Atmospheric Pressure as function of Salinity and Temperature Calculator

✖Salinity of Water is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity).ⓘ Salinity of Water [S]

+10%

-10%

✖Difference of Density Values represent mass per unit volume. High density indicates closely packed particles, while low density indicates more spaced particles.ⓘ Atmospheric Pressure as function of Salinity and Temperature [σ_t]

⎘ Copy

👎

Formula

✖

Atmospheric Pressure as function of Salinity and Temperature

Formula

`"σ"_{"t"} = 0.75*"S"`

Example

`"24.9975"=0.75*"33.33mg/L"`

Calculator

LaTeX

Reset

👍

Download Oceanography Formulas PDF

Atmospheric Pressure as function of Salinity and Temperature Solution

STEP 0: Pre-Calculation Summary

Formula Used

Difference of Density Values = 0.75*Salinity of Water
σ_t = 0.75*S
This formula uses 2 Variables

Variables Used

Difference of Density Values - Difference of Density Values represent mass per unit volume. High density indicates closely packed particles, while low density indicates more spaced particles.
Salinity of Water - (Measured in Milligram per Liter) - Salinity of Water is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity).

STEP 1: Convert Input(s) to Base Unit

Salinity of Water: 33.33 Milligram per Liter --> 33.33 Milligram per Liter No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

σ_t = 0.75*S --> 0.75*33.33

Evaluating ... ...

σ_t = 24.9975

STEP 3: Convert Result to Output's Unit

24.9975 --> No Conversion Required

FINAL ANSWER

24.9975 <-- Difference of Density Values

(Calculation completed in 00.004 seconds)

You are here -

Home » Engineering » Civil » Coastal and Ocean Engineering » Oceanography » Eckman Wind Drift » Atmospheric Pressure as function of Salinity and Temperature

Credits

Created by Mithila Muthamma PA

Coorg Institute of Technology (CIT), Coorg

Mithila Muthamma PA has created this Calculator and 2000+ more calculators!

Verified by M Naveen

National Institute of Technology (NIT), Warangal

M Naveen has verified this Calculator and 900+ more calculators!

< 15 Eckman Wind Drift Calculators

Velocity at Surface given Velocity Component along Horizontal x Axis

Go Velocity at the Surface = Velocity Component along a Horizontal x Axis/(e^(pi*Vertical Coordinate/Depth of Frictional Influence)*cos(45+(pi*Vertical Coordinate/Depth of Frictional Influence)))

Velocity Component along Horizontal x Axis

Go Velocity Component along a Horizontal x Axis = Velocity at the Surface*e^(pi*Vertical Coordinate/Depth of Frictional Influence)*cos(45+(pi*Vertical Coordinate/Depth of Frictional Influence))

Depth of Frictional Influence by Eckman

Go Depth of Frictional Influence by Eckman = pi*sqrt(Vertical Eddy Viscosity Coefficient/(Water Density*Angular Speed of the Earth*sin(Latitude of a Position on Earth Surface)))

Latitude given Depth of Frictional Influence by Eckman

Go Latitude of a Position on Earth Surface = asin(Vertical Eddy Viscosity Coefficient/(Water Density*Angular Speed of the Earth*(Depth of Frictional Influence by Eckman/pi)^2))

Vertical Eddy Viscosity Coefficient given Depth of Frictional Influence by Eckman

Go Vertical Eddy Viscosity Coefficient = (Depth of Frictional Influence by Eckman^2*Water Density*Angular Speed of the Earth*sin(Latitude of a Position on Earth Surface))/pi^2

Velocity in Current Profile in Three Dimensions by introducing Polar Coordinates

Go Velocity in the Current Profile = Velocity at the Surface*e^(pi*Vertical Coordinate/Depth of Frictional Influence)

Volume Flow Rates per unit of Ocean Width

Go Volume Flow Rates per unit of Ocean Width = (Velocity at the Surface*Depth of Frictional Influence)/(pi*sqrt(2))

Depth given Volume Flow rate per unit of Ocean Width

Go Depth of Frictional Influence = (Volume Flow Rates per unit of Ocean Width*pi*sqrt(2))/Velocity at the Surface

Velocity at Surface given Velocity detail of Current Profile in Three Dimensions

Go Velocity at the Surface = Current Profile Velocity/(e^(pi*Vertical Coordinate/Depth of Frictional Influence))

Vertical Coordinate from Ocean Surface given Angle between Wind and Current Direction

Go Vertical Coordinate = Depth of Frictional Influence*(Angle between the Wind and Current Direction-45)/pi

Depth given Angle between Wind and Current Direction

Go Depth of Frictional Influence = pi*Vertical Coordinate/(Angle between the Wind and Current Direction-45)

Angle between Wind and Current Direction

Go Angle between the Wind and Current Direction = 45+(pi*Vertical Coordinate/Depth of Frictional Influence)

Density given Atmospheric Pressure whose value of Thousand is reduced from Density Value

Go Density of Salt Water = Difference of Density Values+1000

Atmospheric Pressure as function of Salinity and Temperature

Go Difference of Density Values = 0.75*Salinity of Water

Salinity given Atmospheric Pressure

Go Salinity of Water = Difference of Density Values/0.75

Atmospheric Pressure as function of Salinity and Temperature Formula

Difference of Density Values = 0.75*Salinity of Water
σ_t = 0.75*S

What is Salinity?

Salinity is the saltiness or amount of salt dissolved in a body of water, called saline water. It is a strong contributor to conductivity and helps determine many aspects of the chemistry of natural waters and the biological processes within them. Salinity, along with temperature and pressure, helps govern physical characteristics of water such as density and heat capacity.

How does atmospheric pressure affect the ocean?

High air pressure exerts a force on the surroundings and results in water movement. So high air pressure over a sea area corresponds to low sea level and conversely low air pressure (a depression) results in higher sea levels. This is called the inverse barometer effect.

How to Calculate Atmospheric Pressure as function of Salinity and Temperature?

Atmospheric Pressure as function of Salinity and Temperature calculator uses Difference of Density Values = 0.75*Salinity of Water to calculate the Difference of Density Values, The Atmospheric Pressure as function of Salinity and Temperature is defined as pressure within atmosphere of Earth. Difference of Density Values is denoted by σ_t symbol.

How to calculate Atmospheric Pressure as function of Salinity and Temperature using this online calculator? To use this online calculator for Atmospheric Pressure as function of Salinity and Temperature, enter Salinity of Water (S) and hit the calculate button. Here is how the Atmospheric Pressure as function of Salinity and Temperature calculation can be explained with given input values -> 24.9975 = 0.75*0.03333.

FAQ

What is Atmospheric Pressure as function of Salinity and Temperature?

The Atmospheric Pressure as function of Salinity and Temperature is defined as pressure within atmosphere of Earth and is represented as σ_t = 0.75*S or Difference of Density Values = 0.75*Salinity of Water. Salinity of Water is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity).

How to calculate Atmospheric Pressure as function of Salinity and Temperature?

The Atmospheric Pressure as function of Salinity and Temperature is defined as pressure within atmosphere of Earth is calculated using Difference of Density Values = 0.75*Salinity of Water. To calculate Atmospheric Pressure as function of Salinity and Temperature, you need Salinity of Water (S). With our tool, you need to enter the respective value for Salinity of Water and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.

Home

FREE PDFs

🔍 Search