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The International Standard Atmosphere (ISA) is a model of the standard variation of pressure, temperature, density, and viscosity with altitude in the Earth's atmosphere. It is based on average conditions at mid latitudes, as determined by the International Civil Aviation Organization (ICAO). The atmosphere is divided into layers with assumed temperature distributions, and the other values are computed from basic physical constants and relationships. The use of water pressure - the Captain Cook Memorial Jet in Lake Burley Griffin, Canberra. ...
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In physics, density is defined as mass m per unit volume V. For the common case of a homogeneous substance, it is expressed as: where, in SI units: Ï (rho) is the density of the substance, measured in kg·m-3 m is the mass of the substance, measured in kg...
The related Category:Units of viscosity has been nominated for deletion, merging, or renaming. ...
Altitude is the elevation of an object from a known level or datum. ...
Layers of Atmosphere - not to scale (NOAA)[2] Earths atmosphere is a layer of gases surrounding the planet Earth and retained by the Earths gravity. ...
The International Civil Aviation Organization (ICAO), an agency of the United Nations, codifies the principles and techniques of international air navigation and fosters the planning and development of international air transport to ensure safe and orderly growth. ...
Various tabulations of the 1976 standard may be found on the web, e.g. at [1], or, of an earlier but similar standard, in publications such as Appendix 1 of Batchelor. The latter tabulation gives at sea level a pressure of 1.013 bar and a temperature of 15 C, and an initial lapse rate of 6.5 C/km. Above 12km the tabulated temperature is essentially constant. The tabulation continues to 18km where the pressure has fallen to 0.075 bar and the temperature to -56.5 C. The lapse rate is the rate at which an atmospheric variable (usually temperature) decreases with altitude. ...
Layers in the ISA
Standard Atmosphere 1976 | Layer | Level Name | Base Geopotential Height h (in km) | Base Geometric Height z (in km) | Lapse Rate (in °C/km) | Base Temperature T (in °C) | Base Atmospheric Pressure p (in kPa) | | 0 | Troposphere | 0.0 | 0.0 | -6.5 | +15.0 | 101,325 | | 1 | Tropopause | 11.000 | 11.019 | +0.0 | -56.5 | 22,632 | | 2 | Stratosphere | 20.000 | 20.063 | +1.0 | -56.5 | 5,474.9 | | 3 | Stratosphere | 32.000 | 32.162 | +2.8 | -44.5 | 868.02 | | 4 | Stratopause | 47.000 | 47.350 | +0.0 | -2.5 | 110.91 | | 5 | Mesosphere | 51.000 | 51.413 | -2.8 | -2.5 | 66.939 | | 6 | Mesosphere | 71.000 | 71.802 | -2.0 | -58.5 | 3.9564 | | 7 | Mesopause | 84.852 | 86.000 | — | -86.2 | 0.3734 | Atmosphere diagram showing the mesosphere and other layers. ...
The tropopause is a boundary region in the atmosphere between the troposphere and the stratosphere. ...
Atmosphere diagram showing stratosphere. ...
Atmosphere diagram showing stratosphere. ...
The stratopause is the level of the atmosphere which is the boundary between the stratosphere and the mesosphere. ...
The mesosphere (from the Greek words mesos = middle and sphaira = ball) is the layer of the Earths atmosphere that is directly above the stratosphere and directly below the thermosphere. ...
The mesosphere (from the Greek words mesos = middle and sphaira = ball) is the layer of the Earths atmosphere that is directly above the stratosphere and directly below the thermosphere. ...
The mesosphere (from the Greek words mesos = middle and sfaira = ball) is the layer of the Earths atmosphere that is directly above the stratosphere and directly below the thermosphere. ...
See also Atmospheric models are mathematical representations of the atmosphere, generally for the Earth. ...
The U.S. Standard Atmosphere is a series of models that define values for atmospheric temperature, density, pressure and other properties over a wide range of altitudes. ...
In chemistry and other sciences, STP or standard temperature and pressure is a standard set of conditions for experimental measurements, to enable comparisons to be made between sets of data. ...
References - Batchelor, G. K., An Introduction to Fluid Dynamics, Cambridge Univ. Press, 1967.
- Tabulation of 1976 standard at University of Sydney aeronautical mechanics site
- ICAO, Manual of the ICAO Standard Atmosphere (extended to 80 kilometres (262 500 feet)), Doc 7488-CD, Third Edition, 1993, ISBN 92-9194-004-6.
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