Modelling Of Pressure-Altitude Equation Covering Up To 2km Above The Sea Level In Lagos, Southwestern Nigeria
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Date
2025-05-27
Journal Title
Journal ISSN
Volume Title
Publisher
IOSR
Abstract
It is generally known that the atmospheric pressure varies inversely as altitude globally. In the absence of real
time data, prediction of atmospheric pressure in the troposphere is based by the famous barometric equation
which depicts exponential inverse relationship between these two variables. This work employed two years
meteorological data of Lagos to study the relationship and model a localized equation. The research results show
that the atmosphere is purely linear with a gradient of -10.1 m/hPa from the sea level to about 2 km. The modeled
equation is useful for better prediction of atmospheric pressure for industrial, scientific and other purposes.
Description
It is generally known that the atmospheric pressure varies inversely as altitude globally. In the absence of real
time data, prediction of atmospheric pressure in the troposphere is based by the famous barometric equation
which depicts exponential inverse relationship between these two variables. This work employed two years
meteorological data of Lagos to study the relationship and model a localized equation. The research results show
that the atmosphere is purely linear with a gradient of -10.1 m/hPa from the sea level to about 2 km. The modeled
equation is useful for better prediction of atmospheric pressure for industrial, scientific and other purposes.
Keywords
Altitude, Pressure, Troposhere, Barometric equation
