Changes between Version 43 and Version 44 of doc/tec/microphysics


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Timestamp:
May 25, 2018 9:01:27 AM (7 years ago)
Author:
schwenkel
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  • doc/tec/microphysics

    v43 v44  
    1818instead of ''θ'' as described in Sect. [wiki:doc/tec/gov governing equations]. Since ''q'' and ''θ'',,l,, are conserved quantities for wet adiabatic processes, condensation/evaporation is not considered for these variables.
    1919
    20 PALM offers three different schemes ([#kessler1969 Kessler (1969)], [#seifert2001 Seifert and Beheng (2001],[#seifert2006  2006)], [#morrison2007 Morrison (2007)]) for the treatment of liquid phase microphysics. The [#kessler1969 Kessler (1969)] scheme provides a computational inexpensive way for the bulk microphysics. However, it only converts supersaturation into liquid water and considering autoconversion after a parameterization of [#kessler1969 Kessler (1969)].
     20PALM offers three different schemes ([#kessler1969 Kessler (1969)], [#seifert2001 Seifert and Beheng (2001],[#seifert2006  2006)], [#morrison2007 Morrison et al. (2007)]) for the treatment of liquid phase microphysics. The [#kessler1969 Kessler (1969)] scheme provides a computational inexpensive way for the bulk microphysics. However, it only converts supersaturation into liquid water and considering autoconversion after a parameterization of [#kessler1969 Kessler (1969)].
    2121
    2222A more detailed parameterization is given by following the two-moment scheme of [#seifert2001 Seifert and Beheng (2001],[#seifert2006  2006)], which is based on the separation of the droplet spectrum into droplets with radii < 40 μm (cloud droplets) and droplets with radii ≥ 40 μm (rain droplets). Here, the model predicts the first two moments of these partial droplet spectra, namely cloud and rain
     
    4747with ''N'',,c,, and ''q'',,c,, being a fixed parameter and a diagnostic quantity, respectively.
    4848
    49 The [#morrison2007 Morrison (2007)] microphysics scheme can be understood as an extension of the scheme of [#seifert2001 Seifert and Beheng (2001],[#seifert2006  2006)], where ''N'',,c,, and ''q'',,c,, are prognostic quantities as well. Moreover, using the [#morrison2007 Morrison (2007)] scheme includes an explicit calculation of diffusional growth and an activation parameterization.
    50 
    51 In the next subsections we will describe the diagnostic/prognostic determination (in dependence of the chosen scheme) of ''q'',,c,,. From Sect. [wiki:doc/tec/microphysics#Autoconversion autoconversion] on, the microphysical processes considered in the sink/source terms of ''θ'',,l,,, ''q'', ''N'',,r,, and ''q'',,r,,, as well as ''N'',,c,, and ''q'',,c,, for the [#morrison2007 Morrison (2007)] scheme.
     49The [#morrison2007 Morrison et al. (2007)] microphysics scheme can be understood as an extension of the scheme of [#seifert2001 Seifert and Beheng (2001],[#seifert2006  2006)], where ''N'',,c,, and ''q'',,c,, are prognostic quantities as well. Moreover, using the [#morrison2007 Morrison et al. (2007)] scheme includes an explicit calculation of diffusional growth and an activation parameterization.
     50
     51In the next subsections we will describe the diagnostic/prognostic determination (in dependence of the chosen scheme) of ''q'',,c,,. From Sect. [wiki:doc/tec/microphysics#Autoconversion autoconversion] on, the microphysical processes considered in the sink/source terms of ''θ'',,l,,, ''q'', ''N'',,r,, and ''q'',,r,,, as well as ''N'',,c,, and ''q'',,c,, for the [#morrison2007 Morrison et al. (2007)] scheme.
    5252{{{
    5353#!Latex
     
    7777== Activation of cloud droplets ==
    7878
    79 The use of the  [#morrison2007 Morrison et al (2007)] enables a prognostic equation for the cloud droplet number concentration. Here, it is assumed that cloud droplets are activated in dependence of the current supersaturation. This basic method is called Twomey activation scheme with the general form of
     79The use of the  [#morrison2007 Morrison et al. (2007)] scheme enables a prognostic equation for the cloud droplet number concentration. Here, it is assumed that cloud droplets are activated in dependence of the current supersaturation. This basic method is called Twomey activation scheme with the general form of
    8080{{{
    8181#!Latex
     
    129129}}}
    130130
    131 In contrast to that an explicit approach for the diffusional growth is applied in case of [#morrison2007 Morrison et al (2007)]. The condensation rate is calculated follwoing [#khairoutdinov2000 Khairoutdinov and Kogan (2000)] and given by
     131In contrast to that an explicit approach for the diffusional growth is applied in case of [#morrison2007 Morrison et al. (2007)]. The condensation rate is calculated follwoing [#khairoutdinov2000 Khairoutdinov and Kogan (2000)] and given by
    132132{{{
    133133#!Latex