Table of Contents - The Atmospheric Studies Group at TRC

Table of Contents - The Atmospheric Studies Group at TRC Table of Contents - The Atmospheric Studies Group at TRC

29.01.2015 Views

Section 7: Prognostic Meteorological Interfaces 7.6 CALTAPM Preprocessor CALTAPM operates on the output from CSIRO’s Division of Atmospheric Research, The Air Pollution Model, (TAPM). It outputs all the TAPM 3D variables: wind speed, wind direction, temperature, relative humidity, potential temperature and turbulent kinetic energy. It also outputs the 2D variables total solar radiation, net radiation, sensible heat flux, evaporative heat flux, friction velocity, potential virtual temperature scale, potential temperature scale, convective velocity scale, mixing height, surface temperature and rainfall. Table 7-32 lists the variables extracted using CALTAPM which are output to the 3D.DAT file format. CALTAPM reads and interprets all information contained in the TAPM configuration input file headers (physical options, dates, grid size and location, etc.). TAPM requires a grid centre coordinate of latitude and longitude corresponding to the centre of the chosen grid domains. TAPM uses a Cartesian system where the x is positive from west to east and y is positive from south to north and specifies the centre of the local system with respect to the latitude and longitude of the grid centre. CALTAPM assumes the TAPM coordinate system is UTM and Datum of WGS-84 and uses this system directly in the 3D data file. Like CALMET TAPM uses a non-staggered horizontal coordinate system (see Figure 7-3) and a terrain-following vertical coordinate system. In the horizontal, all variables are defined at the center of each grid cell and the first level is 10m. The vertical levels of TAPM are used directly with no transformation to sigma levels in the 3D data file. 7-60

Section 7: Prognostic Meteorological Interfaces Table 7-27: Variables Available in CALTAPM Three-dimensional Output Files Variables Vertical profile Pressure Height above M.S.L Temperature Wind direction Wind speed Vertical velocity Relative humidity Vapor mixing ratio Surface variables in header Sea level pressure Rain fall Snow cover Short wave radiation at surface Long wave radiation at surface Air temperature at 2 meters above ground Specific humidity at 2 meters above ground Wind direction at 10m meters above ground Wind speed at 10 meters above ground Sea surface temperature * Exists only when available in TAPM output. ** Set to zero or blank if not available. 3D.DAT Y Y Y Y Y Y Y Y Y Y Y** Y Y Y** Y** Y** Y** Y 7-61

Section 7: Prognostic Meteorological Interfaces<br />

7.6 CALTAPM Preprocessor<br />

CALTAPM oper<strong>at</strong>es on the output from CSIRO’s Division <strong>of</strong> <strong>Atmospheric</strong> Research, <strong>The</strong> Air Pollution<br />

Model, (TAPM). It outputs all the TAPM 3D variables: wind speed, wind direction, temper<strong>at</strong>ure, rel<strong>at</strong>ive<br />

humidity, potential temper<strong>at</strong>ure and turbulent kinetic energy. It also outputs the 2D variables total solar<br />

radi<strong>at</strong>ion, net radi<strong>at</strong>ion, sensible he<strong>at</strong> flux, evapor<strong>at</strong>ive he<strong>at</strong> flux, friction velocity, potential virtual<br />

temper<strong>at</strong>ure scale, potential temper<strong>at</strong>ure scale, convective velocity scale, mixing height, surface<br />

temper<strong>at</strong>ure and rainfall. <strong>Table</strong> 7-32 lists the variables extracted using CALTAPM which are output to the<br />

3D.DAT file form<strong>at</strong>.<br />

CALTAPM reads and interprets all inform<strong>at</strong>ion contained in the TAPM configur<strong>at</strong>ion input file headers<br />

(physical options, d<strong>at</strong>es, grid size and loc<strong>at</strong>ion, etc.). TAPM requires a grid centre coordin<strong>at</strong>e <strong>of</strong> l<strong>at</strong>itude<br />

and longitude corresponding to the centre <strong>of</strong> the chosen grid domains. TAPM uses a Cartesian system<br />

where the x is positive from west to east and y is positive from south to north and specifies the centre <strong>of</strong><br />

the local system with respect to the l<strong>at</strong>itude and longitude <strong>of</strong> the grid centre. CALTAPM assumes the<br />

TAPM coordin<strong>at</strong>e system is UTM and D<strong>at</strong>um <strong>of</strong> WGS-84 and uses this system directly in the 3D d<strong>at</strong>a<br />

file. Like CALMET TAPM uses a non-staggered horizontal coordin<strong>at</strong>e system (see Figure 7-3) and a<br />

terrain-following vertical coordin<strong>at</strong>e system. In the horizontal, all variables are defined <strong>at</strong> the center <strong>of</strong><br />

each grid cell and the first level is 10m. <strong>The</strong> vertical levels <strong>of</strong> TAPM are used directly with no<br />

transform<strong>at</strong>ion to sigma levels in the 3D d<strong>at</strong>a file.<br />

7-60

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