Changes between Version 30 and Version 31 of doc/tec/bc


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Timestamp:
Jun 6, 2017 10:05:07 AM (8 years ago)
Author:
suehring
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  • doc/tec/bc

    v30 v31  
    284284 1. the obstacle shape is approximated by (an appropriate number of) full grid cells to fit the grid, i.e., a grid cell is either 100% fluid or 100% obstacle,
    285285
    286  2. so far, only bottom surface-mounted obstacles are permitted (no holes or overhanging structures), and
    287 
    288  3. the obstacles are fixed (not moving).
    289 
    290 These simplifications transform the 3-D obstacle dimension to a 2.5-D topography. This reduced dimension format is conform to the Digital Elevation Model (DEM) format. DEMs of city morphologies have become increasingly available worldwide due to advances in remote sensing technologies. Consequently, it is sufficient to provide 2-D topography height data to mask obstacles and their faces in PALM. The model domain is then separated into three subdomains (see Fig. 3):
    291 
    292  A. grid points in free fluid without adjacent walls, where the standard PALM code is executed,
    293 
    294  B. grid points next to walls that require extra code (e.g., wall functions), and
     286 2. the obstacles are fixed (not moving).
     287
     288With revision -r2232, the topography implementation is completely revised.
     289Starting from this revision, overhanging structures as for example bridges, ceilings, or tunnels, are allowed, i.e. topography does not necessarily be surface-mounted.
     290If no overhanging structures are present, the 3-D obstacle dimension reduces to a 2.5-D topography format, which is conform to the Digital Elevation Model (DEM) format (DEMs of city morphologies have become increasingly available worldwide due to advances in remote sensing technologies).
     291In case of overhanging structures, however, 3-D topography information is required to mask obstacles and their faces in PALM.
     292
     293The model domain is then separated into three subdomains (see Fig. 3):
     294
     295 A. grid points in free fluid without adjacent surfaces, where the standard PALM code is executed,
     296
     297 B. grid points next to surface that require extra code (e.g., surface parametrization), and
    295298
    296299 C. grid points within obstacles that are excluded from calculations
     
    298301[[Image(04.png,600px,border=1)]]
    299302
    300 Figure 4: Sketch of the 2.5-D implementation of topography using the mask method (here for ''w''). The yellow and red lines represent the limits of the arrays ''nzb_w_inner'' and ''nzb_w_outer'' as described in Sect. [wiki:doc/tec/topography topography implementation], respectively.
    301 
    302 Additional topography code is only executed in grid volumes of subdomain B. The faces of the obstacles are always located where the
    303 respective wall-normal velocity components ''u'', ''v'', and ''w'' are defined (cf. Fig. 1 in Sect. [wiki:doc/tec/discret discretization]) so that the impermeability boundary condition can be implemented by setting the respective wall-normal velocity component to zero.
    304 
    305 An exception is made for the 5th-order advection scheme, where the numerical stencil at grid points adjacent to obstacles would require data within the obstacle. In order to avoid this behavior, the order of the advection scheme is successively degraded at respective grid volumes adjacent to obstacles, i.e., from the 5th-order to 3rd-order at the second grid point above/beside an obstacle and from 3rd-order to 1st-order at grid points directly adjacent to an obstacle.
    306 
    307 Wall surfaces in PALM can be aligned horizontally (bottom surface or rooftop, i.e., always facing upwards) or vertically (facing north,
    308 east, south or west direction). At horizontal surfaces, PALM allows to either specify the surface values (''θ, q,,v,,, s'') or
    309 to prescribe their respective surface fluxes. The latter is the only option for vertically oriented surfaces. Simulations with topography
    310 require the application of MOST between each wall surface and the first computational grid point. For vertical walls, neutral
    311 stratification is assumed for MOST. The topography implementation has been validated by [#letzel2008 Letzel et al. (2008)] and [#kanda2013 Kanda et al. (2013)}. [#park2013 Park and Baik (2013)] have recently extended the vertical wall boundary conditions for non-neutral
     303Figure 4: Sketch of the topograhy implementation using the mask method (here for ''w''). The yellow and red lines represent the limits of the arrays ''nzb_w_inner'' and ''nzb_w_outer'' as described in Sect. [wiki:doc/tec/topography topography implementation], respectively.
     304
     305Additional topography code is executed in grid volumes of subdomain B. The faces of the obstacles are always located where the
     306respective surface-normal velocity components ''u'', ''v'', and ''w'' are defined (cf. Fig. 1 in Sect. [wiki:doc/tec/discret discretization]) so that the impermeability boundary condition can be implemented by setting the respective surface-normal velocity component to zero.
     307
     308In case of 5th-order advection scheme, the numerical stencil at grid points adjacent to obstacles would require data which is located within the obstacle.
     309In order to avoid this, the order of the advection scheme is successively degraded at respective grid volumes adjacent to obstacles, i.e., from the 5th-order to 3rd-order at the second grid point above/beside an obstacle and from 3rd-order to 1st-order at grid points directly adjacent to an obstacle.
     310
     311Surfaces in PALM can be aligned horizontally upward facing (e.g. bottom surface or rooftop), horizontally downward facing (e.g. undersurface of bridges), or vertically (facing north, east, south or west direction).
     312At horizontal surfaces, PALM allows to either specify the surface values (''θ, q,,v,,, s'') or to prescribe their respective surface fluxes.
     313The latter is the only option for vertically oriented surfaces.
     314Simulations with topography require the application of MOST between each surface and the first computational grid point outside of the topography.
     315For vertical and horizontal downward-facing surfaces, neutral stratification is assumed for MOST.
     316The topography implementation has been validated by [#letzel2008 Letzel et al. (2008)] and [#kanda2013 Kanda et al. (2013)}.
     317[#park2013 Park and Baik (2013)] have recently extended the vertical wall boundary conditions for non-neutral
    312318stratifications and validated their results against wind tunnel data. Up to now, however, these modifications are not included in PALM 4.0. Figure 4 shows exemplarily the development of turbulence structures induced by a densely built-up artificial island off the coast of Macau, China (see also animation in [#knoop2014 Knoop et al., 2014]). The approaching flow above the sea exhibits relatively weak turbulence due to the smooth water surface. Within the building areas, strong turbulence is generated by additional wind shear (due to the walls of isolated buildings) and due to a general increase in surface roughness.
    313319