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Standard atmosphere Andonova Alena MA-283 Standard atmosphere Andonova Alena MA-283

Aims Speak about Main characteristics of standard atmosphere Using standard atmosphere patterns in atmospheric Aims Speak about Main characteristics of standard atmosphere Using standard atmosphere patterns in atmospheric sciences Calculating some values of features for ISA http: //earthsciencelessonplans 101. blogspot. ru

Main characteristics of standard atmosphere The real atmosphere never remains constant at any particular Main characteristics of standard atmosphere The real atmosphere never remains constant at any particular time or place, a hypothetical model must be employed as an approximation to what may be expected. This model is known as a standard atmosphere. http: //quest. arc. nasa. gov

International Standard Atmosphere, Mean Sea Level Conditions (1952) Pressure p 0 = 101 325 International Standard Atmosphere, Mean Sea Level Conditions (1952) Pressure p 0 = 101 325 N/m 2 = 1013. 25 h. Pa Density ρ0 = 1. 225 kg/m 3 Temperature T 0 = 288. 15 K (15°C) Speed of sound a 0 = 340. 294 m/sec Acceleration of gravity g 0 = 9. 80665 m/sec 2

Pressure and Temperature variation in US Standard Atmosphere (1976) http: //atmos. caf. dlr. de Pressure and Temperature variation in US Standard Atmosphere (1976) http: //atmos. caf. dlr. de

There are some features: ISA Atmospheric temperature Atmospheric pressure Air density Speed of sound There are some features: ISA Atmospheric temperature Atmospheric pressure Air density Speed of sound Kinematic viscosity Thermal conductivity US SA Atmospheric temperature Absolute pressure Air density Acceleration of Gravity Dynamic viscosity For altitudes from -2000 to 30000 m For altitudes from -1000 to 80000 m

Calculating A vertical gradient of molecular temperature: Temperature is linear function of geopotential height: Calculating A vertical gradient of molecular temperature: Temperature is linear function of geopotential height: where μ 0 = 28. 9645 kg/kmol

Distribution of pressure was calculated by barometric formula for polytrophic and isothermal atmosphere: static Distribution of pressure was calculated by barometric formula for polytrophic and isothermal atmosphere: static equation compiles with and then: where

 In homogeneous atmosphere area gravity acceleration decreases with altitude: where a = 6371. In homogeneous atmosphere area gravity acceleration decreases with altitude: where a = 6371. 21 km and gradient are different in homogeneous atmosphere.

 Linear dependence Tμ of Ф: The formula for isothermal layer (γμ=0): Air density Linear dependence Tμ of Ф: The formula for isothermal layer (γμ=0): Air density is calculated by equation of state:

Conclusion § § § Standard Atmosphere pattern uses in atmospheric sciences for calculating, engineering Conclusion § § § Standard Atmosphere pattern uses in atmospheric sciences for calculating, engineering and other theoretical and practical problems. Online calculators for Standard Atmosphere: http: //www. digitaldutch. com/atmoscalc/ http: //pr. erau. edu/gallyt/stdatm. html http: //www. desktop. aero/stdatm. php

References L. T. Matveev, Fizika atmosfery, Hydrometizdat, 2000 M. Cavcar, The International Standard Atmosphere, References L. T. Matveev, Fizika atmosfery, Hydrometizdat, 2000 M. Cavcar, The International Standard Atmosphere, Anadolu University, 2005 http: //www. engineeringtoolbox. com/ http: //soliton. ae. gatech. edu