Direction in Standard Meteorological Terms Solution

STEP 0: Pre-Calculation Summary
Formula Used
Direction in Standard Meteorological Terms = 270-Direction in Cartesian Coordinate system
θmet = 270-θvec
This formula uses 2 Variables
Variables Used
Direction in Standard Meteorological Terms - Direction in Standard Meteorological Terms is the parameters influencing the measured wind directions expressed in terms of azimuth angle from which winds come.
Direction in Cartesian Coordinate system - Direction in Cartesian Coordinate system with the zero angle wind blowing towards the east.
STEP 1: Convert Input(s) to Base Unit
Direction in Cartesian Coordinate system: 180 --> No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
θmet = 270-θvec --> 270-180
Evaluating ... ...
θmet = 90
STEP 3: Convert Result to Output's Unit
90 --> No Conversion Required
FINAL ANSWER
90 <-- Direction in Standard Meteorological Terms
(Calculation completed in 00.004 seconds)

Credits

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

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​ LaTeX ​ Go Direction in Standard Meteorological Terms = 270-Direction in Cartesian Coordinate system
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Direction in Standard Meteorological Terms Formula

​LaTeX ​Go
Direction in Standard Meteorological Terms = 270-Direction in Cartesian Coordinate system
θmet = 270-θvec

What is an Azimuth?

An Azimuth is an angular measurement in a spherical coordinate system. The vector from an observer to a point of interest is projected perpendicularly onto a reference plane; the angle between the projected vector and a reference vector on the reference plane is called the azimuth.

How to Calculate Direction in Standard Meteorological Terms?

Direction in Standard Meteorological Terms calculator uses Direction in Standard Meteorological Terms = 270-Direction in Cartesian Coordinate system to calculate the Direction in Standard Meteorological Terms, The Direction in Standard Meteorological Terms formula is defined as the parameters influencing the measured wind directions expressed in terms of the azimuth angle from which winds come. This convention is known as the meteorological coordinate system. Direction in Standard Meteorological Terms is denoted by θmet symbol.

How to calculate Direction in Standard Meteorological Terms using this online calculator? To use this online calculator for Direction in Standard Meteorological Terms, enter Direction in Cartesian Coordinate system vec) and hit the calculate button. Here is how the Direction in Standard Meteorological Terms calculation can be explained with given input values -> 90 = 270-180.

FAQ

What is Direction in Standard Meteorological Terms?
The Direction in Standard Meteorological Terms formula is defined as the parameters influencing the measured wind directions expressed in terms of the azimuth angle from which winds come. This convention is known as the meteorological coordinate system and is represented as θmet = 270-θvec or Direction in Standard Meteorological Terms = 270-Direction in Cartesian Coordinate system. Direction in Cartesian Coordinate system with the zero angle wind blowing towards the east.
How to calculate Direction in Standard Meteorological Terms?
The Direction in Standard Meteorological Terms formula is defined as the parameters influencing the measured wind directions expressed in terms of the azimuth angle from which winds come. This convention is known as the meteorological coordinate system is calculated using Direction in Standard Meteorological Terms = 270-Direction in Cartesian Coordinate system. To calculate Direction in Standard Meteorological Terms, you need Direction in Cartesian Coordinate system vec). With our tool, you need to enter the respective value for Direction in Cartesian Coordinate system 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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