netcdf data4papers/Vals_2022/ACSLuginin_aerosol_GCM_thermos.nc {
  dimensions:
    Time = 267;
    altitude = 101;
  variables:
    float longitude(Time=267);
      :units = "degrees_east";
      :description = "East longitude";

    float latitude(Time=267);
      :units = "degrees_north";
      :description = "North latitude";

    float loct(Time=267);
      :description = "Local time";
      :units = "sol fraction";

    float h2o_vap(Time=267, altitude=101);
      :description = "h2o vapour mmr";
      :units = "kg/kg";

    float h2o_ice(Time=267, altitude=101);
      :units = "kg/kg";
      :description = "h2o ice mmr";

    float hdo_vap(Time=267, altitude=101);
      :description = "hdo vapour mmr";
      :units = "kg/kg";

    float saturation(Time=267, altitude=101);
      :description = "Saturation";
      :units = "dimless";

    float temp(Time=267, altitude=101);
      :description = "Temperature";
      :units = "K";

    float rho(Time=267, altitude=101);
      :description = "Density";
      :units = "kg/m3";

    float Ls(Time=267);
      :description = "Solar Longitude";
      :units = "degrees";

    int altitude(altitude=101);
      :description = "Altitude above the areoid";
      :units = "km";

  // global attributes:
  :comment = "Concatenation of martian months 6 to 12 (Ls=180-360) of GCM outputs computed with MY34 dust load scenario. The file has been interpolated to a vertical grid in altitude above the areoid, and to the ACS coordinates. Photochemistry and extension to the thermosphere are turned on in this simulation.";
}