Magnitude of Horizontal Component of Coriolis Acceleration Calculator

✖Angular Speed of the Earth is the measure of how fast the central angle of a rotating body changes with respect to time.ⓘ Angular Speed of the Earth [Ω_E]			+10% -10%
✖Earth Station latitude is the coordinates of earth-station.ⓘ Earth Station Latitude [λ_e]			+10% -10%
✖Horizontal Speed across the Earth’s Surface is defined as the velocity of a motion problem deals with motion in the x direction.ⓘ Horizontal Speed across the Earth’s Surface [U]			+10% -10%

✖Horizontal Component of Coriolis Acceleration is defined as the acceleration due to the rotation of the earth, experienced by particles (water parcels, for example) moving along the earth's surface.ⓘ Magnitude of Horizontal Component of Coriolis Acceleration [a_C]

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Magnitude of Horizontal Component of Coriolis Acceleration Solution

STEP 0: Pre-Calculation Summary

Formula Used

Horizontal Component of Coriolis Acceleration = 2*Angular Speed of the Earth*sin(Earth Station Latitude)*Horizontal Speed across the Earth’s Surface
a_C = 2*Ω_E*sin(λ_e)*U
This formula uses 1 Functions, 4 Variables

Functions Used

sin - Sine is a trigonometric function that describes the ratio of the length of the opposite side of a right triangle to the length of the hypotenuse., sin(Angle)

Variables Used

Horizontal Component of Coriolis Acceleration - Horizontal Component of Coriolis Acceleration is defined as the acceleration due to the rotation of the earth, experienced by particles (water parcels, for example) moving along the earth's surface.
Angular Speed of the Earth - (Measured in Radian per Second) - Angular Speed of the Earth is the measure of how fast the central angle of a rotating body changes with respect to time.
Earth Station Latitude - (Measured in Radian) - Earth Station latitude is the coordinates of earth-station.
Horizontal Speed across the Earth’s Surface - (Measured in Meter per Second) - Horizontal Speed across the Earth’s Surface is defined as the velocity of a motion problem deals with motion in the x direction.

STEP 1: Convert Input(s) to Base Unit

Angular Speed of the Earth: 7.2921159E-05 Radian per Second --> 7.2921159E-05 Radian per Second No Conversion Required
Earth Station Latitude: 43.29 Degree --> 0.755553033188203 Radian (Check conversion here)
Horizontal Speed across the Earth’s Surface: 24.85 Mile per Second --> 39992.1984 Meter per Second (Check conversion here)

STEP 2: Evaluate Formula

Substituting Input Values in Formula

a_C = 2*Ω_E*sin(λ_e)*U --> 2*7.2921159E-05*sin(0.755553033188203)*39992.1984

Evaluating ... ...

a_C = 3.99933229239683

STEP 3: Convert Result to Output's Unit

3.99933229239683 --> No Conversion Required

FINAL ANSWER

3.99933229239683 ≈ 3.999332 <-- Horizontal Component of Coriolis Acceleration

(Calculation completed in 00.004 seconds)

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< Forces Driving Ocean Currents Calculators

Wind Speed at Height 10 m given Wind Stress

LaTeX Go Wind Speed at Height of 10 m = sqrt(Wind Stress/(Drag Coefficient*Density of Air))

Drag Coefficient given Wind Stress

LaTeX Go Drag Coefficient = Wind Stress/(Density of Air*Wind Speed at Height of 10 m^2)

Wind Stress

LaTeX Go Wind Stress = Drag Coefficient*Density of Air*Wind Speed at Height of 10 m^2

Drag Coefficient

LaTeX Go Drag Coefficient = 0.00075+(0.000067*Wind Speed at Height of 10 m)

Magnitude of Horizontal Component of Coriolis Acceleration Formula

LaTeX Go

Horizontal Component of Coriolis Acceleration = 2*Angular Speed of the Earth*sin(Earth Station Latitude)*Horizontal Speed across the Earth’s Surface
a_C = 2*Ω_E*sin(λ_e)*U

What is Wind Stress?

In Physical Oceanography and Fluid Dynamics, the wind stress is the shear stress exerted by the wind on the surface of large bodies of water – such as oceans, seas, estuaries and lakes. It is the force component parallel to the surface, per unit area, as applied by the wind on the water surface.

What does Coriolis mean?

Coriolis is an apparent force that as a result of the earth's rotation deflects moving objects (such as projectiles or air currents) to the right in the northern hemisphere and to the left in the southern hemisphere.

How to Calculate Magnitude of Horizontal Component of Coriolis Acceleration?

Magnitude of Horizontal Component of Coriolis Acceleration calculator uses Horizontal Component of Coriolis Acceleration = 2*Angular Speed of the Earth*sin(Earth Station Latitude)*Horizontal Speed across the Earth’s Surface to calculate the Horizontal Component of Coriolis Acceleration, The Magnitude of horizontal Component of Coriolis Acceleration formula is defined as the acceleration due to the rotation of the earth, experienced by particles (water parcels, for example) moving along the earth's surface. Horizontal Component of Coriolis Acceleration is denoted by a_C symbol.

How to calculate Magnitude of Horizontal Component of Coriolis Acceleration using this online calculator? To use this online calculator for Magnitude of Horizontal Component of Coriolis Acceleration, enter Angular Speed of the Earth (Ω_E), Earth Station Latitude (λ_e) & Horizontal Speed across the Earth’s Surface (U) and hit the calculate button. Here is how the Magnitude of Horizontal Component of Coriolis Acceleration calculation can be explained with given input values -> 3.999332 = 2*7.2921159E-05*sin(0.755553033188203)*39992.1984.

FAQ

What is Magnitude of Horizontal Component of Coriolis Acceleration?

The Magnitude of horizontal Component of Coriolis Acceleration formula is defined as the acceleration due to the rotation of the earth, experienced by particles (water parcels, for example) moving along the earth's surface and is represented as a_C = 2*Ω_E*sin(λ_e)*U or Horizontal Component of Coriolis Acceleration = 2*Angular Speed of the Earth*sin(Earth Station Latitude)*Horizontal Speed across the Earth’s Surface. Angular Speed of the Earth is the measure of how fast the central angle of a rotating body changes with respect to time, Earth Station latitude is the coordinates of earth-station & Horizontal Speed across the Earth’s Surface is defined as the velocity of a motion problem deals with motion in the x direction.

How to calculate Magnitude of Horizontal Component of Coriolis Acceleration?

The Magnitude of horizontal Component of Coriolis Acceleration formula is defined as the acceleration due to the rotation of the earth, experienced by particles (water parcels, for example) moving along the earth's surface is calculated using Horizontal Component of Coriolis Acceleration = 2*Angular Speed of the Earth*sin(Earth Station Latitude)*Horizontal Speed across the Earth’s Surface. To calculate Magnitude of Horizontal Component of Coriolis Acceleration, you need Angular Speed of the Earth (Ω_E), Earth Station Latitude (λ_e) & Horizontal Speed across the Earth’s Surface (U). With our tool, you need to enter the respective value for Angular Speed of the Earth, Earth Station Latitude & Horizontal Speed across the Earth’s Surface 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 Horizontal Component of Coriolis Acceleration?

In this formula, Horizontal Component of Coriolis Acceleration uses Angular Speed of the Earth, Earth Station Latitude & Horizontal Speed across the Earth’s Surface. We can use 1 other way(s) to calculate the same, which is/are as follows -

Horizontal Component of Coriolis Acceleration = Coriolis Frequency*Horizontal Speed across the Earth’s Surface

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