atmoscira
Use COSPAR International Reference Atmosphere 1986 model
Syntax
Description
[
implements the mathematical representation of the Committee on Space Research (COSPAR)
International Reference Atmosphere (CIRA) 1986 model. The CIRA 1986 model provides a mean
climatology using a latitude, T
,pressureOrAltitude
,zonalWind
] = atmoscira(latitude
,ctype
,coord
)latitude
, and a representation of
coordinate type, ctype
. The mean climatology consists of temperature
T
, zonal wind zonalWind
, and pressure or
geopotential height pressureOrAltitude
. The provision encompasses
nearly pole-to-pole coverage (80 degrees S to 80 degrees N) for 0 km to 120 km. This
provision also encompasses the troposphere, middle atmosphere, and lower thermosphere. Use
this mathematical representation as a function of pressure or geopotential height.
This function uses a corrected version of the CIRA data files provided by J. Barnett in July 1990 in ASCII format.
[
uses a mean value type, T
,pressureOrAltitude
,zonalWind
]
= atmoscira(latitude
,ctype
,coord
,mtype
)mtype
, to implement these values.
[
uses a monthly mean value type, T
,pressureOrAltitude
,zonalWind
]
= atmoscira(latitude
,ctype
,coord
,mtype
,month
)month
, to implement these
values.
[
uses a mean value type, T
,pressureOrAltitude
,zonalWind
]
= atmoscira(latitude
,ctype
,coord
,month
)mtype
, and a monthly mean value type,
month
, to implement these values.
[
uses the argument T
,pressureOrAltitude
,zonalWind
]
= atmoscira(___,action
)action
to determine action reporting.
Examples
Input Arguments
Output Arguments
Limitations
This function has the limitations of the CIRA 1986 model and limits the values for the CIRA 1986 model.
The CIRA 1986 model that
atmoscira
implements limits values to latitudes of 80 degrees S to 80 degrees N on Earth and geopotential heights of 0 to 120 kilometers.atmoscira
clips output beyond these ranges.The CIRA 1986 model data also has missing data points.
In each monthly mean data set, the model omits values at 80 degrees S for 101,300 pascals or 0 meters because these levels are within the Antarctic land mass.
In the annual mean data set for latitudes 70, 75, and 80 degrees S, the model also omits these values:
101,300 and 78,895 pascal
0 and 2,500 meters
As a result of the missing data points, input for pressures above 61,441 pascal or geopotential heights below 5000 meters at these latitudes generate
NaN
output.For zonal mean pressure in constant altitude coordinates, pressure data is not available below 20 km. This value is the bottom level of the CIRA climatology.
When
atmoscira
detects an out-of-range input, the function uses theaction
argument to determine the function behavior.
References
[1] Fleming, E. L., S. Chandra, M. R. Shoeberl, and J. J. Barnett. Monthly Mean Global Climatology of Temperature, Wind, Geopotential Height and Pressure for 0-120 km. NASA TM100697, February 1988.