Changes between Version 4 and Version 5 of doc/tec/usm


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Timestamp:
Feb 26, 2019 6:53:51 PM (6 years ago)
Author:
rvtils
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  • doc/tec/usm

    v4 v5  
    33Main page of the urban surface model under construction. Click [wiki:doc/app/chempar here] for first information about capabilities and model steering. Also available, the related article ''PALM-USM v1.0: A new urban surface model integrated into the PALM large-eddy simulation model'' (Resler et al., Geosci. Model Dev., 10, 3635–3659, [https://doi.org/​10.5194/gmd-10-3635-2017 ​10.5194/gmd-10-3635-2017])
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     5[[NoteBox(note,This page is part of the **Urban Surface Model** (USM) documentation. \\ It describes the physical and numerical realization of the USM. \\ Please also see the **[wiki:doc/app/usmpar namelist parameters]**., 450px)]]
    56
     7== Overview ==
     8Since r19xx an urban surface model (USM) is available in PALM (see [source:palm/trunk/SOURCE/urban_surface_mod.f90 urban_surface_mod.f90]). It consists of a multi layer wall and soil model, predicting wall and soil temperature and moisture content, and a solver for the energy balance, predicting the temperature of the surface or the skin layer.
    69Urban surfaces (building surfaces) are simulated using a tile approach. Each surface element consists of a fraction of bare wall/ roof, window and green elements (green roofs/ facades) with underlying soil layers (green roofs only) and a bare wall/ roof structure.
     10
     11== Energy balance solver ==
     12The energy balance of the urban surfaces reads
     13{{{
     14#!Latex
     15\begin{equation*}
     16   C_0 \dfrac{dT_0}{dt} = R_\mathrm{n} - H - LE - G
     17\end{equation*}
     18}}}
     19where ''C'',,0,, and ''T'',,0,, are the heat capacity and radiative temperature of the surface skin layer, respectively. Note that  ''C'',,0,, is usually zero as it is assumed that the skin layer does not have a heat capacity (see also below). ''R'',,n,,, ''H'', ''LE'', and ''G'' are the net radiation, sensible heat flux, latent heat flux, and ground (soil) heat flux at the surface, respectively.
     20
     21The energy balance is calculated for each urban surface tile individually and the three radiation surface temperatures are combined together.
     22
     23
     24The parametrisation of the sensible heat flux, latent heat flux and ground heat flux of the wall/ window/ soil is equivalent to the Land Surface Model (LSM).
     25
    726
    827The wall heat and green heat model consist of prognostic equations for the bare, window and soil temperature and the volumetric soil moisture which are solved for multiple layers. The models only take transport into account that is orthogonal to the urban surface layer orientation and no ice phase is considered. By default, the wall heat model and the green heat soil model consists of four layers each (see Fig. 1 below), in which the orthogonal heat and water transport inside the soil is modelled.
    928
    10 The energy balance is calculated for each urban surface tile individually and the three radiation surface temperatures are combined together.
    11 The parametrisation of the sensible heat flux, latent heat flux and ground heat flux of the wall/ window/ soil is equivalent to the Land Surface Model (LSM).
     29[[Image(urban_surfaces.png,600px, border=1)]]
     30
     31Figure 1: urban surfaces (bare, window, green) in PALM-4U
    1232
    1333The physical properties of the urban surfaces and wall, window and green soil elements can be set using values from a building database where different types of buildings are defined. The insulation value of windows are there only characterized by the U-value and and the heat capacity and heat conductivity is evenly distributed (no real glas or gas layers are taken into account.
     
    1838
    1939
    20 Boundary Conditions
     40=== Boundary conditions ===
    2141Neumann boundary conditions are used for the transport of heat at the upper boundary (surface). The values are given by the energy balance. At the bottom boundary either a fixed temperature of the inner wall and winow layers is set or the ground heat flux from the inner wall and window surface is used that is calculated by the indoor model (Dirichlet conditions).
    22 
    23 
    24 [[Image(urban_surfaces.png,600px, border=1)]]
    25 
    26 Figure 1: urban surfaces (bare, window, green) in PALM-4U