Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar Solution

STEP 0: Pre-Calculation Summary
Formula Used
Tidal Period = Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Maximum Instantaneous Ebb Tide Discharge^3*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2))
T = EΔT*(3*pi*dOB^2*dNC^2)/(4*Qmax^3*(dNC^2-dOB^2))
This formula uses 1 Constants, 5 Variables
Constants Used
pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288
Variables Used
Tidal Period - (Measured in Second) - Tidal Period is the time it takes for a specific site on Earth to rotate from an exact point under moon to same point under moon, also known as “tidal day” and it’s slightly longer than a solar day.
Change in Mean Ebb Tide Flow Energy Flux - Change in Mean Ebb Tide Flow Energy Flux represents the alteration in the energy transferred by ebbing tidal currents over time.
Natural Depth of Ocean Bar - (Measured in Meter) - Natural Depth of Ocean Bar is the original depth of a sandbar or shoal in the ocean before any human intervention, such as dredging.
Depth of Navigation Channel - (Measured in Meter) - Depth of Navigation Channel is the depth of a passage in a stretch of water where the sea or riverbed has been deepened to allow access to large vessels.
Maximum Instantaneous Ebb Tide Discharge - (Measured in Cubic Meter per Second) - Maximum Instantaneous Ebb Tide Discharge per unit width is the tidal phase during which the water level falls & flood tidal phase during which the water level rises.
STEP 1: Convert Input(s) to Base Unit
Change in Mean Ebb Tide Flow Energy Flux: 161.64 --> No Conversion Required
Natural Depth of Ocean Bar: 2 Meter --> 2 Meter No Conversion Required
Depth of Navigation Channel: 4 Meter --> 4 Meter No Conversion Required
Maximum Instantaneous Ebb Tide Discharge: 2.5 Cubic Meter per Second --> 2.5 Cubic Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
T = EΔT*(3*pi*dOB^2*dNC^2)/(4*Qmax^3*(dNC^2-dOB^2)) --> 161.64*(3*pi*2^2*4^2)/(4*2.5^3*(4^2-2^2))
Evaluating ... ...
T = 129.998601350721
STEP 3: Convert Result to Output's Unit
129.998601350721 Second --> No Conversion Required
FINAL ANSWER
129.998601350721 129.9986 Second <-- Tidal Period
(Calculation completed in 00.020 seconds)

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14 Methods to Predict Channel Shoaling Calculators

Change of Ebb Tidal Energy Flux across Ocean Bar between Natural and Channel Conditions
​ Go Change in Mean Ebb Tide Flow Energy Flux = ((4*Tidal Period)/(3*pi))*Maximum Instantaneous Ebb Tide Discharge^3*((Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2)/(Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2))
Maximum Instantaneous Ebb Tide Discharge per Unit Width
​ Go Maximum Instantaneous Ebb Tide Discharge = (Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Tidal Period*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2)))^(1/3)
Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar
​ Go Tidal Period = Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Maximum Instantaneous Ebb Tide Discharge^3*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2))
Hoerls Special Function Distribution
​ Go Hoerls Special Function Distribution = Hoerls Best-fit Coefficient a*(Filling Index^Hoerls Best-fit Coefficient b)*e^(Hoerls Best-fit Coefficient c*Filling Index)
Density of Water given Water Surface Slope
​ Go Density of Water = (Coefficient Eckman*Shear Stress at the Water Surface)/(Water Surface Slope*[g]*Eckman Constant Depth)
Water Surface Slope
​ Go Water Surface Slope = (Coefficient Eckman*Shear Stress at the Water Surface)/(Density of Water*[g]*Eckman Constant Depth)
Shear Stress at Water Surface given Water Surface Slope
​ Go Shear Stress at the Water Surface = (Water Surface Slope*Density of Water*[g]*Eckman Constant Depth)/Coefficient Eckman
Coefficient given Water Surface Slope by Eckman
​ Go Coefficient Eckman = (Water Surface Slope*Density of Water*[g]*Eckman Constant Depth)/Shear Stress at the Water Surface
Ratio of Depth of Channel to Depth at which Seaward Slope of Ocean Bar Meets Sea Bottom
​ Go Depth Ratio = (Depth of Navigation Channel-Natural Depth of Ocean Bar)/(Water Depth between Sea Tip and Offshore Bottom-Natural Depth of Ocean Bar)
Water Depth where Seaward Tip of Ocean Bar meets Offshore Sea Bottom
​ Go Water Depth between Sea Tip and Offshore Bottom = ((Depth of Navigation Channel-Natural Depth of Ocean Bar)/Depth Ratio)+Natural Depth of Ocean Bar
Depth of Navigation Channel given Depth of Channel to depth at which Ocean Bar meets Sea Bottom
​ Go Depth of Navigation Channel = Depth Ratio*(Water Depth between Sea Tip and Offshore Bottom-Natural Depth of Ocean Bar)+Natural Depth of Ocean Bar
Transport Ratio
​ Go Transport Ratio = (Depth before Dredging/Depth after Dredging)^(5/2)
Depth before Dredging given Transport Ratio
​ Go Depth before Dredging = Depth after Dredging*Transport Ratio^(2/5)
Depth after Dredging given Transport Ratio
​ Go Depth after Dredging = Depth before Dredging/Transport Ratio^(2/5)

Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar Formula

Tidal Period = Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Maximum Instantaneous Ebb Tide Discharge^3*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2))
T = EΔT*(3*pi*dOB^2*dNC^2)/(4*Qmax^3*(dNC^2-dOB^2))

What is Ocean Dynamics?

The Ocean Dynamics define and describe the motion of water within the oceans. Ocean temperature and motion fields can be separated into three distinct layers: mixed (surface) layer, upper ocean (above the thermocline), and deep ocean. Ocean dynamics has traditionally been investigated by sampling from instruments in situ.

What is Dredging?

Dredging is the act of removing silt and other material from the bottom of bodies of water. It is a routine necessity in waterways around the world because sedimentation—the natural process of sand and silt washing downstream—gradually fills channels and harbors.

How to Calculate Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar?

Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar calculator uses Tidal Period = Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Maximum Instantaneous Ebb Tide Discharge^3*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2)) to calculate the Tidal Period, The Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar formula is defined as a parameter influencing the normalized, independent filling index as the Earth rotates through two tidal “bulges” every lunar day, coastal areas experience two high and two low tides every 24 hours and 50 minutes. Tidal Period is denoted by T symbol.

How to calculate Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar using this online calculator? To use this online calculator for Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar, enter Change in Mean Ebb Tide Flow Energy Flux (EΔT), Natural Depth of Ocean Bar (dOB), Depth of Navigation Channel (dNC) & Maximum Instantaneous Ebb Tide Discharge (Qmax) and hit the calculate button. Here is how the Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar calculation can be explained with given input values -> 9.650973 = 161.64*(3*pi*2^2*4^2)/(4*2.5^3*(4^2-2^2)).

FAQ

What is Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar?
The Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar formula is defined as a parameter influencing the normalized, independent filling index as the Earth rotates through two tidal “bulges” every lunar day, coastal areas experience two high and two low tides every 24 hours and 50 minutes and is represented as T = EΔT*(3*pi*dOB^2*dNC^2)/(4*Qmax^3*(dNC^2-dOB^2)) or Tidal Period = Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Maximum Instantaneous Ebb Tide Discharge^3*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2)). Change in Mean Ebb Tide Flow Energy Flux represents the alteration in the energy transferred by ebbing tidal currents over time, Natural Depth of Ocean Bar is the original depth of a sandbar or shoal in the ocean before any human intervention, such as dredging, Depth of Navigation Channel is the depth of a passage in a stretch of water where the sea or riverbed has been deepened to allow access to large vessels & Maximum Instantaneous Ebb Tide Discharge per unit width is the tidal phase during which the water level falls & flood tidal phase during which the water level rises.
How to calculate Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar?
The Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar formula is defined as a parameter influencing the normalized, independent filling index as the Earth rotates through two tidal “bulges” every lunar day, coastal areas experience two high and two low tides every 24 hours and 50 minutes is calculated using Tidal Period = Change in Mean Ebb Tide Flow Energy Flux*(3*pi*Natural Depth of Ocean Bar^2*Depth of Navigation Channel^2)/(4*Maximum Instantaneous Ebb Tide Discharge^3*(Depth of Navigation Channel^2-Natural Depth of Ocean Bar^2)). To calculate Tidal Period given Change of Ebb Tidal Energy Flux across Ocean Bar, you need Change in Mean Ebb Tide Flow Energy Flux (EΔT), Natural Depth of Ocean Bar (dOB), Depth of Navigation Channel (dNC) & Maximum Instantaneous Ebb Tide Discharge (Qmax). With our tool, you need to enter the respective value for Change in Mean Ebb Tide Flow Energy Flux, Natural Depth of Ocean Bar, Depth of Navigation Channel & Maximum Instantaneous Ebb Tide Discharge and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
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