Above Sea Level Barometer Reading,
Temperature Correction Calculator
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This calculator requires the use of JavaScript enabled and capable browsers.
This script determines the error in an observed barometer reading, based on elevation above (or below)
sea level of the barometer and the outside air temperature. ; the higher the elevation, the lower the
pressure. With the barometer at elevations above sea level, the correction should be added since it is
a negative value; below sea level, the value is also added but the value is positive. The default values
are typical for the general lower desert area of Southern California. If you wish to show below sea level
changes, just use a negative number for the appropriate elevation. To use the calculator, enter the
elevation of the barometer, the air temperature (OAT) and the known and observed barometer reading,
in any of the possible designations, then click on Calculate. Actual calculations are done on inches
of mercury, feet and degrees F. Results are yielded in both inches of mercury and millibars (mb). The
metric unit hPa (hectoPascal) is for all practical purposes, identical to the pressure unit designated
as millibars; in reality, there is a very small difference, but the scientific community accepts them
as the same. There is also an elevation correction chart, for a given temperature, below the calculator.
The standard value for atmospheric pressure at sea level (ATM) is equal to:
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| Correction For Elevation In Inches Hg Per 100 Foot Difference In Elevation |
To be added to barometer readings when above the datum plane or
subtracted from barometer readings when below the datum plane.
subtracted from barometer readings when below the datum plane.
| Altitude feet |
Temperature, in degrees Fahrenheit | |||||||||
| 0 | 10 | 20 | 30 | 40 | 50 | 60 | 70 | 80 | 90 | |
| 0 | .122 | .119 | .117 | .114 | .112 | .110 | .108 | .106 | .104 | .102 |
| 1000 | .118 | .115 | .113 | .110 | .108 | .106 | .104 | .102 | .100 | .098 |
| 2000 | .113 | .110 | .108 | .106 | .104 | .102 | .100 | .098 | .096 | .094 |
| 3000 | .108 | .106 | .104 | .102 | .100 | .098 | .096 | .094 | .092 | .090 |
| 4000 | .104 | .102 | .100 | .098 | .096 | .094 | .092 | .090 | .088 | .086 |
| 5000 | .100 | .098 | .096 | .094 | .092 | .090 | .088 | .086 | .084 | .082 |
| 6000 | .096 | .094 | .092 | .090 | .088 | .086 | .084 | .082 | .081 | .080 |
| 7000 | .093 | .091 | .089 | .087 | .085 | .084 | .082 | .080 | .079 | .078 |
Version 2.7.8
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