1993
DOI: 10.1002/j.1477-8696.1993.tb05867.x
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Atmospheric pressure, and temperature aloft

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Cited by 7 publications
(3 citation statements)
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“…We have used the same smartphone to collect the Wi-Fi, magnetic and barometer data. The hypsometric equation [55] is used to perform barometric floor identification as follows, h=((PoP)15.2571)×(T+273.15)0.0065. where P is the current atmospheric pressure, Po is the sea-level pressure which is 1013.25 hPa, h is the altitude, and T is the temperature. We have used T as 15 °C in Equation (12).…”
Section: Experiments and Resultsmentioning
confidence: 99%
“…We have used the same smartphone to collect the Wi-Fi, magnetic and barometer data. The hypsometric equation [55] is used to perform barometric floor identification as follows, h=((PoP)15.2571)×(T+273.15)0.0065. where P is the current atmospheric pressure, Po is the sea-level pressure which is 1013.25 hPa, h is the altitude, and T is the temperature. We have used T as 15 °C in Equation (12).…”
Section: Experiments and Resultsmentioning
confidence: 99%
“…Barometer, though it cannot be deployed as an individual sensor for localization, often proves to be very influential to determine the change in altitude for PDR localization. It measures the atmospheric pressure and uses the hypsometeric equation to measure the altitude [172]:…”
Section: Lux Meter and Barometermentioning
confidence: 99%
“…It is usually 'mobile', and much smaller than the warm high. Another variety of cold anticyclone forms over continents in winter where intense radiational cooling of the lowest layers leads to accumulation of extremely cold dense air near the surface ~ the exact reverse of the heat-low process described by Burton (1993). The winter-time Siberian high is the classic example of this latter type.…”
Section: What Is An Anticyclone?mentioning
confidence: 99%