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2007-11-01 Patrick Eriksson <patrick.eriksson@chalmers.se>

	* ARTS-XML-DATA-1-1-17

	* atmosphere/cira86/: Created files describing the CIRA86
	reference atmosphere. See README.FIRST.



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2007-11-01 Patrick Eriksson <patrick.eriksson@chalmers.se>
* ARTS-XML-DATA-1-1-17
* atmosphere/cira86/: Created files describing the CIRA86
reference atmosphere. See README.FIRST.
2007-10-24 Stefan Buehler <sbuehler(at)ltu.se>
* ARTS-XML-DATA-1-1-16
......
COSPAR International Reference Atmosphere (CIRA-86)
This directory contains 7 ascii files with the CIRA data in a
self-explanatory format:
nht.dat Zonally averaged monthly mean temperature as a function of
latitude and log-pressure scale height (resolution: 5 degrees
x 0.25 log-pressure scale heights) for the Northern Hemisphere
nhw.dat Zonally averaged monthly mean zonal wind as a function of
latitude and log-pressure scale height (resolution: 5 degrees
x 0.25 log-pressure scale heights) for the Northern Hemisphere
nhz.dat Zonally averaged monthly mean geopotential height as a function of
latitude and log-pressure scale height (resolution: 5 degrees
x 0.25 log-pressure scale heights) for the Northern Hemisphere
sht.dat Zonally averaged monthly mean temperature as a function of
latitude and log-pressure scale height (resolution: 5 degrees
x 0.25 log-pressure scale heights) for the Southern Hemisphere
shw.dat Zonally averaged monthly mean zonal wind as a function of
latitude and log-pressure scale height (resolution: 5 degrees
x 0.25 log-pressure scale heights) for the Southern Hemisphere
shz.dat Zonally averaged monthly mean geopotential height as a function of
latitude and log-pressure scale height (resolution: 5 degrees
x 0.25 log-pressure scale heights) for the Southern Hemisphere
twp.dat Zonally averaged monthly mean temperature, wind, and pressure
as a function of latitude and altitude (10 dregrees x 5 km)
for the entire globe
References:
Fleming, E.L., S. Chandra, J.J. Barnett, and M. Corney, Zonal mean
temperature, pressure, zonal wind, and geopotential height as
functions of latitude, COSPAR International Reference Atmosphere:
1986, Part II: Middle Atmosphere Models, Adv. Space Res., Vol. 10,
No. 12, pp. 11-59, 1990.
Fleming, E.L., S. Chandra, M.R. Schoeberl, and J.J. Barnett, Monthly
mean global climatology of temperature, wind, geopotential height, and
pressure for 0-120 km, NASA Tech. Memo. NASA TM-100697, 85 pp., 1988.
(reprints available from Eric Fleming fleming@kahuna.gsfc.nasa.gov)
------------------------------------------------------------------
SPARC Data Center August 31, 2000
Petra Udelhofen, e-mail: petra.udelhofen@sunysb.edu
This directory contains files describing the COSPAR International Reference
Atmosphere (CIRA-86)
The original CIRA-86 data are zonally averaged monthly mean
climatologies of several atmospheric parameters.
* Temperatures,
* zonal winds, and
* geopotential heights
are available on a grid with a resolution of 5 degrees in latitude and 0.25
in log-pressure scale height. In addition, data sets of
* temperatures,
* zonal winds, and
* pressures
are accessible on a grid with a resolution of 10 degrees latitude and 5 km
altitude.
Further information in the README file.
The files described in README were downloaded from the SPARC
data centre 2002-08-13 (www.sparc.sunysb.edu/html/fleming.html).
The files sht.dat and nht.dat have been used to create xml files
giving temperature and geometrical altitude as a function of pressure,
for different months. This was done by create_cira_xml.m, found in
this folder. The function modifies the data in some ways:
* Data for latitudes +-80 deg have been copied to +-90 deg, to
cover all possible latitudes.
* CIRA does not contain temperatures for some low altitudes above
Antarctica (no data available as always covered by ice). The
temperature for lowest OK altitude has been copied to all "empty"
positions".
* Altitudes have been calculated by *zt2p*, instead of using CIRA's
own altitudes as they are only approximative (and geopotential
instead of geometrical). A complete dry atmosphere, and that 1013
hPa equals 0 m, are assumed when calculating hydrostatic equilibrium
by *zt2p*.
Patrick Eriksson
2007-11-01
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