========================================================================= National Space Science Data Center Data set MN-17A Nov 1989 ========================================================================= NAME: COSPAR International Reference Atmosphere 1986, 0 - 120 km SCIENTIFIC CONTACT: Sushil Chandra, Goddard Space Flight Center, code 616, Greenbelt, MD 20771 TECHNICAL CONTACT: Eric L. Fleming, Applied Research Corporation Landover, MD 20785 NSSDC CONTACT: D. Bilitza, GSFC/NSSDC code 632, Greenbelt, MD 20771, tel. (301) 286-0190 bilitza@gsfc.nasa.gov FILES: Parameter tables varying with height bytes (1) for January ch11.dat 5034 (2) for February ch12.dat 5034 .... .... (12) for December ch22.dat 5034 Parameter tables varying with pressure (13) for January cp11.dat 28998 (14) for February cp12.dat 28998 .... .... (24) for December cp22.dat 28998 (25) FORTRAN driver program, allows cirat.for 4953 fast display of CIRA values (26) this file aareadme.doc 4596 All data files are in VAX/VMS binary format. BRIEF DESCRIPTION: The COSPAR International Reference Atmosphere (CIRA) provides empirical models of atmospheric temperature and densities as recommended by the Committee on Space Research (COSPAR). Since the early sixties different editions of CIRA have been published. The CIRA Working Group meets bi- annual during the COSPAR General Assemblies. CIRA-86 is described in Advances in Space Research, Volume 8, Numbers 5-6, 1988. In the thermosphere (above about 100 km) CIRA-86 is identical with the MSIS model, which is also available from NSSDC (MI-91E). The lower part (0-120 km) of CIRA-86 consists of tables of the monthly mean values of temperature and zonal wind with almost global coverage (80N - 80S). Two sets of files were compiled by Fleming et al. (1988), one in pressure coordinates including also the geopotential heights, and one in height coordinates including also the pressure values. These tables were generated from several global data compilations including ground-based and satellite (Nimbus 5,6,7) measurements: Oort (1983), Labitzke et al. (1985). The lower part was merged with MSIS-86 at 120 km altitude. In general, hydrostatic and thermal wind balance are maintained at all levels. The model accurately reproduces most of the characteristic features of the atmosphere such as the equatorial wind and the general structure of the tropopause, stratopause, and mesopause. The driver program CIRAT developed at NSSDC allows fast and easy display of density, temperature and pressure for specified conditions. ----------------------------- REFERENCES -------------------------------- CIRA 1972, A.C. Strickland (ed.), Akademie Verlag, Berlin, G.D.R., 1972 CIRA 1986, D. Rees (ed.), Advances in Space Research, Volume 8, Number 5-6, 1988 A.H. Oort, Global Atmospheric Circulation Statistics 1958-1983, National Oceanic and Atmospheric Administration, Professional Paper 14, 180 pp, U.S. Government Printing Office, Washington, D.C., 1983 K. Labitzke, J.J. Barnett, and B. Edwards (eds.), Middle Atmosphere Program, MAP Handbook, Volume 16, University of Illinois, Urbana, 1985 K. Rawer, C.M. Minnis, K.S.W. Champion, and M. Roemer (eds.), Models of the Atmosphere and Ionosphere, Advances in Space Research, Volume 5, Number 7, 1985 K.U. Grossmann, K.S.W. Champion, M. Roemer, W.L. Oliver, and T.A. Blix (eds.), The Earth's Middle and Upper Atmosphere, Advances in Space Research, Volume 7, Number 10, 1987 E.L. Fleming, S. Chandra, M.R. Shoeberl, and J.J. Barnett, Monthly mean global climatology of temperature, wind, geopotential height and pressure for 0-120 km, National Aeronautics and Space Administration, Technical Memorandum 100697, Washington, D.C., 1988 ========================================================================= National Space Science Data Center Data set MN-17A Nov 1989 ==========================================================================