Modified form of epoch accounting for longitude and time meridian corrections Solution

STEP 0: Pre-Calculation Summary
Formula Used
Modified form of the Epoch = Phase Lag+Local and Greenwich Phase Arguments-(Wave Amplitude*Local Time Meridian/15)
κ' = k+pL-(a*LMT/15)
This formula uses 5 Variables
Variables Used
Modified form of the Epoch - Modified form of the Epoch that accounts for the longitude and Time Meridian Corrections.
Phase Lag - Phase Lag is called the local epoch in order to distinguish it from other forms of epochs.
Local and Greenwich Phase Arguments - Local and Greenwich Phase Arguments that account for both differences in location.
Wave Amplitude - (Measured in Meter) - Wave Amplitude is a measurement of the vertical distance of the wave from the average.
Local Time Meridian - (Measured in Second) - Local Time Meridian is a reference meridian used for a particular time zone and is similar to the Prime Meridian, which is used for Greenwich Mean Time.
STEP 1: Convert Input(s) to Base Unit
Phase Lag: 22 --> No Conversion Required
Local and Greenwich Phase Arguments: 11 --> No Conversion Required
Wave Amplitude: 1.56 Meter --> 1.56 Meter No Conversion Required
Local Time Meridian: 0.5 Hour --> 1800 Second (Check conversion ​here)
STEP 2: Evaluate Formula
Substituting Input Values in Formula
κ' = k+pL-(a*LMT/15) --> 22+11-(1.56*1800/15)
Evaluating ... ...
κ' = -154.2
STEP 3: Convert Result to Output's Unit
-154.2 --> No Conversion Required
FINAL ANSWER
-154.2 <-- Modified form of the Epoch
(Calculation completed in 00.004 seconds)

Credits

Creator Image
Created by Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 2000+ more calculators!
Verifier Image
Verified by M Naveen
National Institute of Technology (NIT), Warangal
M Naveen has verified this Calculator and 900+ more calculators!

13 Tide Producing Forces Calculators

Poisson Probability Law for Number of Storms simulated per year
​ Go Poisson Probability Law for the number of storms = (e^-(Mean Frequency of Observed Events*Number of Years)*(Mean Frequency of Observed Events*Number of Years)^Number of Storm Events)/(Number of Storm Events!)
Distance from center of Earth to center of Sun given Attractive Force Potentials
​ Go Distance = ((Mean Radius of the Earth^2*Universal Constant*Mass of the Sun*Harmonic Polynomial Expansion Terms for Sun)/Attractive Force Potentials for Sun)^(1/3)
Separation of distance between centers of mass of two bodies given gravitational forces
​ Go Distance between Two Masses = sqrt((([g])*Mass of Body A*Mass of Body B)/Gravitational Forces Between Particles)
Phase Lag given Modified Epoch that accounts for longitude and Time Meridian Corrections
​ Go Phase Lag = Modified form of the Epoch-Local and Greenwich Phase Arguments+(Wave Amplitude*Local Time Meridian/15)
Local Time Meridian given Modified Epoch for longitude and Time Meridian Corrections
​ Go Local Time Meridian = (Phase Lag-Modified form of the Epoch+Local and Greenwich Phase Arguments)*15/Wave Amplitude
Modified form of epoch accounting for longitude and time meridian corrections
​ Go Modified form of the Epoch = Phase Lag+Local and Greenwich Phase Arguments-(Wave Amplitude*Local Time Meridian/15)
Gravitational Forces on particles
​ Go Gravitational Forces Between Particles = [g]*(Mass of Body A*Mass of Body B/Distance between Two Masses^2)
Distance of point located on surface of Earth to center of Moon
​ Go Distance of point = (Mass of the Moon*Universal Constant)/Attractive Force Potentials for Moon
Distance of point located on surface of earth to center of sun
​ Go Distance of point = (Universal Constant*Mass of the Sun)/Attractive Force Potentials for Sun
Gravitational constant given radius of Earth and acceleration of gravity
​ Go Gravitational Constant = ([g]*Mean Radius of the Earth^2)/[Earth-M]
Local Time Meridian given Greenwich Time Measured
​ Go Local Time Meridian = 15*(Greenwich Time Measured-Local Time)
Local Time given Greenwich Time Measured
​ Go Local Time = Greenwich Time Measured-(Local Time Meridian/15)
Greenwich Time Measured
​ Go Greenwich Time Measured = Local Time+(Local Time Meridian/15)

Modified form of epoch accounting for longitude and time meridian corrections Formula

Modified form of the Epoch = Phase Lag+Local and Greenwich Phase Arguments-(Wave Amplitude*Local Time Meridian/15)
κ' = k+pL-(a*LMT/15)

What do you mean by Tidal Force?

The Tidal Force is a gravitational effect that stretches a body along the line towards the center of mass of another body due to a gradient (difference in strength) in gravitational field from the other body; it is responsible for diverse phenomena, including tides, tidal locking, breaking apart of celestial bodies.

How to Calculate Modified form of epoch accounting for longitude and time meridian corrections?

Modified form of epoch accounting for longitude and time meridian corrections calculator uses Modified form of the Epoch = Phase Lag+Local and Greenwich Phase Arguments-(Wave Amplitude*Local Time Meridian/15) to calculate the Modified form of the Epoch, The Modified form of epoch accounting for longitude and time meridian corrections are Some harmonic analyses that use a modified form of the epoch that automatically accounts for the longitude and time meridian corrections. This modification is designated as κ'. Modified form of the Epoch is denoted by κ' symbol.

How to calculate Modified form of epoch accounting for longitude and time meridian corrections using this online calculator? To use this online calculator for Modified form of epoch accounting for longitude and time meridian corrections, enter Phase Lag (k), Local and Greenwich Phase Arguments (pL), Wave Amplitude (a) & Local Time Meridian (LMT) and hit the calculate button. Here is how the Modified form of epoch accounting for longitude and time meridian corrections calculation can be explained with given input values -> 9 = 22+11-(1.56*1800/15).

FAQ

What is Modified form of epoch accounting for longitude and time meridian corrections?
The Modified form of epoch accounting for longitude and time meridian corrections are Some harmonic analyses that use a modified form of the epoch that automatically accounts for the longitude and time meridian corrections. This modification is designated as κ' and is represented as κ' = k+pL-(a*LMT/15) or Modified form of the Epoch = Phase Lag+Local and Greenwich Phase Arguments-(Wave Amplitude*Local Time Meridian/15). Phase Lag is called the local epoch in order to distinguish it from other forms of epochs, Local and Greenwich Phase Arguments that account for both differences in location, Wave Amplitude is a measurement of the vertical distance of the wave from the average & Local Time Meridian is a reference meridian used for a particular time zone and is similar to the Prime Meridian, which is used for Greenwich Mean Time.
How to calculate Modified form of epoch accounting for longitude and time meridian corrections?
The Modified form of epoch accounting for longitude and time meridian corrections are Some harmonic analyses that use a modified form of the epoch that automatically accounts for the longitude and time meridian corrections. This modification is designated as κ' is calculated using Modified form of the Epoch = Phase Lag+Local and Greenwich Phase Arguments-(Wave Amplitude*Local Time Meridian/15). To calculate Modified form of epoch accounting for longitude and time meridian corrections, you need Phase Lag (k), Local and Greenwich Phase Arguments (pL), Wave Amplitude (a) & Local Time Meridian (LMT). With our tool, you need to enter the respective value for Phase Lag, Local and Greenwich Phase Arguments, Wave Amplitude & Local Time Meridian and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
Let Others Know
Facebook
Twitter
Reddit
LinkedIn
Email
WhatsApp
Copied!