2009-11-03 Patrick Eriksson <patrick.eriksson@chalmers.se>

            * ARTS-XML-DATA-1-1-29

            * climatology/msis90: Created MSIS90 climatology files. 

            * climatology/cira86: Created this folder for climatology version
            of CIRA86. Just README and output files here.

            * atmosphere/cira86: Was not updated. Files now stored as GField3.
            A climatology is also generated. A better treatment of water vapour 
            when calculating HSE added. README.FIRST revised.



git-svn-id: https://radiativetransfer.org/svn/rt/arts-xml-data/trunk@6165 aaf1aab0-4228-0410-ad68-8dceda47f409

ChangeLog

+2009-11-03  Patrick Eriksson  <patrick.eriksson@chalmers.se>
+
+	* ARTS-XML-DATA-1-1-29
+
+	* climatology/msis90: Created MSIS90 climatology files. 
+
+	* climatology/cira86: Created this folder for climatology version
+	of CIRA86. Just README and output files here.
+
+	* atmosphere/cira86: Was not updated. Files now stored as GField3.
+	A climatology is also generated. A better treatment of water vapour 
+	when calculating HSE added. README.FIRST revised.
+
 2009-03-31  Ajil Kottayil <ajil.kottayil@ltu.se>
 
 	* ARTS-XML-DATA-1-1-28

atmosphere/cira86/README.FIRST

-This directory contains files describing the COSPAR International Reference 
-Atmosphere (CIRA-86)
+This directory contains files describing parts of the COSPAR
+International Reference Atmosphere (CIRA-86)
 
 The original CIRA-86 data are zonally averaged monthly mean
 climatologies of several atmospheric parameters.
@@ -39,9 +39,9 @@ this folder. The function modifies the data in some ways:
 
 * 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*.
+  instead of geometrical). For this calculation, water vapour is set
+  to 50% RH for pressures > 350 hPa. A complete dry atmosphere is
+  assumed for higher altitudes.
 
 Patrick Eriksson
 2007-11-01
\ No newline at end of file

atmosphere/cira86/cira86_month1.t.xml

 <?xml version="1.0"?>
 <arts format="ascii" version="1">
-<GriddedField3>
-<Vector nelem="71">
+<GriddedField3 name="CIRA86 temperature for month 1">
+<Vector name="Pressure" nelem="71">
 1.0130000e+05
 7.8893000e+04
 6.1442000e+04
@@ -74,7 +74,7 @@
 3.2700000e-03
 2.5400000e-03
 </Vector>
-<Vector nelem="35">
+<Vector name="Latitude" nelem="35">
 -9.0000000e+01
 -8.0000000e+01
 -7.5000000e+01
@@ -111,10 +111,10 @@
 8.0000000e+01
 9.0000000e+01
 </Vector>
-<Vector nelem="1">
+<Vector name="Longitude" nelem="1">
 0.0000000e+00
 </Vector>
-<Tensor3 npages="71" nrows="35" ncols="1">
+<Tensor3 name="Temperature" npages="71" nrows="35" ncols="1">
 2.4890000e+02
 2.4890000e+02
 2.5000000e+02