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This is in contrast to mean sea-level pressure, which involves the extrapolation of pressure to sea level for locations above or below sea level. The average pressure at mean sea level in the International Standard Atmosphere is 1,013.25 hPa, or 1 atmosphere (atm), or 29.92 inches of mercury.
A pressure of 6.3 kPa—the Armstrong limit—is about 1/16 of the standard sea-level atmospheric pressure of 101.3 kilopascals (760 mmHg). At higher altitudes water vapour from ebullism will add to the decompression bubbles of nitrogen gas and cause the body tissues to swell up, though the tissues and the skin are strong enough not to burst ...
Map of pressure systems across North America. A pressure system is a peak or lull in the sea level pressure distribution. The surface pressure at sea level varies minimally, with the lowest value measured 87 kilopascals (26 inHg) and the highest recorded 108.57 kilopascals (32.06 inHg).
Out of all these tropical cyclones, Typhoon Tip had the lowest atmospheric pressure measured in a tropical cyclone, at 870 mbar (25.69 inHg). It is the third image in the first row. This is a list of the most intense tropical cyclones as measured by minimum atmospheric pressure at sea level.
Orders of magnitude (pressure) on Wikipedia provides an overview of pressure measurements and their corresponding orders of magnitude.
Pressure as a function of the height above the sea level. The human body can perform best at sea level, [7] where the atmospheric pressure is 101,325 Pa or 1013.25 millibars (or 1 atm, by definition). The concentration of oxygen (O 2) in sea-level air is 20.9%, so the partial pressure of O 2 (pO 2) is 21.136 kilopascals (158.
On 26 January 1884, during the Ochtertyre storm the Ben Nevis summit weather station recorded a low pressure of 784.7 hPa (at high altitude (above 750 m) and not reduced to sea level) this is proposed as being almost certainly the lowest surface pressure ever recorded in the UK, [66] though due to altitude and not being a value reduced to sea ...
Thus the standard consists of a tabulation of values at various altitudes, plus some formulas by which those values were derived. To accommodate the lowest points on Earth, the model starts at a base geopotential altitude of 610 meters (2,000 ft) below sea level, with standard temperature set at 19 °C.