_time = (Average Area over the Channel Length*Average Velocity in Channel for flow)/Surface Area of Bay Go
Surface Area of Bay for flow through the Inlet into the Bay
surface_area_of_bay = (Average Velocity in Channel for flow*Average Area over the Channel Length)/Change of Bay Elevation with Time Go
Average Velocity in Channel for flow through Inlet into the Bay
average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length Go

### Average Velocity in Channel for flow through Inlet into the Bay Formula

average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length
V = (Ab*dhb/dt)/Aavg

## What is Seiches?

Seiches are standing waves or oscillations of the free surface of a body of water in a closed or semiclosed basin. These oscillations are of relatively long period, extending from minutes in harbors and bays to over 10 hr in the Great Lakes. Any external perturbation to the lake or embayment can force an oscillation. In harbors, the forcing can be the result of short waves and wave groups at the harbor entrance. Examples include 30- to 400-sec wave-forced oscillations in the Los Angeles-Long Beach harbor (Seabergh 1985).

## How to Calculate Average Velocity in Channel for flow through Inlet into the Bay?

Average Velocity in Channel for flow through Inlet into the Bay calculator uses average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length to calculate the Average Velocity in Channel for flow, The Average Velocity in Channel for flow through Inlet into the Bay is defined as The time average of the velocity of a fluid at a fixed point, over a somewhat arbitrary time interval T counted from some fixed time. Average Velocity in Channel for flow and is denoted by V symbol.

How to calculate Average Velocity in Channel for flow through Inlet into the Bay using this online calculator? To use this online calculator for Average Velocity in Channel for flow through Inlet into the Bay, enter Surface Area of Bay (Ab), Change of Bay Elevation with Time (dhb/dt) and Average Area over the Channel Length (Aavg) and hit the calculate button. Here is how the Average Velocity in Channel for flow through Inlet into the Bay calculation can be explained with given input values -> 4 = (20*10)/50.

### FAQ

What is Average Velocity in Channel for flow through Inlet into the Bay?
The Average Velocity in Channel for flow through Inlet into the Bay is defined as The time average of the velocity of a fluid at a fixed point, over a somewhat arbitrary time interval T counted from some fixed time and is represented as V = (Ab*dhb/dt)/Aavg or average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length. Surface Area of Bay is defined as a small body of water set off from the main body, Change of Bay Elevation with Time and Average Area over the Channel Length.
How to calculate Average Velocity in Channel for flow through Inlet into the Bay?
The Average Velocity in Channel for flow through Inlet into the Bay is defined as The time average of the velocity of a fluid at a fixed point, over a somewhat arbitrary time interval T counted from some fixed time is calculated using average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length. To calculate Average Velocity in Channel for flow through Inlet into the Bay, you need Surface Area of Bay (Ab), Change of Bay Elevation with Time (dhb/dt) and Average Area over the Channel Length (Aavg). With our tool, you need to enter the respective value for Surface Area of Bay, Change of Bay Elevation with Time and Average Area over the Channel Length 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 Average Velocity in Channel for flow?
In this formula, Average Velocity in Channel for flow uses Surface Area of Bay, Change of Bay Elevation with Time and Average Area over the Channel Length. We can use 10 other way(s) to calculate the same, which is/are as follows -
• average_velocity_channel = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Area over the Channel Length
• average_area_over_the_channel_length = (Surface Area of Bay*Change of Bay Elevation with Time)/Average Velocity in Channel for flow
• surface_area_of_bay = (Average Velocity in Channel for flow*Average Area over the Channel Length)/Change of Bay Elevation with Time
• change_of_bay_elevation_with_time = (Average Area over the Channel Length*Average Velocity in Channel for flow)/Surface Area of Bay
• average_area_over_the_channel_length = (King’s Dimensionless Velocity*2*pi*Ocean Tide Amplitude*Surface Area of Bay)/Tidal Period*Maximum Cross-sectionally Averaged Velocity
• tidal_period = (2*pi*Ocean Tide Amplitude*Surface Area of Bay*King’s Dimensionless Velocity)/Average Area over the Channel Length*Maximum Cross-sectionally Averaged Velocity
• max_avg_velocity_tidal = (King’s Dimensionless Velocity*2*pi*Ocean Tide Amplitude*Surface Area of Bay)/Average Area over the Channel Length*Tidal Period
• ocean_tide_amplitude = (Average Area over the Channel Length*Maximum Cross-sectionally Averaged Velocity*Tidal Period)/ (King’s Dimensionless Velocity*2*pi*Surface Area of Bay)
• surface_area_of_bay = (Average Area over the Channel Length*Tidal Period*Maximum Cross-sectionally Averaged Velocity)/King’s Dimensionless Velocity*2*pi*Ocean Tide Amplitude
• inlet_length = ([g]*Average Area over the Channel Length*(King’s Inlet Friction Coefficient*Tidal Period/2*pi)^2)/Surface Area of Bay
Where is the Average Velocity in Channel for flow through Inlet into the Bay calculator used?
Among many, Average Velocity in Channel for flow through Inlet into the Bay calculator is widely used in real life applications like {FormulaUses}. Here are few more real life examples -
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